Clean Water Rule: Definition of “Waters of the United States”, 37053-37127 [2015-13435]
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Vol. 80
Monday,
No. 124
June 29, 2015
Part II
Department of Defense
Department of the Army, Corps of Engineers
33 CFR Part 328
Environmental Protection Agency
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40 CFR Parts 110, 112, 116, et al.
Clean Water Rule: Definition of ‘‘Waters of the United States’’; Final Rule
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Federal Register / Vol. 80, No. 124 / Monday, June 29, 2015 / Rules
DEPARTMENT OF DEFENSE
Department of the Army, Corps of
Engineers
33 CFR Part 328
ENVIRONMENTAL PROTECTION
AGENCY
40 CFR Parts 110, 112, 116, 117, 122,
230, 232, 300, 302, and 401
[EPA–HQ–OW–2011–0880; FRL–9927–20–
OW]
RIN 2040–AF30
Clean Water Rule: Definition of
‘‘Waters of the United States’’
U.S. Army Corps of Engineers,
Department of the Army, Department of
Defense; and Environmental Protection
Agency (EPA).
ACTION: Final rule.
AGENCY:
The Environmental Protection
Agency (EPA) and the U.S. Army Corps
of Engineers (Corps) are publishing a
final rule defining the scope of waters
protected under the Clean Water Act
(CWA or the Act), in light of the statute,
science, Supreme Court decisions in
U.S. v. Riverside Bayview Homes, Solid
Waste Agency of Northern Cook County
v. U.S. Army Corps of Engineers
(SWANCC), and Rapanos v. United
States (Rapanos), and the agencies’
experience and technical expertise. This
final rule reflects consideration of the
extensive public comments received on
the proposed rule. The rule will ensure
protection for the nation’s public health
and aquatic resources, and increase
CWA program predictability and
consistency by clarifying the scope of
‘‘waters of the United States’’ protected
under the Act.
DATES: This rule is effective on August
28, 2015. In accordance with 40 CFR
part 23, this regulation shall be
considered issued for purposes of
judicial review at 1 p.m. Eastern time on
July 13, 2015.
FOR FURTHER INFORMATION CONTACT: Ms.
Donna Downing, Office of Water (4502–
T), Environmental Protection Agency,
1200 Pennsylvania Avenue NW.,
Washington, DC 20460; telephone
number 202–566–2428; email address:
CWAwaters@epa.go v. Ms. Stacey
Jensen, Regulatory Community of
Practice (CECW–CO–R), U.S. Army
Corps of Engineers, 441 G Street NW.,
Washington, DC 20314; telephone
number 202–761–5856; email address:
USACE_CWA_Rule@usace.army.mil.
SUPPLEMENTARY INFORMATION: This final
rule does not establish any regulatory
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SUMMARY:
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requirements. Instead, it is a definitional
rule that clarifies the scope of ‘‘waters
of the United States’’ consistent with the
Clean Water Act (CWA), Supreme Court
precedent, and science. Programs
established by the CWA, such as the
section 402 National Pollutant
Discharge Elimination System (NPDES)
permit program, the section 404 permit
program for discharge of dredged or fill
material, and the section 311 oil spill
prevention and response programs, all
rely on the definition of ‘‘waters of the
United States.’’ Entities currently are,
and will continue to be, regulated under
these programs that protect ‘‘waters of
the United States’’ from pollution and
destruction.
State, tribal, and local governments
have well-defined and longstanding
relationships with the Federal
government in implementing CWA
programs and these relationships are not
altered by the final rule. Forty-six states
and the U.S. Virgin Islands have been
authorized by EPA to administer the
NPDES program under section 402, and
two states have been authorized by the
EPA to administer the section 404
program. All states and forty tribes have
developed water quality standards
under the CWA for waters within their
boundaries. A federal advisory
committee has recently been announced
to assist states in identifying the scope
of waters assumable under the section
404 program.
The scope of jurisdiction in this rule
is narrower than that under the existing
regulation. Fewer waters will be defined
as ‘‘waters of the United States’’ under
the rule than under the existing
regulations, in part because the rule
puts important qualifiers on some
existing categories such as tributaries. In
addition, the rule provides greater
clarity regarding which waters are
subject to CWA jurisdiction, reducing
the instances in which permitting
authorities, including the states and
tribes with authorized section 402 and
404 CWA permitting programs, would
need to make jurisdictional
determinations on a case-specific basis.
Table of Contents
I. General Information
A. How can I get copies of this document
and related information?
B. Under what legal authority is this rule
issued?
II. Executive Summary
III. Significant Nexus Determinations
A. The Significant Nexus Standard
B. Science Report
C. Significant Nexus Conclusions
1. Scope of Significant Nexus Analysis
2. Categories of Waters Determined to Have
a Significant Nexus
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3. Case-Specific Significant Nexus
Determinations
IV. Definition of ‘‘Waters of the United
States’’
A. Summary of Rule
B. Traditional Navigable Waters
C. Interstate Waters
D. Territorial Seas
E. Impoundments
F. Tributaries
G. Adjacent Waters
H. Case-Specific ‘‘Waters of the United
States’’
I. Waters and Features That Are Not
‘‘Waters of the United States’’
V. Economic Impacts
VI. Related Acts of Congress, Executive
Orders, and Agency Initiatives
A. Executive Order 12866: Regulatory
Planning and Review and Executive
Order 13563: Improving Regulation and
Regulatory Review
B. Paperwork Reduction Act
C. Regulatory Flexibility Act
D. Unfunded Mandates Reform Act
E. Executive Order 13132: Federalism
F. Executive Order 13175: Consultation
and Coordination With Indian Tribal
Governments
G. Executive Order 13045: Protection of
Children From Environmental Health
and Safety Risks
H. Executive Order 13211: Actions
Concerning Regulations That
Significantly Affect Energy Supply,
Distribution, or Use
I. National Technology Transfer and
Advancement Act
J. Executive Order 12898: Federal Actions
To Address Environmental Justice in
Minority Populations and Low-Income
Populations
K. Congressional Review Act
L. Environmental Documentation
M. Judicial Review
I. General Information
A. How can I get copies of this
document and related information?
1. Docket. An official public docket
for this action has been established
under Docket Id. No. EPA–HQ–OW–
2011–0880. The official public docket
consists of the documents specifically
referenced in this action, any public
comments received, and other
information related to this action. The
official public docket also includes a
Technical Support Document that
provides additional legal and scientific
discussion for issues raised in this rule,
and the Response to Comments
document. Although a part of the
official docket, the public docket does
not include Confidential Business
Information or other information whose
disclosure is restricted by statute. The
official public docket is the collection of
materials that is available for public
viewing at the OW Docket, EPA West,
Room 3334, 1301 Constitution Ave.
NW., Washington, DC 20004. This
Docket Facility is open from 8:30 a.m.
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Federal Register / Vol. 80, No. 124 / Monday, June 29, 2015 / Rules
403, 404, 407. The CWA is the nation’s
single most important statute for
protecting America’s clean water against
pollution, degradation, and destruction.
To provide that protection, the Supreme
Court has consistently agreed that the
geographic scope of the CWA reaches
beyond waters that are navigable in fact.
Peer-reviewed science and practical
experience demonstrate that upstream
waters, including headwaters and
wetlands, significantly affect the
chemical, physical, and biological
integrity of downstream waters by
playing a crucial role in controlling
sediment, filtering pollutants, reducing
flooding, providing habitat for fish and
other aquatic wildlife, and many other
vital chemical, physical, and biological
processes.
This final rule interprets the CWA to
cover those waters that require
protection in order to restore and
maintain the chemical, physical, or
biological integrity of traditional
navigable waters, interstate waters, and
the territorial seas. This interpretation is
based not only on legal precedent and
the best available peer-reviewed
B. Under what legal authority is this rule science, but also on the agencies’
issued?
technical expertise and extensive
experience in implementing the CWA
The authority for this rule is the
Federal Water Pollution Control Act, 33 over the past four decades. The rule will
clarify and simplify implementation of
U.S.C. 1251, et seq., including sections
the CWA consistent with its purposes
301, 304, 311, 401, 402, 404 and 501.
through clearer definitions and
II. Executive Summary
increased use of bright-line boundaries
to establish waters that are jurisdictional
In this final rule, the agencies clarify
by rule and limit the need for casethe scope of ‘‘waters of the United
specific analysis. The agencies
States’’ that are protected under the
Clean Water Act (CWA), based upon the emphasize that, while the CWA
establishes permitting requirements for
text of the statute, Supreme Court
covered waters to ensure protection of
decisions, the best available peerwater quality, these requirements only
reviewed science, public input, and the
apply with respect to discharges of
agencies’ technical expertise and
experience in implementing the statute. pollutants to the covered water. In the
absence of a discharge of a pollutant, the
This rule makes the process of
identifying waters 1 protected under the CWA does not impose permitting
restrictions on the use of such water.
CWA easier to understand, more
Additionally, Congress has exempted
predictable, and consistent with the law
certain discharges, and the rule does not
and peer-reviewed science, while
protecting the streams and wetlands that affect any of the exemptions from CWA
section 404 permitting requirements
form the foundation of our nation’s
provided by CWA section 404(f),
water resources.
Congress enacted the CWA ‘‘to restore including those for normal farming,
ranching, and silviculture activities.
and maintain the chemical, physical,
CWA section 404(f); 40 CFR 232.3; 33
and biological integrity of the Nation’s
CFR 323.4. This rule not only maintains
waters,’’ section 101(a), and to
current statutory exemptions, it expands
complement statutes that protect the
regulatory exclusions from the
navigability of waters, such as the
definition of ‘‘waters of the United
Rivers and Harbors Act. 33 U.S.C. 401,
States’’ to make it clear that this rule
does not add any additional permitting
1 The agencies use the term ‘‘water’’ and ‘‘waters’’
requirements on agriculture. The rule
in categorical reference to rivers, streams, ditches,
wetlands, ponds, lakes, oxbows, and other types of
also does not regulate shallow
natural or man-made aquatic systems, identifiable
subsurface connections nor any type of
by the water contained in these aquatic systems or
groundwater, erosional features, or land
by their chemical, physical, and biological
indicators. The agencies use the terms ‘‘waters’’ and use, nor does it affect either the existing
‘‘water bodies’’ interchangeably in this preamble.
statutory or regulatory exemptions from
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to 4:30 p.m., Monday through Friday,
excluding legal holidays. The OW
Docket telephone number is 202–566–
2426. A reasonable fee will be charged
for copies.
2. Electronic Access. You may access
this Federal Register document
electronically under the ‘‘Federal
Register’’ listings at https://
www.regulations.gov. An electronic
version of the public docket is available
through EPA’s electronic public docket
and comment system, EPA Dockets. You
may access EPA Dockets at https://
www.regulations.gov to view public
comments, access the index listing of
the contents of the official public
docket, and access those documents in
the public docket that are available
electronically. For additional
information about EPA’s public docket,
visit the EPA Docket Center homepage
at https://www.epa.gov/epahome/
dockets.htm. Although not all docket
materials may be available
electronically, you may still access any
of the publicly available docket
materials through the Docket Facility.
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NPDES permitting requirements, such
as for agricultural stormwater discharges
and return flows from irrigated
agriculture, or the status of water
transfers. CWA section 402(l)(1); CWA
section 402(l)(2); CWA section 502(14);
40 CFR 122.3(f); 40 CFR 122.2.
Finally, even where waters are
covered by the CWA, the agencies have
adopted many streamlined regulatory
requirements to simplify and expedite
compliance through the use of measures
such as general permits and
standardized mitigation measures. The
agencies will continue to develop
general permits and simplified
procedures, particularly as they affect
crossings of covered ephemeral and
intermittent tributaries jurisdictional
under this rule to ensure that projects
that offer significant social benefits,
such as renewable energy development,
can proceed with the necessary
environmental safeguards while
minimizing permitting delays.
The jurisdictional scope of the CWA
is ‘‘navigable waters,’’ defined in section
502(7) of the statute as ‘‘waters of the
United States, including the territorial
seas.’’ The term ‘‘navigable waters’’ is
used in a number of provisions of the
CWA, including the section 402
National Pollutant Discharge
Elimination System (NPDES) permit
program, the section 404 permit
program, the section 311 oil spill
prevention and response program,2 the
water quality standards and total
maximum daily load programs (TMDL)
under section 303, and the section 401
state water quality certification process.
However, while there is only one CWA
definition of ‘‘waters of the United
States,’’ there may be other statutory
factors that define the reach of a
particular CWA program or provision.3
2 While section 311 uses the phrase ‘‘navigable
waters of the United States,’’ EPA has interpreted
it to have the same breadth as the phrase ‘‘navigable
waters’’ used elsewhere in section 311, and in other
sections of the CWA. See United States v. Texas
Pipe Line Co., 611 F.2d 345, 347 (10th Cir. 1979);
United States v. Ashland Oil & Transp. Co., 504
F.2d 1317, 1324–25 (6th Cir. 1974). In 2002, EPA
revised its regulatory definition of ‘‘waters of the
United States’’ in 40 CFR part 112 to ensure that
the language of the rule was consistent with the
regulatory language of other CWA programs. Oil
Pollution Prevention & Response; NonTransportation-Related Onshore & Offshore
Facilities, 67 FR 47042, July 17, 2002. A district
court vacated the rule for failure to comply with the
Administrative Procedure Act, and reinstated the
prior regulatory language. American Petroleum Ins.
v. Johnson, 541 F. Supp. 2d 165 (D. D.C. 2008).
However, EPA interprets ‘‘navigable waters of the
United States’’ in CWA section 311(b), in the pre2002 regulations, and in the 2002 rule to have the
same meaning as ‘‘navigable waters’’ in CWA
section 502(7).
3 For example, the CWA section 402 (33 U.S.C.
1342) program regulates discharges of pollutants
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Existing regulations (last codified in
1986) define ‘‘waters of the United
States’’ as traditional navigable waters,
interstate waters, all other waters that
could affect interstate or foreign
commerce, impoundments of waters of
the United States, tributaries, the
territorial seas, and adjacent wetlands.
33 CFR 328.3; 40 CFR 122.2.4
However, the Supreme Court has
issued three decisions that provide
critical context and guidance in
determining the appropriate scope of
‘‘waters of the United States’’ covered
by the CWA. In United States v.
Riverside Bayview Homes, 474 U.S. 121
(1985) (Riverside), the Court, in a
unanimous opinion, deferred to the
Corps’ ecological judgment that adjacent
wetlands are ‘‘inseparably bound up’’
with the waters to which they are
adjacent, and upheld the inclusion of
adjacent wetlands in the regulatory
definition of ‘‘waters of the United
States.’’ Id. at 134. The Court observed
that the broad objective of the CWA to
restore and maintain the integrity of the
Nation’s waters ‘‘incorporated a broad,
systemic view of the goal of maintaining
and improving water quality. . . .
Protection of aquatic ecosystems,
Congress recognized, demanded broad
federal authority to control pollution,
for ‘[w]ater moves in hydrologic cycles
and it is essential that discharge of
pollutants be controlled at the source.’
In keeping with these views, Congress
chose to define the waters covered by
the Act broadly.’’ Id. at 132–33 (citing
Senate Report No. 92–414, p. 77 (1972)).
In Solid Waste Agency of Northern
Cook County v. U.S. Army Corps of
Engineers, 531 U.S. 159 (2001)
(SWANCC), the Supreme Court held
that the use of ‘‘isolated’’ non-navigable
intrastate ponds by migratory birds was
not by itself a sufficient basis for the
from ‘‘point sources’’ to ‘‘waters of the United
States,’’ whether these pollutants reach
jurisdictional waters directly or indirectly. The
plurality opinion in Rapanos noted that ‘‘there is
no reason to suppose that our construction today
significantly affects the enforcement of § 1342. . . .
The Act does not forbid the ‘addition of any
pollutant directly to navigable waters from any
point source,’ but rather the ‘addition of any
pollutant to navigable waters.’ ’’ 547 U.S. at 743.
4 There are numerous regulations that utilize the
definition of ‘‘waters of the United States’’ and each
is codified consistent with its place in a particular
section of the Code of Federal Regulations. For
simplicity, throughout the preamble the agencies
refer to the rule as organized into (a), (b), (c)
provisions and intend the reference to encompass
the appropriate cites in each section of the Code of
Federal Regulations. For example, a reference to
(a)(1) is a reference to all instances in the CFR
identified as subject to this rule that state ‘‘All
waters which are currently used, were used in the
past, or may be susceptible to use in interstate or
foreign commerce, including all waters which are
subject to the ebb and flow of the tide.’’
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exercise of federal regulatory authority
under the CWA. Although the SWANCC
decision did not call into question
earlier decisions upholding the CWA’s
coverage of wetlands or other waters
‘‘adjacent’’ to traditional navigable
waters, it created uncertainty with
regard to the jurisdiction of other waters
and wetlands that, in many instances,
may play an important role in protecting
the integrity of the nation’s waters. The
majority opinion in SWANCC
introduced the concept that it was a
‘‘significant nexus’’ that informed the
Court’s reading of CWA jurisdiction
over waters that are not navigable in
fact.
Five years later, in Rapanos v. United
States, 547 U.S. 715 (2006) (Rapanos),
all Members of the Court agreed that the
term ‘‘waters of the United States’’
encompasses some waters that are not
navigable in the traditional sense. In
addition, Justice Kennedy’s opinion
indicated that the critical factor in
determining the CWA’s coverage is
whether a water has a ‘‘significant
nexus’’ to downstream traditional
navigable waters such that the water is
important to protecting the chemical,
physical, or biological integrity of the
navigable water, referring back to the
Court’s decision in SWANCC. Justice
Kennedy’s concurrence in Rapanos
stated that to constitute a ‘‘water of the
United States’’ covered by the CWA, ‘‘a
water or wetland must possess a
‘significant nexus’ to waters that are or
were navigable in fact or that could
reasonably be so made.’’ Id. at 759
(Kennedy, J., concurring in the
judgment) (citing SWANCC, 531 U.S. at
167, 172). Justice Kennedy concluded
that wetlands possess the requisite
significant nexus if the wetlands ‘‘either
alone or in combination with similarly
situated [wet]lands in the region,
significantly affect the chemical,
physical, and biological integrity of
other covered waters more readily
understood as ‘navigable.’’’ 547 U.S. at
780.
In this rule, the agencies interpret the
scope of the ‘‘waters of the United
States’’ for the CWA using the goals,
objectives, and policies of the statute,
the Supreme Court case law, the
relevant and available science, and the
agencies’ technical expertise and
experience as support. In particular, the
agencies looked to the objective of the
CWA ‘‘to restore and maintain the
chemical, physical, and biological
integrity of the Nation’s waters,’’ and
the scientific consensus on the strength
of the effects of upstream tributaries and
adjacent waters, including wetlands, on
downstream traditional navigable
waters, interstate waters, and the
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territorial seas. An important element of
the agencies’ interpretation of the CWA
is the significant nexus standard. This
significant nexus standard was first
informed by the ecological and
hydrological connections the Supreme
Court noted in Riverside Bayview,
developed and established by the
Supreme Court in SWANCC, and further
refined in Justice Kennedy’s opinion in
Rapanos. The agencies also utilized the
plurality standard in Rapanos by
establishing boundaries on the scope of
‘‘waters of the United States’’ and in
support of the exclusions from the
definition of ‘‘waters of the United
States.’’ The analysis used by the
agencies has been supported by all nine
of the United States Courts of Appeals
that have considered the issue.
The agencies assess the significance of
the nexus in terms of the CWA’s
objective to ‘‘restore and maintain the
chemical, physical, and biological
integrity of the Nation’s waters.’’ When
the effects are speculative or
insubstantial, the ‘‘significant nexus’’
would not be present. The science
demonstrates that the protection of
upstream waters is critical to
maintaining the integrity of the
downstream waters. The upstream
waters identified in the rule as
jurisdictional function as integral parts
of the aquatic environment, and if these
waters are polluted or destroyed, there
is a significant effect downstream.
In response to the Supreme Court
opinions, the agencies issued guidance
in 2003 (post-SWANCC) and 2008 (postRapanos). However, these two guidance
documents did not provide the public or
agency staff with the kind of
information needed to ensure timely,
consistent, and predictable
jurisdictional determinations. Many
waters are currently subject to casespecific jurisdictional analysis to
determine whether a ‘‘significant
nexus’’ exists, and this time and
resource intensive process can result in
inconsistent interpretation of CWA
jurisdiction and perpetuate ambiguity
over where the CWA applies. As a result
of the ambiguity that exists under
current regulations and practice
following these recent decisions, almost
all waters and wetlands across the
country theoretically could be subject to
a case-specific jurisdictional
determination.
Members of Congress, developers,
farmers, state and local governments,
energy companies, and many others
requested new regulations to make the
process of identifying waters protected
under the CWA clearer, simpler, and
faster. Chief Justice Roberts’
concurrence in Rapanos underscores
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the importance of this rulemaking
effort.5 In this final rule, the agencies are
responding to those requests from across
the country to make the process of
identifying waters protected under the
CWA easier to understand, more
predictable, and more consistent with
the law and peer-reviewed science.
The agencies proposed a rule
clarifying the scope of waters of the
United States April 21, 2014 (79 FR
22188), and solicited comments for over
200 days. This final rule reflects the
over 1 million public comments on the
proposal, the substantial majority of
which supported the proposed rule, as
well as input provided through the
agencies’ extensive public outreach
effort, which included over 400
meetings nationwide with states, small
businesses, farmers, academics, miners,
energy companies, counties,
municipalities, environmental
organizations, other federal agencies,
and many others. The agencies sought
comment on a number of approaches to
specific jurisdictional questions, and
many of these commenters and
stakeholders urged EPA to improve
upon the April 2014 proposal, by
providing more bright line boundaries
and simplifying definitions that identify
waters that are protected under the
CWA, all for the purpose of minimizing
delays and costs, making protection of
clean water more effective, and
improving predictability and
consistency for landowners and
regulated entities.
The agencies’ interpretation of the
CWA’s scope in this final rule is guided
by the best available peer-reviewed
science—particularly as that science
informs the determinations as to which
waters have a ‘‘significant nexus’’ with
traditional navigable waters, interstate
waters, or the territorial seas.
The relevant science on the
relationship and downstream effects of
waters has advanced considerably in
recent years. A comprehensive report
prepared by the EPA’s Office of
Research and Development entitled
‘‘Connectivity of Streams and Wetlands
to Downstream Waters: A Review and
Synthesis of the Scientific Evidence’’ 6
5 Chief Justice Roberts’ concurrence in Rapanos
emphasized that ‘‘[a]gencies delegated rulemaking
authority under a statute such as the Clean Water
Act are afforded generous leeway by the courts in
interpreting the statute they are entrusted to
administer.’’ Id. at 758. Chief Justice Roberts made
clear that, if the agencies had undertaken such a
rulemaking, ‘‘the Corps and the EPA would have
enjoyed plenty of room to operate in developing
some notion of an outer bound to the reach of their
authority.’’ Id. (Emphasis in original.)
6 U.S. Environmental Protection Agency,
Connectivity of Streams and Wetlands to
Downstream Waters: A Review and Synthesis of the
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(hereafter the Science Report)
synthesizes the peer-reviewed science.
The Science Report provides much of
the technical basis for this rule. The
Science Report is based on a review of
more than 1,200 peer-reviewed
publications. EPA’s Science Advisory
Board (SAB) conducted a
comprehensive technical review of the
Science Report and reviewed the
adequacy of the scientific and technical
basis of the proposed rule. The Science
Report and the SAB review confirmed
that:
• Waters are connected in myriad
ways, including physical connections
and the hydrologic cycle; however,
connections occur on a continuum or
gradient from highly connected to
highly isolated.
• These variations in the degree of
connectivity are a critical consideration
to the ecological integrity and
sustainability of downstream waters.
• The critical contribution of
upstream waters to the chemical,
physical, and biological integrity of
downstream waters results from the
accumulative contribution of similar
waters in the same watershed and in the
context of their functions considered
over time.
The Science Report and the SAB review
also confirmed that:
• Tributary streams, including
perennial, intermittent, and ephemeral
streams, are chemically, physically, and
biologically connected to downstream
waters, and influence the integrity of
downstream waters.
• Wetlands and open waters in
floodplains and riparian areas are
chemically, physically, and biologically
connected with downstream waters and
influence the ecological integrity of
such waters.
• Non-floodplain wetlands and open
waters provide many functions that
benefit downstream water quality and
ecological integrity, but their effects on
downstream waters are difficult to
assess based solely on the available
science.
Although these conclusions play a
critical role in informing the agencies’
interpretation of the CWA’s scope, the
agencies’ interpretive task in this rule—
determining which waters have a
‘‘significant nexus’’—requires scientific
and policy judgment, as well as legal
interpretation. The science
demonstrates that waters fall along a
gradient of chemical, physical, and
biological connection to traditional
Scientific Evidence (Final Report), EPA/600/R–14/
475F, (Washington, DC: U.S. Environmental
Protection Agency, (2015)). https://www.epa.gov/
ncea.
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navigable waters, and it is the agencies’
task to determine where along that
gradient to draw lines of jurisdiction
under the CWA. In making this
determination, the agencies must rely,
not only on the science, but also on
their technical expertise and practical
experience in implementing the CWA
during a period of over 40 years. In
addition, the agencies are guided, in
part, by the compelling need for clearer,
more consistent, and easily
implementable standards to govern
administration of the Act, including
brighter line boundaries where feasible
and appropriate.
Major Rule Provisions
In this final rule, the agencies define
‘‘waters of the United States’’ to include
eight categories of jurisdictional waters.
The rule maintains existing exclusions
for certain categories of waters, and
adds additional categorical exclusions
that are regularly applied in practice.
The rule reflects the agencies’ goal of
providing simpler, clearer, and more
consistent approaches for identifying
the geographic scope of the CWA. The
rule recognizes jurisdiction for three
basic categories: Waters that are
jurisdictional in all instances, waters
that are excluded from jurisdiction, and
a narrow category of waters subject to
case-specific analysis to determine
whether they are jurisdictional.
Decisions about waters in each of
these categories are based on the law,
peer-reviewed science, and the agencies’
technical expertise, and were informed
by public comments. This rule replaces
existing procedures that often depend
on individual, time-consuming, and
inconsistent analyses of the relationship
between a particular stream, wetland,
lake, or other water with downstream
waters. The agencies have greatly
reduced the extent of waters subject to
this individual review by carefully
incorporating the scientific literature
and by utilizing agency expertise and
experience to characterize the nature
and strength of the chemical, physical,
and biological connections between
upstream and downstream waters. The
result of applying this scientific analysis
is that the agencies can more effectively
focus the rule on identifying waters that
are clearly covered by the CWA and
those that are clearly not covered,
making the rule easier to understand,
consistent, and environmentally more
protective.
The jurisdictional categories reflect
the current state of the best available
science, and are based upon the law and
Supreme Court decisions. The agencies
will continue a transparent review of
the science, and learn from on-going
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experience and expertise as the agencies
implement the rule. If evolving science
and the agencies’ experience lead to a
need for action to alter the jurisdictional
categories, any such action will be
conducted as part of a rule-making
process.
The first three types of jurisdictional
waters, traditional navigable waters,
interstate waters, and the territorial seas,
are jurisdictional by rule in all cases.
The fourth type of water,
impoundments of jurisdictional waters,
is also jurisdictional by rule in all cases.
The next two types of waters,
‘‘tributaries’’ and ‘‘adjacent’’ waters, are
jurisdictional by rule, as defined,
because the science confirms that they
have a significant nexus to traditional
navigable waters, interstate waters, or
territorial seas. For waters that are
jurisdictional by rule, no additional
analysis is required.
The final two types of jurisdictional
waters are those waters found after a
case-specific analysis to have a
significant nexus to traditional
navigable waters, interstate waters, or
the territorial seas, either alone or in
combination with similarly situated
waters in the region. Justice Kennedy
acknowledged the agencies could
establish more specific regulations or
establish a significant nexus on a caseby-case basis, Rapanos at 782, and for
these waters the agencies will continue
to assess significant nexus on a casespecific basis.
The major elements of the final rule
are briefly summarized here.
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Traditional Navigable Waters, Interstate
Waters, Territorial Seas, and
Impoundments of Jurisdictional Waters
Consistent with existing regulations
and the April 2014 proposed rule, the
final rule includes traditional navigable
waters, interstate waters, territorial seas,
and impoundments of jurisdictional
waters in the definition of ‘‘waters of the
United States.’’ These waters are
jurisdictional by rule.
Tributaries
Previous definitions of ‘‘waters of the
United States’’ regulated all tributaries
without qualification. This final rule
more precisely defines ‘‘tributaries’’ as
waters that are characterized by the
presence of physical indicators of
flow—bed and banks and ordinary high
water mark—and that contribute flow
directly or indirectly to a traditional
navigable water, an interstate water, or
the territorial seas. The rule concludes
that such tributaries are ‘‘waters of the
United States.’’ The great majority of
tributaries as defined by the rule are
headwater streams that play an
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important role in the transport of water,
sediments, organic matter, nutrients,
and organisms to downstream waters.
The physical indicators of bed and
banks and ordinary high water mark
demonstrate that there is sufficient
volume, frequency, and flow in such
tributaries to a traditional navigable
water, interstate water, or the territorial
seas to establish a significant nexus.
‘‘Tributaries,’’ as defined, are
jurisdictional by rule.
The rule only covers as tributaries
those waters that science tells us
provide chemical, physical, or
biological functions to downstream
waters and that meet the significant
nexus standard. The agencies identify
these functions in the definition of
‘‘significant nexus’’ at paragraph (c)(5).
Features not meeting this legal and
scientific test are not jurisdictional
under this rule. The rule continues the
current policy of regulating ditches that
are constructed in tributaries or are
relocated tributaries or, in certain
circumstances drain wetlands, or that
science clearly demonstrates are
functioning as a tributary. These
jurisdictional waters affect the chemical,
physical, and biological integrity of
downstream waters. The rule further
reduces existing confusion and
inconsistency regarding the regulation
of ditches by explicitly excluding
certain categories of ditches, such as
ditches that flow only after
precipitation. Further, the rule
explicitly excludes from the definition
of ‘‘waters of the United States’’
erosional features, including gullies,
rills, and ephemeral features such as
ephemeral streams that do not have a
bed and banks and ordinary high water
mark.
Adjacent Waters
The agencies determined that
‘‘adjacent waters,’’ as defined in the
rule, have a significant nexus to
traditional navigable waters, interstate
waters, and the territorial seas based
upon their hydrological and ecological
connections to, and interactions with,
those waters. Under this final rule,
‘‘adjacent’’ means bordering,
contiguous, or neighboring, including
waters separated from other ‘‘waters of
the United States’’ by constructed dikes
or barriers, natural river berms, beach
dunes and the like. Further, waters that
connect segments of, or are at the head
of, a stream or river are ‘‘adjacent’’ to
that stream or river. ‘‘Adjacent waters’’
include wetlands, ponds, lakes, oxbows,
impoundments, and similar water
features. However, it is important to
note that ‘‘adjacent waters’’ do not
include waters that are subject to
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established normal farming, silviculture,
and ranching activities as those terms
are used in Section 404(f) of the CWA.
The final rule establishes a definition
of ‘‘neighboring’’ for purposes of
determining adjacency. In the rule, the
agencies identify three circumstances
under which waters would be
‘‘neighboring’’ and therefore ‘‘waters of
the United States’’:
(1) Waters located in whole or in part
within 100 feet of the ordinary high
water mark of a traditional navigable
water, interstate water, the territorial
seas, an impoundment of a
jurisdictional water, or a tributary, as
defined in the rule.
(2) Waters located in whole or in part
in the 100-year floodplain and that are
within 1,500 feet of the ordinary high
water mark of a traditional navigable
water, interstate water, the territorial
seas, an impoundment, or a tributary, as
defined in the rule (‘‘floodplain
waters’’).
(3) Waters located in whole or in part
within 1,500 feet of the high tide line of
a traditional navigable water or the
territorial seas and waters located
within 1,500 feet of the ordinary high
water mark of the Great Lakes.
The agencies emphasize that the rule
has defined as ‘‘adjacent waters’’ those
waters that currently available science
demonstrates possess the requisite
connection to downstream waters and
function as a system to protect the
chemical, physical, or biological
integrity of those waters. The agencies
also emphasize that the rule does not
cover ‘‘adjacent waters’’ that are
otherwise excluded. Further, the
agencies recognize the establishment of
bright line boundaries in the rule for
adjacency does not in any way restrict
states from considering state specific
information and concerns, as well as
emerging science to evaluate the need to
more broadly protect their waters under
state law. The CWA establishes both
national and state roles to ensure that
states specific circumstances are
properly considered to complement and
reinforce actions taken at the national
level.
‘‘Adjacent’’ waters as defined are
jurisdictional by rule. The agencies
recognize that there are individual
waters outside of the ‘‘neighboring’’
boundaries stated above where the
science may demonstrate through a
case-specific analysis that there exists a
significant nexus to a downstream
traditional navigable water, interstate
water, or the territorial seas. However,
these waters are not determined
jurisdictional by rule and will be
evaluated through a case-specific
analysis. The strength of the science and
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the significance of the nexus will be
established on a case-specific basis as
described below.
Case-Specific Significant Nexus
The rule identifies particular waters
that are not jurisdictional by rule but are
subject to case-specific analysis to
determine if a significant nexus exists
and the water is a ‘‘water of the United
States.’’ This category of case-specific
waters is based upon available science
and the law, and in response to public
comments that encouraged the agencies
to ensure more consistent
determinations and reduce the
complexity of conducting jurisdictional
determinations. Consistent with the
significant nexus standard articulated in
the Supreme Court opinions, waters are
‘‘waters of the United States’’ if they
significantly affect the chemical,
physical, or biological integrity of
traditional navigable waters, interstate
waters, or the territorial seas. This
determination will most typically be
made on a water individually, but can,
when warranted, be made in
combination with other waters where
waters function together.
In this final rule, the agencies have
identified by rule, five specific types of
waters in specific regions that science
demonstrates should be subject to a
significant nexus analysis and are
considered similarly situated by rule
because they function alike and are
sufficiently close to function together in
affecting downstream waters. These five
types of waters are Prairie potholes,
Carolina and Delmarva bays, pocosins,
western vernal pools in California, and
Texas coastal prairie wetlands.
Consistent with Justice Kennedy’s
opinion in Rapanos, the agencies
determined that such waters should be
analyzed ‘‘in combination’’ (as a group,
rather than individually) in the
watershed that drains to the nearest
traditional navigable water, interstate
water, or the territorial seas when
making a case-specific analysis of
whether these waters have a significant
nexus to traditional navigable waters,
interstate waters, or territorial seas.
The final rule also provides that
waters within the 100-year floodplain of
a traditional navigable water, interstate
water, or the territorial seas and waters
within 4,000 feet of the high tide line or
the ordinary high water mark of a
traditional navigable water, interstate
water, the territorial seas,
impoundments, or covered tributary are
subject to case-specific significant nexus
determinations, unless the water is
excluded under paragraph (b) of the
rule. The science available today does
not establish that waters beyond those
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defined as ‘‘adjacent’’ should be
jurisdictional as a category under the
CWA, but the agencies’ experience and
expertise indicate that there are many
waters within the 100-year floodplain of
a traditional navigable water, interstate
water, or the territorial seas or out to
4,000 feet where the science
demonstrates that they have a
significant effect on downstream waters.
In circumstances where waters within
the 100-year floodplain of a traditional
navigable water, interstate water, or the
territorial seas or within 4,000 feet of
the high tide line or ordinary high water
mark are subject to a case-specific
significant nexus analysis and such
waters may be evaluated as ‘‘similarly
situated,’’ it must be first demonstrated
that these waters function alike and are
sufficiently close to function together in
affecting downstream waters. The
significant nexus analysis must then be
conducted based on consideration of the
functions provided by those waters in
combination in the point of entry
watershed. A ‘‘similarly situated’’
analysis is conducted where it is
determined that there is a likelihood
that there are waters that function
together to affect downstream water
integrity. To provide greater clarity and
transparency in determining what
functions will be considered in
determining what constitutes a
significant nexus, the final rule lists
specific functions that the agencies will
consider.
In establishing both the 100-year
floodplain and the 4,000 foot bright line
boundaries for these case-specific
significant nexus determinations in the
rule, the agencies are carefully applying
the available science. Consistent with
the CWA, the agencies will work with
the states in connection with the
prevention, reduction and elimination
of pollution from state waters. The
agencies will work with states to more
closely evaluate state-specific
circumstances that may be present
within their borders and, as appropriate,
encourage states to develop rules that
reflect their circumstances and emerging
science to ensure consistent and
effective protection for waters in the
states. As is the case today, nothing in
this rule restricts the ability of states to
more broadly protect state waters.
Exclusions
All existing exclusions from the
definition of ‘‘waters of the United
States’’ are retained, and several
exclusions reflecting longstanding
agency practice are added to the
regulation for the first time.
Prior converted cropland and waste
treatment systems have been excluded
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from the definition of ‘‘waters of the
United States’’ definition since 1992
and 1979 respectively, and continue to
be excluded. Ministerial changes are
made for purposes of clarity, but these
two exclusions remain substantively
and operationally unchanged. The
agencies add exclusions for waters and
features previously identified as
generally exempt (e.g., exclusion for
certain ditches that are not located in or
drain wetlands) in preamble language
from Federal Register documents by the
Corps on November 13, 1986, and by
EPA on June 6, 1988. This is the first
time these exclusions have been
established by rule. The agencies for the
first time also establish by rule that
certain ditches are excluded from
jurisdiction, including ditches with
ephemeral flow that are not a relocated
tributary or excavated in a tributary, and
ditches with intermittent flow that are
not a relocated tributary, or excavated in
a tributary, or drain wetlands. The
agencies add exclusions for
groundwater and erosional features, as
well as exclusions for some waters that
were identified in public comments as
possibly being found jurisdictional
under proposed rule language where
this was never the agencies’ intent, such
as stormwater control features
constructed to convey, treat, or store
stormwater, and cooling ponds that are
created in dry land. These exclusions
reflect the agencies’ current practice,
and their inclusion in the rule as
specifically excluded furthers the
agencies’ goal of providing greater
clarity over what waters are and are not
protected under the CWA.
Role of States and Tribes Under the
Clean Water Act
States and tribes play a vital role in
the implementation and enforcement of
the CWA. Section 101(b) of the CWA
states that it is Congressional policy to
preserve the primary responsibilities
and rights of states to prevent, reduce,
and eliminate pollution, to plan the
development and use of land and water
resources, and to consult with the
Administrator with respect to the
exercise of the Administrator’s authority
under the CWA.
Of particular importance, states and
tribes may be authorized by the EPA to
administer the permitting programs of
CWA sections 402 and 404. Forty-six
states and the U.S. Virgin Islands are
authorized to administer the NPDES
program under section 402, while two
states administer the section 404
program. The CWA identifies the waters
over which states may assume section
404 permitting jurisdiction. See CWA
section 404(g)(1). The scope of waters
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that are subject to state and tribal
permitting is a separate inquiry and
must be based on the statutory language
in CWA section 404. States administer
approved CWA section 404 programs for
‘‘waters of the United States’’ within the
state, except those waters remaining
under Corps jurisdiction pursuant to
CWA section 404(g)(1) as identified in a
Memorandum of Agreement between
the state and the Corps. 40 CFR 233.14;
40 CFR 233.70(c)(2); 40 CFR
233.71(d)(2). EPA has initiated a
separate process to address how the
EPA can best clarify assumable waters
for dredged and fill material permit
programs pursuant to the Clean Water
Act section 404(g)(1). 80 FR 13539 (Mar.
16, 2015). Additional CWA programs
that utilize the definition of ‘‘waters of
the United States’’ and are of
importance to the states and tribes
include the section 311 oil spill
prevention and response program, the
water quality standards and total
maximum daily load (TMDL) programs
under section 303, and the section 401
state water quality certification process.
States and federally-recognized tribes,
consistent with the CWA, retain full
authority to implement their own
programs to more broadly and more
fully protect the waters in their
jurisdiction. Under section 510 of the
CWA, unless expressly stated, nothing
in the CWA precludes or denies the
right of any state to establish more
protective standards or limits than the
Federal CWA. Congress has also
provided roles for eligible Indian tribes
to administer CWA programs over their
reservations and expressed a preference
for tribal regulation of surface water
quality on Indian reservations to ensure
compliance with the goals of the CWA.
See 33 U.S.C. 1377; 56 FR 64876,
64878–79 (Dec. 12, 1991)). Tribes also
have inherent sovereign authority to
establish more protective standards or
limits than the Federal CWA. Where
appropriate, references to states in this
document may also include eligible
tribes. Many states and tribes, for
example, regulate groundwater, and
some others protect wetlands that are
vital to their environment and economy
but outside the jurisdiction of the CWA.
Nothing in this rule limits or impedes
any existing or future state or tribal
efforts to further protect their waters. In
fact, providing greater clarity regarding
what waters are subject to CWA
jurisdiction will reduce the need for
permitting authorities, including the
states and tribes with authorized section
402 and 404 CWA permitting programs,
to make jurisdictional determinations
on a case-specific basis.
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Overview of the Preamble
The remainder of this preamble is
organized as follows. Section III
(Significant Nexus Standard) provides
additional background on the rule,
including a discussion of Supreme
Court precedent, the science
underpinning the rule, and the agencies’
overall interpretive approach to
applying the significant nexus standard.
Section IV (Definition of Waters of the
United States) explains the provisions of
the final rule, including subsections on
each of the major elements of the rule.
Section V summarizes the economic
analysis of the rule and Section VI
addresses Related Acts of Congress,
Executive Orders and Agency
Initiatives.
III. Significant Nexus Standard
With this rule, the agencies interpret
the scope of the ‘‘waters of the United
States’’ for the CWA in light of the goals,
objectives, and policies of the statute,
the Supreme Court case law, the
relevant and available science, and the
agencies’ technical expertise and
experience. The key to the agencies’
interpretation of the CWA is the
significant nexus standard, as
established and refined in Supreme
Court opinions: Waters are ‘‘waters of
the United States’’ if they, either alone
or in combination with similarly
situated waters in the region,
significantly affect the chemical,
physical, or biological integrity of
traditional navigable waters, interstate
waters, or the territorial seas. The
agencies interpret specific aspects of the
significant nexus standard in light of the
science, the law, and the agencies’
technical expertise: The scope of the
region in which to evaluate waters when
making a significant nexus
determination; the waters to evaluate in
combination with each other; and the
functions provided by waters and
strength of those functions, and when
such waters significantly affect the
chemical, physical, or biological
integrity of the downstream traditional
navigable waters, interstate waters, or
the territorial seas.
In the rule, the agencies determine
that tributaries, as defined (‘‘covered
tributaries’’), and ‘‘adjacent waters’’, as
defined (‘‘covered adjacent waters’’),
have a significant nexus to downstream
traditional navigable waters, interstate
waters, and the territorial seas and
therefore are ‘‘waters of the United
States.’’ In the rule, the agencies also
establish that defined sets of additional
waters may be determined to have a
significant nexus on a case-specific
basis: (1) Five specific types of waters
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that the agencies conclude are
‘‘similarly situated’’ and therefore must
be analyzed ‘‘in combination’’ in the
watershed that drains to the nearest
traditional navigable water, interstate
water, or the territorial seas when
making a case-specific significant nexus
analysis; and (2) waters within the 100year floodplain of a traditional
navigable water, interstate water, or the
territorial seas, or waters within 4,000
feet of the high tide line or ordinary
high water mark of traditional navigable
waters, interstate waters, the territorial
seas, impoundments or covered
tributaries. The rule establishes a
definition of significant nexus, based on
Supreme Court opinions and the
science, to use when making these casespecific determinations.
Significant nexus is not a purely
scientific determination. The opinions
of the Supreme Court have noted that as
the agencies charged with interpreting
the statute, EPA and the Corps must
develop the outer bounds of the scope
of the CWA, while science does not
provide bright line boundaries with
respect to where ‘‘water ends’’ for
purposes of the CWA. Therefore, the
agencies’ interpretation of the CWA is
informed by the Science Report and the
review and comments of the SAB, but
not dictated by them. With this context,
this section addresses, first, the
Supreme Court case law and the
significant nexus standard, second, the
relevant scientific conclusions reached
by analysis of existing scientific
literature, and third, the agencies’
significant nexus determinations
underpinning the rule. Section IV of the
preamble addresses in more detail the
precise definitions of the covered waters
promulgated by the agencies to provide
the bright line boundaries identifying
‘‘waters of the United States.’’
A. The Significant Nexus Standard
Congress enacted the CWA ‘‘to restore
and maintain the chemical, physical,
and biological integrity of the Nation’s
waters.’’ Section 101(a). The agencies’
longstanding regulations define ‘‘waters
of the United States’’ for purposes of the
Clean Water Act, and the Supreme
Court has addressed the scope of
‘‘waters of the United States’’ protected
by the CWA in three cases. The
significant nexus standard evolved
through those cases.
In United States v. Riverside Bayview
Homes, 474 U.S. 121 (1985) (Riverside),
which involved wetlands adjacent to a
traditional navigable water in Michigan,
the Court, in a unanimous opinion,
deferred to the Corps’ ecological
judgment that adjacent wetlands are
‘‘inseparably bound up’’ with the waters
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to which they are adjacent, and upheld
the inclusion of adjacent wetlands in
the regulatory definition of ‘‘waters of
the United States.’’ Id. at 134. The Court
observed that the broad objective of the
CWA to restore and maintain the
integrity of the Nation’s waters
‘‘incorporated a broad, systemic view of
the goal of maintaining and improving
water quality . . .. Protection of aquatic
ecosystems, Congress recognized,
demanded broad federal authority to
control pollution, for ‘[w]ater moves in
hydrologic cycles and it is essential that
discharge of pollutants be controlled at
the source.’ In keeping with these views,
Congress chose to define the waters
covered by the Act broadly.’’ Id. at 132–
33 (citing Senate Report No. 92–414).
The Court also recognized that ‘‘[i]n
determining the limits of its power to
regulate discharges under the Act, the
Corps must necessarily choose some
point at which water ends and land
begins. Our common experience tells us
that this is often no easy task: The
transition from water to solid ground is
not necessarily or even typically an
abrupt one. Rather, between open
waters and dry land may lie shallows,
marshes, mudflats, swamps, bogs—in
short, a huge array of areas that are not
wholly aquatic but nevertheless fall far
short of being dry land. Where on this
continuum to find the limit of ‘waters’
is far from obvious.’’ Id. The Court then
deferred to the agencies’ interpretation:
‘‘In view of the breadth of federal
regulatory authority contemplated by
the Act itself and the inherent
difficulties of defining precise bounds to
regulable waters, the Corps’ ecological
judgment about the relationship
between waters and their adjacent
wetlands provides an adequate basis for
a legal judgment that adjacent wetlands
may be defined as waters under the
Act.’’ Id. at 134.
The issue of CWA jurisdiction over
‘‘waters of the United States’’ was
addressed again by the Supreme Court
in Solid Waste Agency of Northern Cook
County v. U.S. Army Corps of Engineers,
531 U.S. 159 (2001) (SWANCC). In
SWANCC, the Court (in a 5–4 opinion)
held that the use of ‘‘isolated’’ nonnavigable intrastate ponds by migratory
birds was not by itself a sufficient basis
for the exercise of federal regulatory
authority under the CWA. The
SWANCC Court noted that in Riverside
it had ‘‘found that Congress’ concern for
the protection of water quality and
aquatic ecosystems indicated its intent
to regulate wetlands ‘inseparably bound
up’ with the ‘waters’ of the United
States’’ and that ‘‘[i]t was the significant
nexus between the wetlands and
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‘navigable waters’ that informed our
reading of the CWA’’ in that case. Id. at
167. SWANCC did not invalidate any
parts of the regulatory definition of
‘‘waters of the United States.’’
Five years after SWANCC, the Court
again addressed the term ‘‘waters of the
United States’’ in Rapanos v. United
States, 547 U.S. 715 (2006) (Rapanos).
Rapanos involved two consolidated
cases in which the CWA had been
applied to wetlands adjacent to nonnavigable tributaries of traditional
navigable waters. All Members of the
Court agreed that the term ‘‘waters of
the United States’’ encompasses some
waters that are not navigable in the
traditional sense. A four-Justice
plurality in Rapanos interpreted the
term ‘‘waters of the United States’’ as
covering ‘‘relatively permanent,
standing or continuously flowing bodies
of water . . .,’’ id. at 739, that are
connected to traditional navigable
waters, id. at 742, as well as wetlands
with a ‘‘continuous surface connection
. . .’’ to such water bodies, id. (Scalia,
J., plurality opinion). The Rapanos
plurality noted that its reference to
‘‘relatively permanent’’ waters did ‘‘not
necessarily exclude streams, rivers, or
lakes that might dry up in extraordinary
circumstances, such as drought,’’ or
‘‘seasonal rivers, which contain
continuous flow during some months of
the year but no flow during dry months.
. . .’’ Id. at 732 n.5 (emphasis in
original).
Justice Kennedy concurred that the
cases should be remanded for further
decision making, and stated that ‘‘to
constitute ‘navigable waters’ under the
Act, a water or wetland must possess a
‘significant nexus’ to waters that are or
were navigable in fact or that could
reasonably be so made.’’ Id. at 759
(citing SWANCC, 531 U.S. at 167, 172).
Justice Kennedy concluded that ‘‘The
required nexus must be assessed in
terms of the statute’s goals and
purposes. Congress enacted the law to
‘restore and maintain the chemical,
physical, and biological integrity of the
Nation’s waters,’ 33 U.S.C. 1251(a), and
it pursued that objective by restricting
dumping and filling in ‘navigable
waters,’ §§ 1311(a), 1362(12).’’ Id. at
779. He concluded that wetlands
possess the requisite significant nexus if
the wetlands ‘‘either alone or in
combination with similarly situated
[wet]lands in the region, significantly
affect the chemical, physical, and
biological integrity of other covered
waters more readily understood as
‘navigable.’ ’’ 547 U.S. at 780. Justice
Kennedy’s opinion notes that such a
relationship with navigable waters must
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be more than ‘‘speculative or
insubstantial.’’ Id. at 780.
While Justice Kennedy’s opinion
focused on adjacent wetlands in light of
the facts of the cases before him, his
opinion is clear that a significant nexus
is the basis for jurisdiction to protect
non-navigable waters and wetlands
under the CWA (id. at 759), and there
is no indication in his opinion that the
analytical framework his opinion
provides for determining significant
nexus for adjacent wetlands is limited to
adjacent wetlands. In addition, the four
dissenting Justices in Rapanos, who
would have affirmed the court of
appeals’ application of the agencies’
regulation, also concluded that the term
‘‘waters of the United States’’
encompasses, inter alia, all tributaries
and wetlands that satisfy ‘‘either the
plurality’s [standard] or Justice
Kennedy’s.’’ Id. at 810 & n.14 (Stevens,
J., dissenting). Neither the plurality nor
the Kennedy opinion invalidated any of
the current regulatory provisions
defining ‘‘waters of the United States.’’
Chief Justice Roberts’ concurrence in
Rapanos emphasized that ‘‘[a]gencies
delegated rulemaking authority under a
statute such as the Clean Water Act are
afforded generous leeway by the courts
in interpreting the statute they are
entrusted to administer.’’ Id. at 758.
Chief Justice Roberts made clear that, if
the agencies had undertaken such a
rulemaking, ‘‘the Corps and the EPA
would have enjoyed plenty of room to
operate in developing some notion of an
outer bound to the reach of their
authority.’’ Id. (Emphasis in original.)
The agencies utilize the significant
nexus standard, as articulated by Justice
Kennedy’s opinion and informed by the
unanimous opinion in Riverside
Bayview and the plurality opinion in
Rapanos which all recognize that the
Act and the agencies must identify the
scope of CWA jurisdiction ‘‘on this
continuum to find the limit of ‘waters,’ ’’
Riverside Bayview at 132, to interpret
the scope of the statutory term ‘‘waters
of the United States.’’ While a
significant nexus determination is
primarily weighted in the scientific
evidence and criteria, the agencies also
consider the statutory language, the
statute’s goals, objectives and policies,
the case law, and the agencies’ technical
expertise and experience when
interpreting the terms of the CWA.
B. Science Report
EPA’s Office of Research and
Development prepared the Science
Report, a peer-reviewed compilation
and analysis of published peer-reviewed
scientific literature summarizing the
current scientific understanding of the
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connectivity of and mechanisms by
which streams and wetlands, singly or
in combination, affect the chemical,
physical, and biological integrity of
downstream waters. The final Science
Report is available in the docket and at
https://cfpub.epa.gov/ncea/cfm/
recordisplay.cfm?deid=296414.
The process for developing the
Science Report followed standard
information quality guidelines for EPA.
In September 2013, EPA released a draft
of the Science Report for an
independent SAB review and invited
submissions of public comments for
consideration by the SAB panel. In
October 2014, after several public
meetings and hearings, the SAB
completed its peer review of the draft
Science Report. The SAB was highly
supportive of the draft Science Report’s
conclusions regarding streams, riparian
and floodplain wetlands, and open
waters, and recommended strengthening
the conclusion regarding non-floodplain
waters to include a more definitive
statement that reflects how numerous
functions of such waters sustain the
integrity of downstream waters.7 The
final peer review report is available on
the SAB Web site, as well as in the
docket for this rulemaking. EPA revised
the draft Science Report based on
comments from the public and
recommendations from the SAB panel.
The SAB was established in 1978 by
the Environmental Research,
Development, and Demonstration
Authorization Act (ERDDAA), to
provide independent scientific and
technical advice to the EPA
Administrator on the technical basis for
Agency positions and regulations.
Advisory functions include peer review
of EPA’s technical documents, such as
the Science Report. At the time the peer
review was completed, the chartered
SAB was comprised of more than 50
members from a variety of sectors
including academia, non-profit
organizations, foundations, state
governments, consulting firms, and
industry. To conduct the peer review,
EPA’s SAB staff formed an ad hoc panel
based on nominations from the public to
serve as the primary reviewers. The
panel consisted of 27 technical experts
in an array of relevant fields, including
hydrology, wetland and stream ecology,
biology, geomorphology,
biogeochemistry, and freshwater
science. Similar to the chartered SAB,
the panel members represented sectors
7 U.S. EPA. 2014. SAB review of the draft EPA
report Connectivity of Streams and Wetlands to
Downstream Waters: A Review and Synthesis of the
Scientific Evidence. EPA–SAB–15–001, U.S.
Environmental Protection Agency, Washington, DC.
(‘‘SAB 2014a.’’)
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including academia, a federal
government agency, non-profit
organizations, and consulting firms. The
chair of the panel was a member of the
chartered SAB.
The SAB process is open and
transparent, consistent with the Federal
Advisory Committee Act, 5 U.S.C., App
2, and agency policies regarding Federal
advisory committees. Consequently, the
SAB has an approved charter, which
must be renewed biennially, announces
its meetings in the Federal Register, and
provides opportunities for public
comment on issues before the Board.
The SAB staff announced via the
Federal Register that they sought public
nominations of technical experts to
serve on the expert panel: SAB Panel for
the Review of the EPA Water Body
Connectivity Report (via a similar
process the public also is invited to
nominate chartered SAB members). 78
FR 15012 (Mar. 8, 2013). The SAB staff
then invited the public to comment on
the list of candidates for the panel. Once
the panel was selected, the SAB staff
posted a memo on its Web site
addressing the formation of the panel
and the set of determinations that were
necessary for its formation (e.g., no
conflicts of interest). In the public
notice of the first public meetings
interested members of the public were
invited to submit relevant comments for
the SAB Panel to consider pertaining to
the review materials, including the
charge to the Panel. Over 133,000 public
comments were received by the Docket.
Every meeting was open to the public,
noticed in the Federal Register, and had
time allotted for the public to present
their views. In total, the Panel held a
two-day in-person meeting in
Washington, DC, in December 2013, and
three four-hour public teleconferences
in April, May, and June 2014. The SAB
Panel also compiled four draft versions
of its peer review report to inform and
assist the meeting deliberations that
were posted on the SAB Web site. In
September 2014, the chartered SAB
conducted a public teleconference to
conduct the quality review of the
Panel’s final draft peer review report.
The peer review report was approved at
that meeting, and revisions were made
to reflect the chartered SAB’s review.
The culmination of that public process
was the release of the final peer review
report in October 2014. All meeting
minutes and draft reports are available
on the SAB Web site for public access.
The final Science Report states that
connectivity is a foundational concept
in hydrology and freshwater ecology.
Connectivity is the degree to which
components of a system are joined, or
connected, by various transport
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mechanisms and is determined by the
characteristics of both the physical
landscape and the biota of the specific
system. Connectivity for purposes of
interpreting the scope of ‘‘waters of the
United States’’ under the CWA serves to
demonstrate the ‘‘nexus’’ between
upstream water bodies and the
downstream traditional navigable water,
interstate water, or the territorial sea.
The scientific literature does not use the
term ‘‘significant’’ as it is defined in a
legal context, but it does provide
information on the strength of the
effects on the chemical, physical, and
biological functioning of the
downstream water bodies from the
connections among covered tributaries,
covered adjacent waters, and casespecific waters and those downstream
waters. The scientific literature also
does not use the terms traditional
navigable waters, interstate waters, or
the territorial seas. However, evidence
of strong chemical, physical, and
biological connections to larger rivers,
estuaries, and lakes applies to that
subset of rivers, estuaries, and lakes that
are traditional navigable waters,
interstate waters, or the territorial seas.
The Science Report presents evidence
of those connections from various
categories of waters, evaluated singly or
in combination, which affect
downstream waters and the strength of
that effect. The objectives of the Science
Report are (1) to provide a context for
considering the evidence of connections
between downstream waters and their
tributary waters, and (2) to summarize
current understanding about these
connections, the factors that influence
them, and the mechanisms by which the
connections affect the function or
condition of downstream waters. The
connections and mechanisms discussed
in the Science Report include transport
of physical materials and chemicals
such as water, wood, sediment,
nutrients, pesticides, and mercury;
functions that covered adjacent waters
perform, such as storing and cleansing
water; movement of organisms or their
seeds and eggs; and hydrologic and
biogeochemical interactions occurring
in and among surface and groundwater
flows, including hyporheic zones 8 and
alluvial aquifers.
The Science Report presents five
major conclusions:
8 The hyporheic zone is the subsurface area
immediately below the bed of intermittent and
ephemeral streams that remains wet even when
there is no surface flow. These areas are extremely
important to macro-benthic organisms critical to the
bio-chemical integrity of streams.
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Conclusion 1: Streams
The scientific literature unequivocally
demonstrates that streams, individually
or cumulatively, exert a strong influence
on the chemical, physical, and
biological integrity of downstream
waters. All tributary streams, including
perennial, intermittent, and ephemeral
streams, are chemically, physically, and
biologically connected to downstream
rivers via channels and associated
alluvial deposits where water and other
materials are concentrated, mixed,
transformed, and transported. Streams
are the dominant source of water in
most rivers, and the majority of
tributaries are perennial, intermittent, or
ephemeral headwater streams.
Headwater streams also convey water
into local storage compartments such as
ponds, shallow aquifers, and
floodplains, and into regional and
alluvial aquifers; these local storage
compartments are important sources of
water for maintaining baseflow in rivers.
In addition to water, streams transport
sediment, wood, organic matter,
nutrients, chemical contaminants, and
many of the organisms found in rivers.
The scientific literature provides robust
evidence that streams are biologically
connected to downstream waters by the
dispersal and migration of aquatic and
semiaquatic organisms, including fish,
amphibians, plants, microorganisms,
and invertebrates, that use both
upstream and downstream habitats
during one or more stages of their life
cycles, or provide food resources to
downstream communities. In addition
to material transport and biological
connectivity, ephemeral, intermittent,
and perennial flows influence
fundamental biogeochemical processes
by connecting channels and shallow
groundwater with other landscape
elements. Chemical, physical, and
biological connections between streams
and downstream waters interact via
integrative processes such as nutrient
spiraling. This occurs when stream
communities assimilate and chemically
transform large quantities of nitrogen
and other nutrients that otherwise
would be transported directly
downstream, thereby increasing nutrient
loads and associated impairments due
to excess nutrients in downstream
waters. Science Report at ES–2.
Conclusion 2: Riparian/Floodplain
Wetlands and Open Waters
The scientific literature clearly shows
that wetlands and open waters in
riparian areas and floodplains are
chemically, physically, and biologically
integrated with rivers via functions that
improve downstream water quality,
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including the temporary storage and
deposition of channel-forming sediment
and woody debris, temporary storage of
local groundwater that supports
baseflow in rivers, and transformation
and transport of stored organic matter.
Riparian/floodplain wetlands and open
waters improve water quality through
the assimilation, transformation, and
sequestration of pollutants, including
excess nutrients and chemical
contaminants such as pesticides and
metals that can degrade downstream
water integrity. In addition to providing
effective buffers to protect downstream
waters from point source and nonpoint
source pollution, these systems form
integral components of river food webs,
providing nursery habitat for breeding
fish and amphibians, colonization
opportunities for stream invertebrates,
and maturation habitat for stream
insects. Lateral expansion and
contraction of the river in its floodplain
result in an exchange of organic matter
and organisms, including fish
populations that are adapted to use
floodplain habitats for feeding and
spawning during high water, that are
critical to river ecosystem function.
Riparian/floodplain wetlands and open
waters also affect the integrity of
downstream waters by subsequently
releasing (desynchronizing) floodwaters
and retaining large volumes of
stormwater, sediment, and
contaminants in runoff that could
otherwise negatively affect the
condition or function of downstream
waters. Science Report at ES–2 to
ES–3.
Conclusion 3: Non-Floodplain Wetlands
and Open Waters
Wetlands and open waters in nonfloodplain landscape settings (‘‘nonfloodplain wetlands’’) provide
numerous functions that benefit
downstream water integrity. These
functions include storage of floodwater;
recharge of groundwater that sustains
river baseflow; retention and
transformation of nutrients, metals, and
pesticides; export of organisms or seeds
to downstream waters; and habitats
needed for stream species. This diverse
group of wetlands (e.g., many Prairie
potholes or vernal pools) can be
connected to downstream waters
through surface water, shallow
subsurface water, and groundwater
flows, and through biological and
chemical connections.
In general, connectivity of nonfloodplain wetlands occurs along a
gradient, and can be described in terms
of the frequency, duration, magnitude,
timing, and rate of change of water,
material, and biotic fluxes to
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downstream waters. These descriptors
are influenced by climate, geology, and
terrain, which interact with factors such
as the magnitudes of the various
functions within wetlands (e.g., amount
of water storage or carbon export) and
their proximity to downstream waters to
determine where wetlands occur along
the connectivity gradient. At one end of
this gradient, the functions of nonfloodplain wetlands clearly affect the
condition of downstream waters if a
visible (e.g., channelized) surface water
or a regular shallow subsurface-water
connection to the river network is
present. For non-floodplain wetlands
lacking a channelized surface or regular
shallow subsurface connection (i.e.,
those at intermediate points along the
gradient of connectivity),
generalizations about their specific
effects on downstream waters from the
available literature are difficult because
information on both function and
connectivity is needed. Science Report
at ES–3.
Conclusion 4: Degrees and Determinants
of Connectivity
Connectivity of streams and wetlands
to downstream waters occurs along a
gradient that can be described in terms
of the frequency, duration, magnitude,
timing, and rate of change of water,
material, and biotic fluxes to
downstream waters. These terms, which
we refer to collectively as connectivity
descriptors, characterize the range over
which streams and wetlands vary and
shift along the connectivity gradient in
response to changes in natural and
anthropogenic factors and, when
considered in a watershed context, can
be used to predict probable effects of
different degrees of connectivity over
time. The evidence unequivocally
demonstrates that the stream channels
and riparian/floodplain wetlands or
open waters that together form river
networks are clearly connected to
downstream waters in ways that
profoundly influence downstream water
integrity. The connectivity and effects of
non-floodplain wetlands and open
waters are more variable and thus more
difficult to address solely from evidence
available in peer-reviewed studies.
Science Report at ES–3 to ES–4.
Conclusion 5: Cumulative Effects
The incremental effects of individual
streams and wetlands are cumulative
across entire watersheds, and therefore,
must be evaluated in context with other
streams and wetlands. Downstream
waters are the time-integrated result of
all waters contributing to them. For
example, the amount of water or
biomass contributed by a specific
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ephemeral stream in a given year might
be small, but the aggregate contribution
of that stream over multiple years, or by
all ephemeral streams draining that
watershed in a given year or over
multiple years, can have substantial
consequences on the integrity of the
downstream waters. Similarly, the
downstream effect of a single event,
such as pollutant discharge into a single
stream or wetland, might be negligible
but the cumulative effect of multiple
discharges could degrade the integrity of
downstream waters.
When considering the effect of an
individual stream or wetland, all
contributions and functions of that
stream or wetland should be evaluated
cumulatively. For example, the same
stream transports water, removes excess
nutrients, transports pollutants,
mitigates flooding, and provides refuge
for fish when conditions downstream
are unfavorable; if any of these
functions is ignored, the overall effect of
that stream would be underestimated.
Science Report at ES–5 to ES–6.
SAB Review of the Proposed Rule
In addition to its peer review of the
draft Science Report, in a separate effort
the SAB also reviewed the adequacy of
the scientific and technical basis of the
proposed rule and provided its advice
and comments on the proposal in
September 2014.9 The same SAB Panel
that reviewed the draft Science Report
met via two public teleconferences in
August 2014 to discuss the scientific
and technical basis of the proposed rule.
The Panel submitted comments to the
Chair of the chartered SAB. A work
group of chartered SAB members
considered comments provided by
panel members, agency representatives,
and the public on the adequacy of the
science informing the rule. This work
group then led the September 2014
public teleconference discussion of the
chartered SAB. The public had an
opportunity to submit oral or written
comments during these two public
meetings. The SAB’s final letter to the
EPA Administrator can be found on the
SAB Web site and in the docket for this
rule.
The SAB found that the available
science provides an adequate scientific
basis for the key components of the
proposed rule. The SAB noted that
although water bodies differ in degree of
connectivity that affects the extent of
9 U.S. EPA. 2014. SAB Consideration of the
Adequacy of the Scientific and Technical Basis of
the EPA’s Proposed Rule titled ‘‘Definition of
Waters of the United States under the Clean Water
Act.’’ EPA–SAB–14–007, U.S. Environmental
Protection Agency, Washington, DC. (‘‘SAB
2014b.’’)
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influence they exert on downstream
waters (i.e., they exist on a
‘‘connectivity gradient’’), the available
science supports the conclusion that the
types of water bodies identified as
‘‘waters of the United States’’ in the
proposed rule exert strong influence on
the chemical, physical, and biological
integrity of downstream waters. In
particular, the SAB expressed support
for the proposed rule’s inclusion of
tributaries and ‘‘adjacent waters’’ as
categorical waters of the United States
and the inclusion of ‘‘other waters’’ on
a case-specific basis, though noting that
certain ‘‘other waters’’ can be
determined as a subcategory to be
similarly situated.
Regarding tributaries, the SAB found,
‘‘[t]here is strong scientific evidence to
support the EPA’s proposal to include
all tributaries within the jurisdiction of
the Clean Water Act. Tributaries, as a
group, exert strong influence on the
physical, chemical, and biological
integrity of downstream waters, even
though the degree of connectivity is a
function of variation in the frequency,
duration, magnitude, predictability, and
consequences of physical, chemical, and
biological processes.’’ The Board
advised EPA to reconsider the definition
of tributaries because not all tributaries
have ordinary high water marks (e.g.,
ephemeral streams with arid and semiarid environments or in low gradient
landscapes where the flow of water is
unlikely to cause an ordinary high water
mark). The SAB also advised EPA to
consider changing the wording in the
definition to ‘‘bed, bank, and other
evidence of flow.’’ SAB 2014b at 2. The
agencies did not make this change
because this recommendation seemed to
suggest that any hydrologic connection
is sufficient for CWA jurisdiction. The
definition of ‘‘tributary’’ in the rule
better identifies tributaries that have a
significant nexus to downstream
traditional navigable waters, interstate
waters, or the territorial seas. In
addition, the SAB suggested that EPA
reconsider whether flow-through lentic
systems should be included as ‘‘adjacent
waters’’ and wetlands, rather than as
tributaries.
Regarding ‘‘adjacent waters’’ and
wetlands, the SAB stated, ‘‘[t]he
available science supports the EPA’s
proposal to include ‘‘adjacent waters’’
and wetlands as a waters of the United
States. . . . because [they] have a strong
influence on the physical, chemical, and
biological integrity of navigable waters.’’
Id. In particular, the SAB noted, ‘‘the
available science supports defining
adjacency or determination of adjacency
on the basis of functional
relationships,’’ rather than ‘‘solely on
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the basis of geographical proximity or
distance to jurisdictional waters.’’ Id. at
2–3. The agencies have determined
which waters are adjacent, and thus
jurisdictional under the rule, based on
both functional relationships and
proximity because those factors identify
the waters that have a strong influence
on the chemical, physical, or biological
integrity of traditional navigable waters,
interstate waters, or the territorial seas.
Section C. and IV.F below. The
agencies’ determination is informed by
the science, and consideration of
proximity is reasonable in interpreting
the scope of adjacency.
In the evaluation of ‘‘other waters,’’
the SAB found that ‘‘scientific literature
has established that ‘other waters’ can
influence downstream waters,
particularly when considered in
aggregate.’’ Id. at 3. The SAB thus found
it ‘‘appropriate to define ‘other waters’
as waters of the United States on a caseby-case basis, either alone or in
combination with similarly situated
waters in the same region.’’ Id. The SAB
found that distance could not be the
sole indicator used to evaluate the
connection of ‘‘other waters’’ to
jurisdictional waters. The agencies’
identification of the areas within which
a water is assessed on a case-specific
basis for a significant nexus is informed
by the science and the agencies’
experience and technical expertise, and
consideration of proximity is reasonable
in interpreting the scope of the statute.
The SAB also expressed support for
language in one of the options discussed
in the preamble to the proposed rule.
Specifically, the SAB stated there is
‘‘also adequate scientific evidence to
support a determination that certain
subcategories and types of ‘other waters’
in particular regions of the United States
(e.g., Carolina and Delmarva Bays, Texas
coastal prairie wetlands, prairie
potholes, pocosins, western vernal
pools) are similarly situated (i.e., they
have a similar influence on the
chemical, physical, and biological
integrity of downstream waters and are
similarly situated on the landscape) and
thus could be considered waters of the
United States.’’ Id. The Board noted that
other sets of wetlands could be
identified as ‘‘similarly situated’’ as the
science continues to develop and that
science does not support excluding
groups of ‘‘other waters’’ or
subcategories thereof from jurisdiction.
The exclusions paragraph of the
proposed rule generated the most
comments from the SAB. The SAB
noted, ‘‘[t]he Clean Water Act
exclusions of groundwater and certain
other exclusions listed in the proposed
rule and the current regulation do not
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have scientific justification.’’ Id. With
regard to ditches, the Board found that
there is a lack of scientific knowledge to
determine whether ditches should be
categorically excluded. For example,
some ditches that would be excluded in
the Midwest may drain Cowardin
wetlands and may provide certain
ecosystem services, while gullies, rills,
and non-wetland swales can be
important conduits for moving water
between jurisdictional waters. The SAB
also noted that artificial lakes or ponds,
or reflection pools, can be directly
connected to jurisdictional waters via
either shallow or deep groundwater.
The SAB also recommended that the
agencies clarify in the preamble to the
final rule that ‘‘significant nexus’’ is a
legal term, not a scientific one.
C. Significant Nexus Conclusions
As noted earlier, the agencies
interpret the scope of ‘‘waters of the
United States’’ protected under the
CWA based on the information and
conclusions in the Science Report, other
relevant scientific literature, the
Technical Support Document that
provides additional legal and scientific
discussion for issues raised in this rule,
the relevant Supreme Court decisions,
the agencies’ technical expertise and
experience, and the objectives and
requirements of the CWA. In light of
this information, the agencies made
scientifically and technically informed
judgments about the nexus between the
relevant waters and the significance of
that nexus and conclude that
‘‘tributaries’’ and ‘‘adjacent waters,’’
each as defined by the rule, have a
significant nexus such that they are
‘‘waters of the United States’’ and no
additional analysis is required. The
agencies also determined that additional
waters may, on a case-specific basis,
have a significant nexus to traditional
navigable waters, interstate waters, and
the territorial seas, either alone or in
combination with similarly situated
waters. The agencies’ interpretation of
the scope of ‘‘waters of the United
States’’ is informed by the Science
Report and the review and comments of
the SAB. The rule reflects the judgment
of the agencies in balancing the science,
the agencies’ expertise, and the
regulatory goals of providing clarity to
the public while protecting the
environment and public health,
consistent with the law.
Since the Rapanos decision, the
agencies have gained extensive
experience making significant nexus
determinations, and that experience and
expertise has informed the judgment of
the agencies as reflected in the
provisions of the rule. The agencies,
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most often the Corps, have made more
than 400,000 CWA jurisdictional
determinations since 2008. Of those,
more than 120,000 are case-specific
significant nexus determinations. The
agencies made determinations in every
state in the country, from the arid West
to the tropics of Hawaii, from the
Appalachian Mountains in the East to
the lush forests of the Northwest. With
field staff located in 38 Corps District
offices and 10 EPA regional offices, the
agencies have almost a decade of
nationwide experience in making
significant nexus determinations. These
individual jurisdictional determinations
have been made for waters ranging from
an intermittent stream that provides
flow to a drinking water source, to a
group of floodplain wetlands in North
Dakota that provide important
protection from floodwaters to
downstream communities alongside the
Red River, to headwater mountain
streams that provide high quality water
that supplies baseflow and reduces the
harmful concentrations of pollutants in
the main part of the river below.
Through this experience, the agencies
developed wide-ranging technical
expertise in assessing the hydrologic
flowpaths along which water and
materials are transported and
transformed that determine the degree
of chemical, physical, or biological
connectivity, as well as the variations in
climate, geology, and terrain within and
among watersheds and over time that
affect the functions (such as the removal
or transformation of pollutants)
performed by streams and wetlands for
downstream traditional navigable
waters, interstate waters or the
territorial seas.
The agencies utilize many tools and
many sources of information to help
make jurisdictional determinations,
including U.S. Geological Survey
(USGS) and state and local topographic
maps, aerial photography, soil surveys,
watershed studies, scientific literature
and references, and field work. For
example, USGS and state and local
stream maps and datasets, aerial
photography, gage data, watershed
assessments, monitoring data, and field
observations are often used to help
assess the contributions of flow of
tributary streams, including intermittent
and ephemeral streams, to downstream
traditional navigable waters, interstate
waters or the territorial seas. Similarly,
floodplain and topographic maps of
federal, state and local agencies,
modeling tools, and field observations
can be used to assess how wetlands are
trapping floodwaters that might
otherwise affect downstream waters.
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Further, the agencies utilize the large
body of scientific literature regarding
the functions of tributaries, including
tributaries with ephemeral, intermittent
and perennial flow and of wetlands and
open waters to inform their evaluations
of significant nexus. In addition, the
agencies have experience and expertise
for decades prior to and since the
SWANCC and Rapanos decisions with
making jurisdictional determinations,
and consider hydrology, ordinary high
water mark, biota, and other technical
factors in implementing Clean Water
Act programs. This immersion in the
science along with the practical
expertise developed through casespecific determinations across the
country and in diverse settings is
reflected in the agencies’ conclusions
with respect to waters that have a
significant nexus, as well as where the
agencies have drawn boundaries
demarking where ‘‘waters of the United
States’’ end.
1. Scope of Significant Nexus Analysis
Under the significant nexus standard,
waters possess the requisite significant
nexus if they ‘‘either alone or in
combination with similarly situated
[wet]lands in the region, significantly
affect the chemical, physical, and
biological integrity of other covered
waters more readily understood as
‘navigable.’ ’’ Rapanos at 780. Several
terms in this standard were not defined.
In this rule the agencies interpret these
terms and the scope of ‘‘waters of the
United States’’ based on the goals,
objectives, and policies of the statute,
the scientific literature, the Supreme
Court opinions, and the agencies’
technical expertise and experience.
Therefore, for purposes of a significant
nexus analysis, the agencies have
determined (1) which waters are
‘‘similarly situated,’’ and thus should be
analyzed in combination, in (2) the
‘‘region,’’ for purposes of a significant
nexus analysis, and (3) the types of
functions that should be analyzed to
determine if waters significantly affect
the chemical, physical, or biological
integrity of traditional navigable waters,
interstate waters, or the territorial seas.
These determinations underpin many of
the key elements of the rule and are
reflected in the definition of ‘‘significant
nexus’’ in the rule.
a. Similarly Situated Waters
As reflected in the rule’s definition of
‘‘significant nexus,’’ the agencies
determined that it is reasonable to
consider waters as ‘‘similarly situated’’
where they function alike and are
sufficiently close to function together in
affecting the nearest traditional
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navigable water, interstate water, or the
territorial sea. Since the focus of the
significant nexus standard is on
protecting and restoring the chemical,
physical, and biological integrity of the
nation’s waters, the agencies interpret
the phrase ‘‘similarly situated’’ in terms
of whether particular waters are
providing common, or similar, functions
for downstream waters such that it is
reasonable to consider their effect
together. Regarding covered tributaries
and covered adjacent waters, the
agencies define each water type such
that the functions provided are similar
and the waters are situated so as to
provide those functions together to
affect downstream waters.
The science demonstrates that
covered tributaries provide many
common vital functions important to the
chemical, physical, and biological
integrity of downstream waters,
regardless of the size of the tributaries.
The science also supports the
conclusion that sufficient volume,
duration, and frequency of flow are
required to create a bed and banks and
ordinary high water mark. The science
also supports the conclusion that
tributaries function together to affect
downstream waters. The agencies
conclude that covered tributaries with a
bed and banks and ordinary high water
mark are similarly situated for purposes
of the agencies’ significant nexus
analysis.
For covered adjacent waters, the
science demonstrates that these waters
provide many similar vital functions to
downstream waters, and the agencies
defined ‘‘adjacent waters’’ with distance
boundaries to ensure that the waters are
providing similar functions to
downstream waters and that the waters
are located comparably in the region
such that the agencies’ reasonably
judged them to be similarly situated.
For waters for which a case-specific
significant nexus determination is
required the agencies have determined
that some waters in specific regions are
similarly situated; for other specified
waters, the determination of whether
there are any other waters providing
similar functions in a similar situation
in the region must be made as part of
a case-specific determination. See
section IV.H.
Assessing the functions of identified
waters in combination is consistent not
only with Justice Kennedy’s significant
nexus standard, but with the science.
Scientists routinely combine the effects
of groups of waters, aggregating the
known effect of one water with those of
ecologically similar waters in a specific
geographic area, or to a certain scale.
This is because the chemical, physical,
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and biological integrity of downstream
waters is directly related to the
aggregate contribution of upstream
waters that flow into them, including
any tributaries and connected wetlands.
As a result, the scientific literature and
the Science Report consistently
document that the health of larger
downstream waters is directly related to
the aggregate health of waters located
upstream, including waters such as
wetlands that may not be hydrologically
connected but function together to
ameliorate the potential impacts of
flooding and pollutant contamination
from affecting downstream waters. See
Technical Support Document.
For example, excess nutrients
discharged into small tributary streams
in the aggregate can cause algal blooms
downstream that reduce dissolved
oxygen levels and increase turbidity in
traditional navigable waters, interstate
waters, and the territorial seas. Water
low in dissolved oxygen cannot support
aquatic life. This widely-recognized
phenomenon, known as hypoxia, has
impacted commercial and recreational
fisheries in the northern Gulf of Mexico.
In this instance, the cumulative effects
of nutrient export from the many small
headwater streams of the Mississippi
River have resulted in large-scale
ecological and economically harmful
impacts hundreds of miles downstream.
See Technical Support Document.
In review of the scientific and
technical adequacy of the rule, the SAB
panel members ‘‘generally agreed that
aggregating ‘similarly situated’ waters is
scientifically justified, given that the
combined effects of these waters on
downstream waters are often only
measurable in aggregate.’’ 10 As stated in
section III.B. above, one of the main
conclusions of the Science Report is that
the incremental contributions of
individual streams and wetlands are
cumulative across entire watersheds,
and their effects on downstream waters
should be evaluated within the context
of other streams and wetlands in that
watershed. For example, the Science
Report finds, ‘‘[t]he amount of nutrients
removed by any one stream over
multiple years or by all headwater
streams in a watershed in a given year
can have substantial consequences for
downstream waters.’’ Science Report at
1–11. Cumulative effects of streams,
wetlands, and open waters across a
watershed must be considered because
10 September 2, 2014. Memorandum from Dr.
Amanda Rodewald to Dr. David Allen. Comments
to the chartered SAB on the Adequacy of the
Scientific and Technical Basis of the EPA’s
Proposed Rule titled ‘‘Definition of ‘Waters of the
United States’ under the Clean Water Act.’’ (‘‘SAB
2014c.’’)
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‘‘[t]he downstream consequences (e.g.,
the amount and quality of materials that
eventually reach a river) are determined
by the aggregate effect of contributions
and sequential alterations that begin at
the source waters and function along
continuous flowpaths to the watershed
outlet.’’ Id. at 1–19.
The agencies conclude that it is
appropriate to assess the effects of
waters in combination based on the
similarity of the functions they provide
to the downstream water and their
location in the watershed. This is
consistent with the science and
effectively meets the goals of the CWA.
b. In the Region
Since Justice Kennedy did not define
the ‘‘region,’’ the agencies determined
that the single point of entry watershed
is a reasonable and technically
appropriate scale for identifying ‘‘in the
region’’ for purposes of the significant
nexus standard. A single point of entry
watershed is the drainage basin within
whose boundaries all precipitation
ultimately flows to the nearest single
traditional navigable water, interstate
water, or the territorial sea. The agencies
determined that because the movement
of water from watershed drainage basins
to coastal waters, river networks, and
lakes shapes the development and
function of these systems in a way that
is critical to their long-term health, the
watershed is a reasonable and
technically appropriate way to identify
the scope of waters that together may
have an effect on the chemical, physical,
or biological integrity of a particular
traditional navigable water, interstate
water, or territorial sea. The watershed
includes all streams, wetlands, lakes,
and open waters within its boundaries.
Using the watershed that flows to the
nearest single traditional navigable
water, interstate water, or territorial sea
is consistent with court decisions that
these waters are the ultimate focus of
CWA protections. Using the single point
of entry watershed ensures that any
analysis of significant nexus is
appropriately connected to these
touchstone waters.
Because the movement of water from
watershed drainage basins to coastal
waters, river networks, and lakes shapes
the development and function of these
systems in a way that is critical to their
integrity, using a watershed as the
framework for conducting significant
nexus evaluations is scientifically
supportable. Watersheds are generally
regarded as the most appropriate spatial
unit for water resource management.
Anthropogenic actions and natural
events can have widespread effects
within the watershed that collectively
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impact the integrity and quality of the
relevant traditional navigable water,
interstate water, or the territorial sea.
The functions of the contributing waters
are inextricably linked and have a
cumulative effect on the integrity of the
downstream traditional navigable water,
interstate water, or the territorial sea.
For these reasons, it is more appropriate
to conduct a significant nexus analysis
at the watershed scale than to focus on
a specific site, such as an individual
stream segment. See proposal Appendix
A, Scientific Analysis, 79 FR 22246,
April 21, 2014, Science Report, and
Technical Support Document.
Concluding that the watershed is the
reasonable and appropriate region for
purposes of a significant nexus analysis
is also consistent with the agencies’
longstanding practice and experience.
To restore or maintain the health of the
downstream affected water, the
agencies’ standard practice is to
evaluate the condition of the waters that
are in the contributing watersheds and
to develop a plan to address the issues
of concern. The Corps has used
watershed framework approaches for
water sources, for navigation
approaches for more than 100 years, and
in the regulatory program since its
inception. Also, using a watershed
framework is consistent with more than
two decades of practice by EPA and
many other governmental, academic,
and additional entities that recognize
that a watershed approach is the most
effective framework to address water
resource challenges. Finally, the
watershed that drains to the nearest (i.e.,
first downstream) traditional navigable
water, interstate water, or the territorial
seas is likely to be of a size commonly
understood as a ‘‘region.’’
In light of the scientific literature, the
longstanding approach of the agencies’
implementation of the CWA, and the
statutory goals underpinning Justice
Kennedy’s significant nexus framework,
the watershed draining to the nearest
traditional navigable water, interstate
water, or the territorial sea, is the
appropriate ‘‘region’’ for a significant
nexus analysis. See the proposed rule
preamble and Technical Support
Document.
c. Significantly Affect Chemical,
Physical, or Biological Integrity
The agencies’ definition of the term
‘‘significant nexus’’ in the rule is
consistent with language in Riverside
Bayview, SWANCC, and Rapanos, and
with the goals, objectives, and policies
of the CWA. The definition reflects that
not all waters have a requisite
connection to traditional navigable
waters, interstate waters, or the
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territorial seas sufficient to be
determined jurisdictional. Justice
Kennedy was clear that to be covered,
waters must significantly affect the
chemical, physical, or biological
integrity of a downstream navigable
water and that the requisite nexus must
be more than ‘‘speculative or
insubstantial,’’ Rapanos, at 780. The
agencies define significant nexus in
precisely those terms. Under the rule a
‘‘significant nexus’’ is established by a
showing of a significant chemical,
physical, or biological effect. In
characterizing the significant nexus
standard, Justice Kennedy stated: ‘‘[t]he
required nexus must be assessed in
terms of the statute’s goals and
purposes. Congress enacted the [CWA]
to ‘restore and maintain the chemical,
physical, and biological integrity of the
Nation’s waters’. . . .’’ 547 U.S. at 779.
It is clear that Congress intended the
CWA to ‘‘restore and maintain’’ all three
forms of ‘‘integrity,’’ Section 101(a), so
if any one is compromised then that is
contrary to the statute’s stated objective.
It would subvert the objective if the
CWA only protected waters upon a
showing that they had effects on every
attribute of the integrity of a traditional
navigable water, interstate water, or the
territorial sea.
In the rule’s definition of ‘‘significant
nexus,’’ the agencies identify the
functions that waters provide that can
significantly affect the chemical,
physical, or biological integrity of
traditional navigable waters, interstate
waters and the territorial seas. In
identifying the functions to be
considered the agencies were informed
by the goals of the statute and the
available science. Among the means to
achieve the CWA’s objective to restore
and maintain the chemical, physical,
and biological integrity of the Nation’s
waters, Congress established an interim
national goal to achieve wherever
possible ‘‘water quality which provides
for the protection and propagation of
fish, shellfish, and wildlife and provides
for recreation in and on the water.’’
Section 101(a)(2). Functions to be
considered for the purposes of
determining significant nexus are
sediment trapping; nutrient recycling;
pollutant trapping, transformation,
filtering, and transport; retention and
attenuation of floodwaters; runoff
storage; contribution of flow; export of
organic matter; export of food resources;
and provision of life-cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning,
and use as a nursery area) for species
located in traditional navigable waters,
interstate waters, or the territorial seas.
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The effect of an upstream water can be
significant even when a water, alone or
in combination, is providing a subset, or
even just one, of the functions listed.
Science demonstrates that these
aquatic functions provided by smaller
streams, ponds, wetlands and other
waters are important for protecting the
chemical, physical, and biological
integrity of downstream traditional
navigable waters, interstate waters, and
the territorial seas. For example, States
identify sediment and nutrients as the
primary contaminants in the nation’s
waters. Sediment storage and export via
streams to downstream waters is critical
for maintaining the river network,
including the formation of channel
features. Although sediment is essential
to river systems, excess sediment can
impair ecological integrity by filling
interstitial spaces, reducing channel
capacity, blocking sunlight transmission
through the water column, and
increasing contaminant and nutrient
concentrations. Streams and wetlands
can prevent excess deposits of sediment
downstream and reduce pollutant
concentrations in downstream waters.
Thus the function of trapping of excess
sediment, along with export of
sediment, have a significant effect on
the chemical, physical, and biological
integrity of downstream waters.
Nutrient recycling results in the
uptake and transformation of large
quantities of nitrogen and other
nutrients that otherwise would be
transported directly downstream,
thereby decreasing nutrient loads and
associated impairments due to excess
nutrients in downstream waters.
Streams, wetlands and open waters
improve water quality through the
assimilation, transformation, or
sequestration of pollutants, including
excess nutrients and chemical
contaminants such as pesticides and
metals that can degrade downstream
water integrity. Nutrient transport
exports nutrients downstream and can
degrade water quality and lead to stream
impairments. Nutrients are necessary to
support aquatic life, but excess nutrients
lead to excessive plant growth and
hypoxia, in which over-enrichment
causes dissolved oxygen concentrations
to fall below the level necessary to
sustain most aquatic animal life in the
downstream waters. Nutrient recycling,
retention, and export can significantly
affect downstream chemical integrity by
impacting downstream water quality.
The contribution of flow downstream
is an important role, as upstream waters
can be a cumulative source of the
majority of the total mean annual flow
to bigger downstream rivers and waters,
including via the recharge of baseflow.
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Streams, wetlands, and open waters
contribute surface and subsurface water
downstream, and are the dominant
sources of water in most rivers.
Contribution of flow can significantly
affect the physical integrity of
downstream waters, helping to sustain
the volume of water in larger waters.
Small streams and wetlands are
particularly effective at retaining and
attenuating floodwaters. By
subsequently releasing
(desynchronizing) floodwaters and
retaining large volumes of stormwater
that could otherwise negatively affect
the condition or function of downstream
waters, streams and adjacent wetlands
and open waters affect the physical
integrity of downstream traditional
navigable waters, interstate waters, or
the territorial seas. This function can
reduce flood peaks downstream and can
also maintain downstream river
baseflows by recharging alluvial
aquifers.
Streams, wetlands, and open waters
supply downstream waters with
dissolved and particulate organic matter
(e.g., leaves, wood), which support
biological activity throughout the river
network. In addition to organic matter,
streams, wetlands, and open waters can
also export other food resources
downstream, such as aquatic insects
that are the food source for fish in
downstream waters. The export of
organic matter and food resources
downstream is important to maintaining
the food webs and thus the biological
integrity of traditional navigable waters,
interstate waters, and the territorial seas.
Streams, wetlands, and open waters
provide life-cycle dependent aquatic
habitat (such as foraging, feeding,
nesting, breeding, spawning, and use as
a nursery area) for species located in
traditional navigable waters, interstate
waters, or the territorial seas. Many
species require different habitats for
different resources (e.g., food, spawning
habitat, overwintering habitat), and thus
move throughout the river network over
their life-cycles. For example,
headwater streams can provide refuge
habitat under adverse conditions,
enabling fish to persist and recolonize
downstream areas once conditions have
improved. These upstream systems form
integral components of downstream
food webs, providing nursery habitat for
breeding fish and amphibians,
colonization opportunities for stream
invertebrates, and maturation habitat for
stream insects, including for species
that are critical to downstream
ecosystem function. The provision of
life-cycle dependent aquatic habitat for
species located in downstream waters
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significantly affects the biological
integrity of those downstream waters.
Tributaries, adjacent wetlands, and
open waters can perform multiple
functions, including functions that
change depending upon the season. For
example, the same stream can
contribute flow when
evapotranspiration is low and can retain
water when evapotranspiration is high.
These functions, particularly when
considered in aggregate with the
functions of similarly situated waters in
the region, can significantly affect the
chemical, physical, or biological
integrity of a traditional navigable
water, interstate water, or the territorial
seas. When considering the effect of an
individual stream, wetland, or open
water, all contributions and functions
that the water provides should be
evaluated cumulatively. For example,
the same wetland retains sediment,
removes excess nutrients, mitigates
flooding, and provides habitat for
amphibians that also live downstream;
if any of these functions is ignored, the
overall effect of that wetland would be
underestimated. It is important to note,
however, that a water or wetland can
provide just one function that may
significantly affect the chemical,
physical or biological integrity of the
downstream water.
2. Categories of Waters Determined to
Have a Significant Nexus
In this rule, the agencies determine
that: (1) Covered tributaries, in
combination with other covered
tributaries located in a watershed that
drains to a traditional navigable water,
interstate water, or the territorial seas,
significantly affect the chemical,
physical, and biological integrity of that
water; and (2) covered adjacent waters,
in combination with other covered
adjacent waters located in a watershed
that drains to a traditional navigable
water, interstate water, or the territorial
seas, significantly affect the chemical,
physical, and biological integrity of that
water.
a. Covered Tributaries
The agencies determine based on their
scientific and technical expertise that
waters meeting the definition of
‘‘tributary’’ in a single point of entry
watershed are similarly situated and
have a significant nexus because they
significantly affect the chemical,
physical, or biological integrity of
traditional navigable waters, interstate
waters, and the territorial seas. As such,
it is appropriate to conclude covered
tributaries as a category are ‘‘waters of
the United States.’’ See Technical
Support Document. The agencies
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limited the tributaries that are ‘‘waters
of the United States’’ to those that have
both a bed and banks and another
indicator of ordinary high water mark.
That limitation served as a reasonable
basis to consider covered tributaries
similarly situated because those
physical characteristics indicated
sufficient flow that the covered
tributaries are performing similar
functions and located such that they are
working together in the region to
provide those functions to the nearest
traditional navigable water, interstate
water, or the territorial seas. Justice
Kennedy noted that the requirement of
a perceptible ordinary high water mark
for tributaries, a measure that had been
used by the Corps, ‘‘may well provide
a reasonable measure of whether
specific minor tributaries bear a
sufficient nexus with other regulated
waters to constitute ‘navigable waters’
under the Act.’’ 547 U.S. at 781, see also
id. at 761. The science supports this.
The agencies analyzed the Science
Report and other scientific literature to
determine whether tributaries to
traditional navigable waters, interstate
waters, or the territorial seas have a
significant nexus to constitute ‘‘waters
of the United States’’ under the Act such
that it is reasonable to assert CWA
jurisdiction over all such tributaries by
rule. Covered tributaries have a
significant impact on the chemical,
physical, or biological integrity of
waters into which they eventually
flow—for CWA purposes, traditional
navigable waters, interstate waters, and
the territorial seas. The great majority of
covered tributaries are headwater
streams, and whether they are
perennial, intermittent, or ephemeral,
they play an important role in the
transport of water, sediments, organic
matter, nutrients, and organisms to
downstream waters. Covered tributaries
serve to store water, thereby reducing
flooding; provide biogeochemical
functions that help maintain water
quality; trap and transport sediments;
transport, store and modify pollutants;
provide habitat for plants and animals;
and sustain the biological productivity
of downstream rivers, lakes, and
estuaries. Such waters have these
significant effects whether they are
natural, modified, or constructed.
Covered tributaries significantly affect
the chemical integrity of traditional
navigable waters, interstate waters, and
the territorial seas. Covered tributaries
influence the chemical composition of
downstream waters, through the
transport and removal of chemical
elements and compounds, such as
nutrients, ions, organic matter and
pollutants. Ecosystem processes in
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covered tributaries transform, remove,
and transport these substances to
downstream waters. In turn, these
chemical compounds can influence
water quality, sediment deposition,
nutrient availability, and biotic
functions in rivers. Because water flow
transports chemical substances
downstream, chemical effects are
closely related to hydrological
connectivity. Within covered tributaries,
there are processes that occur that
transform and export nutrients and
carbon to downstream waters, serving
important source functions that
influence the chemical integrity of
downstream waters. Organic carbon, in
both dissolved and particulate forms,
exported from covered tributaries is
consumed by downstream organisms.
The organic carbon that is exported
downstream thus supports biological
activity throughout the river network.
Covered tributaries act as both sinks
and sources of chemical substances,
further affecting the chemical integrity
of traditional navigable waters,
interstate waters, and the territorial seas.
Covered tributaries provide sink
functions by trapping chemicals through
absorption to sediments in the stream
substrate (e.g., phosphorous adsorption
to clay particles). They provide source
functions by transporting chemicals to
downstream traditional navigable
waters, interstate waters, and the
territorial seas as chemicals dissolved in
the waters or as chemicals attached to
suspended sediments.
Covered tributaries significantly affect
the physical integrity of traditional
navigable waters, interstate waters, and
the territorial seas. Physical connections
between covered tributaries and
traditional navigable waters, interstate
waters, and the territorial seas result
from the hydrologic transport from
covered tributaries to downstream
waters of numerous materials, including
water, sediment and organic matter such
as leaves and wood. This transport
affects the physical characteristics of
downstream waters. Covered tributaries,
even when seasonally dry, are the
dominant source of water in most rivers,
rather than direct precipitation or
groundwater input to main stem river
segments. One of the primary functions
of covered tributaries is transporting
sediment to downstream waters.
Covered tributaries, particularly
headwaters, shape and maintain river
channels by accumulating and gradually
or episodically releasing sediment and
large woody debris into river channels.
These effects occur even when the
covered tributaries flow infrequently
(such as ephemeral covered tributaries),
and even when the covered tributaries
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are great distances from the traditional
navigable water, interstate water, or the
territorial sea (such as some headwater
covered tributaries).
Covered tributaries significantly affect
the biological integrity of traditional
navigable waters, interstate waters, and
the territorial seas. Covered tributaries,
including intermittent and ephemeral
streams, are critical in the life-cycles of
many organisms capable of moving
throughout river networks. In fact, many
organisms, such as anadromous salmon,
have complex life-cycles which involve
migration through the river network,
from headwaters to downstream rivers
and oceans and back, over the course of
their lives. In addition to providing
critical habitat for complex life-cycle
completion, covered tributaries provide
refuge from predators and adverse
physical conditions in rivers, and are
reservoirs of genetic- and species-level
diversity. Covered tributaries contribute
materials to downstream food networks
and supporting populations for aquatic
species, including economically
important species such as salmon.
These effects occur even when the
covered tributaries flow infrequently
(such as ephemeral covered tributaries),
and even when the covered tributaries
are large distances from the traditional
navigable waters, interstate waters, and
the territorial seas (such as some
headwater covered tributaries).
Similarly, modified and constructed
tributaries perform the same functions
as natural tributaries, especially the
conveyance of water that carries
nutrients, pollutants, and other
constituents, both good and bad, to
traditional navigable waters, interstate
waters, and the territorial seas. Modified
and constructed covered tributaries also
provide corridors for movement of
organisms between headwaters and
traditional navigable waters, interstate
waters, and the territorial seas. The
important effect—and thus the
significant nexus—between a covered
tributary and a traditional navigable
water, interstate water, and the
territorial sea is not broken where the
covered tributary flows through a
culvert or other structure. The scientific
literature recognizes that features that
convey water, whether they are natural,
modified, or constructed, provide
substantial connectivity between
streams and downstream waters. For
example, ditches that meet the
definition of tributary and are not
excluded quickly move water
downstream to traditional navigable
waters, interstate waters, and the
territorial seas due to their often
straightened and channelized nature,
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transporting downstream sediment,
nutrients, and other materials.
The CWA regulates and controls
pollution at its source, in part because
most pollutants do not remain at the site
of the discharge, but instead flow and
are washed downstream through the
tributary system to endanger drinking
water supplies, fisheries, and recreation
areas. These fundamental facts about the
movement of pollutants and the
interconnected nature of the tributary
system demonstrate why covered
tributaries of traditional navigable
waters, interstate waters, and the
territorial seas, alone or in combination
with other covered tributaries in a
watershed, have a significant nexus
with those downstream waters. Thus, in
the rule the agencies assert CWA
jurisdiction over all covered tributaries
as defined. Those covered tributaries are
‘‘waters of the United States’’ without
the need for further analysis.
b. Covered Adjacent Waters
Based on the agencies’ review of the
scientific literature and the law, the
agencies determine that covered
adjacent waters, as defined, have a
significant nexus and are ‘‘waters of the
United States.’’ The scientific literature,
including the Science Report,
consistently supports the conclusion
that covered adjacent waters provide
similar functions and work together to
maintain the chemical, physical, and
biological integrity of the downstream
traditional navigable waters, interstate
waters, and the territorial seas because
of their hydrological and ecological
connections to, and interactions with,
those waters. Science demonstrates that
this functional connectivity is
particularly evident where covered
adjacent waters are located within the
floodplain of the traditional navigable
water, interstate water, the territorial
seas, covered tributary, or impoundment
to which they are adjacent or are
otherwise sufficiently proximate to
waters with no floodplain, such as lakes
and ponds. Location within the
floodplain and proximity ensure that
the aquatic functions performed by
covered adjacent waters are effectively
and consistently provided to
downstream waters. See Technical
Support Document.
The agencies conclude that all waters
meeting the definition of ‘‘adjacent’’ in
the rule are similarly situated for
purposes of analyzing whether they
have a significant nexus to a traditional
navigable water, interstate water, or the
territorial sea. Based on a review of the
scientific literature, the agencies
conclude that these bordering,
contiguous, or neighboring waters
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provide similar functions and function
together to significantly affect the
chemical, physical, or biological
integrity of traditional navigable waters,
interstate waters, or the territorial seas.
Further, because the definition of
‘‘adjacent’’ considers both the functional
relationships and the proximity of the
waters (i.e., those that are located near
traditional navigable waters, interstate
waters, the territorial seas,
impoundments, and covered
tributaries), interpreting the term
‘‘similarly situated’’ to include all
covered adjacent waters, as defined in
the rule, is informed by the science and
is a reasonable interpretation of the
scope of the statute. The geographic
proximity of an ‘‘adjacent’’ water
relative to the traditional navigable
waters, interstate waters, the territorial
seas, impoundments, and covered
tributaries is indicative of the
relationship to it, with many of its
defining characteristics resulting from
the movement of materials and energy
between the categories of waters. The
scientific literature supports that waters,
including wetlands, ponds, lakes,
oxbow lakes, and similar waters, that
are ‘‘adjacent,’’ as defined in the rule, to
traditional navigable waters, interstate
waters, the territorial seas,
impoundments, and covered tributaries,
are integral parts of stream networks
because of their ecological functions
and how they interact with each other,
and with downstream traditional
navigable waters, interstate waters, or
the territorial seas.
Covered adjacent waters function
together to maintain the chemical,
physical, or biological health of
traditional navigable waters, interstate
waters, and the territorial seas to which
they are directly adjacent or to which
they are connected by the tributary
system. This functional interaction can
result from hydrologic connections or
because covered adjacent waters can act
as water storage areas holding damaging
floodwaters or filtering harmful
pollutants. These chemical, physical,
and biological connections affect the
integrity of downstream traditional
navigable waters, interstate waters, and
the territorial seas through the
temporary storage and deposition of
channel-forming sediment and woody
debris, temporary storage of local
groundwater sources of baseflow for
downstream waters and their tributaries,
and transformation and transport of
organic matter. Covered adjacent waters
improve water quality through the
assimilation, transformation, or
sequestration of pollutants, including
excess nitrogen and phosphorus, and
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chemical contaminants such as
pesticides and metals that can degrade
downstream water integrity. In addition
to providing effective buffers to protect
downstream waters from pollution,
covered adjacent waters form integral
components of downstream food webs,
providing nursery habitat for breeding
fish and amphibians, colonization
opportunities for stream invertebrates,
and maturation habitat for stream
insects. Covered adjacent waters serve
an important role in the integrity of
traditional navigable waters, interstate
waters, and the territorial seas by
subsequently releasing
(desynchronizing) floodwaters and
retaining large volumes of stormwater,
sediment, nutrients, and contaminants
that could otherwise negatively impact
the condition or function of traditional
navigable waters, interstate waters, and
the territorial seas.
Floodplain areas connect aquatic
environments through both surface and
shallow subsurface hydrologic
flowpaths. Waters in these areas are
therefore uniquely situated in
watersheds to receive and process water
that passes over densely vegetated areas
and through subsurface zones before
reaching streams and rivers. When
contaminants reach a floodplain water,
they can be sequestered in sediments,
assimilated into wetland plants and
animals, transformed into less harmful
and/or mobile forms or compounds, or
lost to the atmosphere. Wetlands located
in floodplains store large amounts of
sediment and organic matter from
upstream and upland areas. In addition,
the primary function of many floodplain
wetlands in the Western United States
is sediment exchange, which can
transform materials and compounds
temporarily on floodplains.
Wetlands and other similar waters in
floodplain areas act as buffers that are
among the most effective tools for
mitigating nonpoint source pollution.
The literature shows that collectively,
wetlands and other similar waters
improve water quality through
assimilation, transformation, or
sequestration of nutrients, sediment,
and other pollutants—such as pesticides
and metals—that can affect downstream
water quality. These pollutants enter
floodplain wetlands from dry and wet
atmospheric deposition, runoff from
upland agricultural and urban areas,
spray drift, subsurface water flows,
outfalls, pipes, and ditches.
Floodplain waters, including
wetlands, can reduce flood peaks by
storing and desynchronizing
floodwaters. They can also maintain
river baseflows by recharging alluvial
aquifers. Many studies have
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documented the ability of floodplain
wetlands to reduce flood pulses by
storing excess water from streams and
rivers. One review of wetland studies
reported that floodplain wetlands
reduced or delayed floods in 23 of 28
studies. For example, peak discharges
between upstream and downstream
gaging stations on the Cache River in
Arkansas were reduced 10–20 percent
primarily due to floodplain water
storage.
Ecosystem function within a river
system is driven by interactions
between the physical environment and
the diverse biological communities
living within the river system. Wetlands
in floodplains become important seed
sources for the river network, especially
if catastrophic flooding scours
vegetation and seed banks in other parts
of the channel. Movements of organisms
that connect aquatic habitats and their
populations, even across different
watersheds, are important for the
survival of individuals, populations,
and species, and for the functioning of
the river ecosystem. For example, lateral
expansion and contraction of the river
in its floodplain results in an exchange
of matter and organisms, including fish
populations that are adapted to use
floodplain habitat for feeding and
spawning during high water. The
organisms that live within the
hyporheic zone for these mid- and largesized river systems have a demonstrated
connection outward to several miles
within the floodplain. General field
practice observations further indicate
that covered adjacent waters with a
close proximity have a significant nexus
with the downstream waters.
Waters adjacent to impoundments
and covered tributaries are integrally
linked to the chemical, physical, and
biological functions of the waters to
which they are adjacent and, through
those waters, are integrally linked to the
chemical, physical, and biological
functions of the downstream traditional
navigable waters, interstate waters, or
the territorial seas. Thus, where waters
are adjacent to impoundments or
covered tributaries, they also have a
significant nexus to the downstream
traditional navigable waters, interstate
waters, or the territorial seas. The
important functions that covered
adjacent waters perform that impact
downstream traditional navigable
waters, interstate waters, and the
territorial seas and their integrated
behavior with the tributary system
demonstrate why all waters adjacent to
traditional navigable waters, interstate
waters, or the territorial seas as well as
impoundments and covered tributaries,
alone or in combination with other
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covered adjacent wetlands in a
watershed have a significant nexus with
those downstream waters.
Based on the science and their
technical expertise and experience, the
agencies determine it is appropriate to
protect all covered adjacent waters
because those waters are functioning as
an integrated system with the
downstream traditional navigable
waters, interstate waters, or the
territorial seas and significantly affect
such downstream waters. Consequently,
these waters are ‘‘adjacent’’ and
therefore ‘‘waters of the United States’’
under the CWA. Covered adjacent
waters are ‘‘waters of the United States’’
without the need for further analysis.
3. Case-Specific Significant Nexus
Determinations
a. Two Exclusive Circumstances for
Case-Specific Significant Nexus
Determinations
The rule identifies two exclusive
circumstances under which a significant
nexus determination is made on a casespecific basis to determine whether the
water is a ‘‘water of the United States.’’
First, there are five subcategories of
waters—Prairie potholes, Carolina and
Delmarva bays, pocosins, western vernal
pools in California, and Texas coastal
prairie wetlands—that the agencies
conclude must be analyzed ‘‘in
combination’’ as ‘‘similarly situated ’’
waters when making a case-specific
significant nexus analysis. Second, there
are waters for which the agencies have
made no conclusions with respect to
which waters are ‘‘similarly situated’’
but for which a case-specific significant
nexus analyses may be undertaken. The
rule establishes that case-specific
determinations may be made for waters
located within the 100-year floodplain
of a traditional navigable water,
interstate water, or the territorial seas,
and for waters located within 4,000 feet
from the high tide line or the ordinary
high water mark of traditional navigable
waters, interstate waters, the territorial
seas, impoundments, or tributaries.
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b. Summary of Rationale for ‘‘Similarly
Situated’’ Determinations
Based on the agencies’ expertise and
experience and available literature and
data, the agencies have determined that
waters in the five subcategories of
waters identified in paragraph (a)(7) are
similarly situated and must be
combined with other waters in the same
subcategory located in the same
watershed that drains to the nearest
traditional navigable water, interstate
water, or the territorial seas. See
Technical Support Document. The
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scientific literature shows that these
subcategories of waters are frequently
located together in a complex or are
otherwise closely co-located and
perform similar functions. The agencies
specifically sought comment in the
proposal on options to address these
five subcategories of waters, including
whether waters in these subcategories
should be found ‘‘similarly situated’’ by
rule.
Based on the body of scientific
literature regarding the subcategories of
waters specified in paragraph (a)(7) and
their functions, the agencies determined
that waters of the specified
subcategories are similarly situated
because they perform similar functions
and they are located sufficiently close to
each other to function together in
affecting downstream waters and
therefore reasonably be evaluated in
combination with regard to their effects
on the integrity of traditional navigable
waters, interstate waters, or the
territorial seas. The specified
subcategories of waters perform similar
functions as waters of the same
subcategory in the same single point of
entry watershed and collectively
function together to affect a traditional
navigable water, interstate water, or the
territorial seas. Among the functions
and relationships in the landscape the
agencies considered to conclude that the
subcategories are each similarly situated
are the physical capacity of the waters
to provide flood and sediment retention.
In determining that the waters in each
of the five subcategories are ‘‘similarly
situated,’’ the agencies concluded that
these subcategories of waters are colocated to each other or similar to the
tributary system such that they have
cumulative and additive effects on
pollutant removal through parallel,
serial, or sequential processing, such as
the role of pocosins in maintaining
water quality in estuaries. The
subcategories of waters are sufficiently
near each other or the tributary system
to function as an integrated habitat that
can support the life-cycle of a species or
more broadly provide habitat to a large
number of a single species.
The SAB expressed support for the
agencies’ option in the preamble of the
proposed rule to identify certain
subcategories of waters as similarly
situated and highlighted these same five
subcategories. It stated, ‘‘[t]here is also
adequate scientific evidence to support
a determination that certain
subcategories and types of ‘other waters’
in particular regions of the United States
(e.g., Carolina and Delmarva Bays, Texas
coastal prairie wetlands, prairie
potholes, pocosins, western vernal
pools) are similarly situated (i.e., they
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have a similar influence on the physical,
chemical and biological integrity of
downstream waters and are similarly
situated on the landscape) and thus
could be considered waters of the
United States. Furthermore, as the
science continues to develop, other sets
of wetlands may be identified as
‘similarly situated.’ ’’ SAB 2014b at 3.
The agencies concluded that the
specific subcategories of waters listed in
paragraph (a)(7) are similarly situated
for purposes of a case-specific
significant nexus based on the
following:
(i) Prairie potholes are a complex of
glacially formed wetlands, usually
occurring in depressions that lack
permanent natural outlets that are found
in the central United States and Canada.
In the United States, they are found
from central Iowa through western
Minnesota, Montana, eastern South
Dakota, and North Dakota. Prairie
potholes demonstrate a wide range of
hydrologic permanence; some hold
permanent standing water and others
are wet only in years with high
precipitation. This in turn influences
the diversity and structure of their
biological communities.
Prairie potholes generally accumulate
and retain water effectively due to the
low permeability of their underlying
soil, which can modulate flow
characteristics of nearby streams and
rivers. One of the most noted hydrologic
functions of Prairie potholes is water
storage. Because most of the water
outflow in Prairie potholes is via
evapotranspiration, Prairie potholes can
become water sinks, preventing flow to
downstream waters. Prairie potholes
also can accumulate chemicals in
overland flow, thereby reducing
chemical loading to other bodies of
water. When Prairie potholes are
artificially connected to streams and
lakes through drainage, they become
sources of water and chemicals to
downstream waters. Prairie potholes
also support a community of highly
mobile organisms, from plants to
invertebrates that move among Prairie
potholes and that can biologically
connect the entire complex to the river
network.
Prairie potholes can be highly
connected to other Prairie potholes via
shallow subsurface connections and via
surface hydrologic connections during
the wet season. They can also be
connected to the stream network via
surface and shallow subsurface
connections. Intense precipitation
events or high cumulative precipitation
over one or more seasons can result in
temporary hydrologic connectivity
between Prairie potholes and from
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Prairie potholes to the tributary system
via ‘‘fill-and-spill’’ events.
Their density across the landscape
varies from region to region as the result
of several factors, including patterns of
glacial movement, topography, and
climate. In some parts of the region,
prairie pothole density is very high.
Though their density varies across the
landscape, Prairie potholes often act as
a complex. They have similar functions
that can collectively impact downstream
waters.
Prairie potholes have been
determined to be similarly situated
based on the characteristics of Prairie
potholes, including their density on the
landscape, their interaction and
formation as a complex of wetlands and
open waters, their connections to each
other and the tributary network, and
their similar functions. In addition, their
chemical, physical, and biological
connections to downstream waters and
the strength of their effects on the
chemical, physical, or biological
integrity of a traditional navigable
water, interstate water, or the territorial
seas support this determination that
Prairie potholes are similarly situated by
rule.
(ii) Carolina and Delmarva bays are
ponded depressional wetlands that
occur along the Atlantic coastal plain
from northern Florida to New Jersey.
Though Carolina and Delmarva bays are
from the same category of wetland and
perform similar functions, they are
located in different parts of the Atlantic
coastal plain and thus have unique
names. Carolina bays are most abundant
in North Carolina and South Carolina,
while Carolina bays found in the
Delmarva Peninsula are commonly
referred to as Delmarva bays or
Delmarva potholes.
Most bays receive water through
precipitation, lose water through
evapotranspiration, and lack natural
surface outlets. Both mineral-based and
peat-based bays have shown
connections to shallow groundwater.
Bays typically are in proximity to each
other or to streams, providing for
hydrologic connections to each other
and to downstream waters in large rain
events via overland flow or shallow
subsurface connections. Some Delmarva
bays have surface water connections to
the Chesapeake Bay. In addition, human
channeling and ditching of the bays are
widespread and create surface
connections to other waters, including
the tributary system and estuaries.
These ditches commonly connect the
surface water of bays to other bays that
are lower on the landscape, and
ultimately, to streams.
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The hydrology in bays allow for
denitrification (chemical and biological
processes that remove nitrogen from
water), which can reduce the amount of
nitrate in both groundwater and
downstream surface waters. Because
bays are frequently connected
chemically to downstream waters
through ditches, they can be sources of
sediment and nutrients to downstream
waters. Where they are not connected
via confined surface connections, bays
can act as sediment and nutrient sinks.
Fish are reported in bays that are
known to dry out, indirectly
demonstrating surficial connections.
Amphibians and reptiles use bays
extensively for breeding and for rearing
young. These animals can disperse
many feet on the landscape and can
colonize, or serve as a food source to,
downstream waters. Similarly, bays
foster abundant insects that have the
potential to become part of the
downstream food chain. Humans have
ditched and channelized a high
percentage of bays, creating new surface
connections to downstream waters and
allowing transfer of nutrients, sediment,
and other pollutants, such as
methylmercury.
Carolina and Delmarva bays can occur
in high density on the landscape and
can act as a wetlands complex. Bays
have similar functions to other bays and
cumulatively these functions can impact
downstream waters.
The agencies conclude that Carolina
and Delmarva bays are similarly
situated based on their close proximity
to each other and the tributary network,
their hydrologic connections to each
other and the tributary network, their
density on the landscape, and their
similar functions.
(iii) The word pocosin comes from the
Algonquin Native American word for
‘‘swamp on a hill,’’ and these evergreen
shrub and tree-dominated wetlands are
found from Virginia to northern Florida,
but mainly in North Carolina. Typically,
there is no standing water present in
these peat-accumulating wetlands, but a
shallow water table leaves the soil
saturated for much of the year. They
range in size from less than an acre to
several thousand acres. The slow
movement of water through the dense
organic matter in pocosins removes
excess nutrients deposited by rainwater.
The same organic matter also acidifies
the water. This water is slowly released
to downstream waters and estuaries,
where it helps to maintain the proper
salinity, nutrients, and acidity.
Because pocosins are the topographic
high areas on the regional landscape,
they serve as the source of water for
downstream waters. Pocosins often have
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seasonal connections to drainageways
leading to estuaries or are adjoining
other wetlands draining into perennial
streams or estuaries. Other pocosins
have been ditched and are directly
connected to streams.
The agencies conclude that pocosins
are similarly situated based on their
close proximity to each other and the
tributary network, their hydrologic
connections to each other and the
tributary network, their density on the
landscape, and their similar functions.
(iv) Western vernal pools are shallow,
seasonal wetlands that accumulate
water during colder, wetter months and
gradually dry up during warmer, drier
months. Western vernal pools are
seasonal wetlands from the Pacific
Northwest to northern Baja California,
Mexico associated with topographic
depressions, soils with poor drainage,
mild, wet winters and hot, dry
summers. The agencies have determined
that California vernal pools are
‘‘similarly situated.’’
Because their hydrology and ecology
are so tightly coupled with the local and
regional geological processes that
formed them, western vernal pools in
California typically occur within
‘‘vernal pool landscapes,’’ or complexes
of pools in which swales connect pools
to each other and to seasonal streams.
Some common findings about the
hydrologic connectivity of western
vernal pools include evidence for
temporary or permanent outlets,
frequent filling and spilling of higher
pools into lower elevation swales and
stream channels, and conditions
supporting subsurface flows through
pools without perched aquifers to
nearby streams.
Non-glaciated vernal pools in western
states are reservoirs of biodiversity and
can be connected genetically to other
locations and aquatic habitats through
wind- and animal-mediated dispersal.
Animals and other organisms can move
between western vernal pool complexes
and streams. Insects and zooplankton
can be flushed from vernal pools into
streams and other waters during periods
of overflow, carried by animal vectors
(including humans), or dispersed by
wind.
The agencies conclude that western
vernal pools in California are similarly
situated based on their close proximity
to each other and the tributary network,
their interaction and arrangement as a
complex of wetlands, their hydrologic
connections to each other and the
tributary network, their density on the
landscape, and their similar functions.
(v) Along the Gulf of Mexico from
western Louisiana to south Texas,
freshwater wetlands occur as a mosaic
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of depressions, ridges, intermound flats,
and mima mounds. These coastal prairie
wetlands were formed thousands of
years ago by ancient rivers and bayous
and once occupied almost a third of the
landscape around Galveston Bay, Texas.
The term Texas coastal prairie wetlands
is not used uniformly in the scientific
literature but encompasses Texas prairie
pothole (freshwater depressional
wetlands) and marsh wetlands that are
described in some studies that occur on
the Lissie and Beaumont Geological
Formations, and the Ingleside Sand.
Texas coastal prairie wetlands are
locally abundant and in close proximity
to other coastal prairie wetlands and
function together cumulatively.
Collectively as a complex, Texas coastal
prairie wetlands can be geographically
and hydrologically connected to each
other via swales and connected to
downstream waters, contributing flow to
those downstream waters.
Cumulatively, these wetlands can
control nutrient release levels and rates
to downstream waters, as they capture,
store, transform, and pulse releases of
nutrients to those waters.
The agencies conclude that Texas
coastal prairie wetlands are similarly
situated based on their close proximity
to each other and the tributary network,
their hydrologic connections to each
other and the tributary network, their
interaction and formation as a complex
of wetlands, their density on the
landscape, and their similar functions.
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IV. Definition of ‘‘Waters of the United
States’’
A. Summary of the Rule
The rule revises the existing
definition of ‘‘waters of the United
States’’ consistent with the CWA,
science, the agencies’ technical
expertise and experience, and Supreme
Court decisions. The final rule
establishes categories of waters that are
jurisdictional and other categories of
waters that are excluded, as well as
categories of waters and wetlands that
require a case-specific significant nexus
evaluation to determine if they are
‘‘waters of the United States’’ and
covered by the CWA. The rule also
provides definitions for key terms used
in the regulation. The final rule retains
much of the structure of the agencies’
longstanding definition of ‘‘waters of the
United States,’’ and many of the existing
provisions of that definition where
revisions are not required in light of
Supreme Court decisions or other bases
for revision. All existing exclusions
from the definition of ‘‘waters of the
United States’’ are retained, and several
exclusions reflecting longstanding
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agencies’ practice are added to the
regulation for the first time.
The agencies define ‘‘waters of the
United States’’ in paragraph (a) of the
rule for all sections of the CWA to
include the traditional navigable waters
(a)(1), interstate waters (a)(2), the
territorial seas (a)(3), impoundments of
jurisdictional waters (a)(4), covered
tributaries (a)(5), and covered adjacent
waters (a)(6). Waters in these categories
are jurisdictional ‘‘waters of the United
States’’ by rule—no additional analysis
is required. This eliminates the need to
make a case-specific significant nexus
determination for covered tributaries or
covered adjacent waters because the
agencies determined that these waters
have a significant nexus to waters
identified in (a)(1) through (a)(3) of the
rule and thus are ‘‘waters of the United
States.’’ The agencies emphasize that
the finding of jurisdiction for these
covered tributaries and covered adjacent
waters was not based on the mere
connection of a water body to
downstream waters, but rather a
determination that the nexus, alone or
in combination with other of these
covered tributaries or covered adjacent
waters in the watershed, is significant.
The agencies exclude specified waters
from the definition of ‘‘waters of the
United States’’ in paragraph (b) of the
rule. The rule makes no substantive
change to the existing exclusion for
waste treatment systems designed
consistent with the requirements of the
CWA and makes no change to the
existing exclusion for prior converted
cropland. The rule excludes for the first
time certain waters and features over
which the agencies have generally not
asserted CWA jurisdiction, as well as
groundwater, which the agencies have
never interpreted to be a ‘‘water of the
United States’’ under the CWA.
Codifying these longstanding practices
supports the agencies’ goals of
providing greater clarity, certainty, and
predictability for the regulated public
and regulators, and makes rule
implementation clear and practical.
This final rule provides clear
exclusions for certain types of ditches.
The final rule also expressly excludes
stormwater control features created in
dry land and certain wastewater
recycling structures created in dry land.
Waters and features that are excluded
under paragraph (b) of the rule cannot
be determined to be jurisdictional under
any of the categories in the rule under
paragraph (a).
In addition to waters that are
categorically ‘‘waters of the United
States’’ or categorically excluded under
paragraphs (a) and (b), the rule
identifies certain waters that can be
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‘‘waters of the United States’’ only
where a case-specific determination has
found a significant nexus between the
water and traditional navigable waters,
interstate waters, or the territorial seas.
First, paragraph (a)(7) of the rule
specifies five types of waters (Prairie
potholes, Delmarva and Carolina bays,
pocosins, western vernal pools in
California, and Texas coastal prairie
wetlands) that the agencies have
determined to be ‘‘similarly situated,’’
and thus are to be considered in
combination in a significant nexus
analysis. Second, paragraph (a)(8)
specifies that waters located within the
100-year floodplain of a traditional
navigable water, interstate water, or the
territorial seas, and waters located
within 4,000 feet from the high tide line
or the ordinary high water mark of
traditional navigable waters, interstate
waters, the territorial seas,
impoundments, or covered tributaries
may be found to have a significant
nexus on a case-specific basis, but the
agencies have not made a determination
that the waters are ‘‘similarly situated.’’
As a result, a significant nexus analysis
for these waters will include a casespecific assessment of whether there are
any similarly situated waters, as well as
whether the water, alone or in
combination with any waters
determined to be similarly situated, has
a significant nexus to a traditional
navigable water, interstate water, or
territorial sea. The rule outlines at
(c)(5)(i)–(ix) functions relevant to these
case-specific significant nexus analyses.
Paragraph (c) of the rule provides
definitions for key terms used in the
regulation. Some of these are unchanged
from the current regulations, including
the definitions for ‘‘wetlands’’ at (c)(4),
‘‘ordinary high water mark’’ at (c)(6) and
‘‘high tide line’’ at (c)(7), although the
latter two are existing, unchanged
Corps’ definitions added to EPA’s
regulations for the first time. 33 CFR
328.3(d)–(e). The rule also defines for
the first time ‘‘tributary’’ and
‘‘tributaries’’ at (c)(3), ‘‘neighboring’’ (an
aspect of adjacency) at (c)(2), and
‘‘significant nexus’’ at (c)(5).
This rule is effective on August 28,
2015. Under existing Corps’ regulations
and guidance, approved jurisdictional
determinations generally are valid for
five years. The agencies will not reopen
existing approved jurisdictional
determinations unless requested to do
so by the applicant or, consistent with
existing Corps’ guidance, unless new
information warrants revision of the
determination before the expiration
period. Similarly, consistent with
existing regulations and guidance,
approved jurisdictional determinations
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associated with issued permits and
authorizations are valid until the
expiration date of the permit or
authorization.
As a general matter, the agencies’
actions are governed by the rule in effect
at the time the agency issues a
jurisdictional determination or permit
authorization, not by the date of a
permit application, request for
authorization, or request for a
jurisdictional determination. However,
any jurisdictional determinations issued
prior to the effective date of the rule and
jurisdictional determinations associated
with permit applications deemed by the
Corps to have been complete on the date
this rule is published in the Federal
Register, including complete preconstruction notifications, will be made
consistent with the existing rule, unless
the applicant requests that its approved
jurisdictional determination or permit
authorization be decided after the
effective date of the new rule. Reliance
on preliminary jurisdictional
determinations is also not affected by
the issuance of this rule. All other
jurisdictional determinations and
requests for authorization requiring an
approved jurisdictional determination
issued on or after the effective date of
this rule will be made consistent with
this rule.
It is important to emphasize that the
agencies do not anticipate being able to
complete new jurisdictional
determinations submitted after this rule
is published before it becomes effective.
As a result, requesters seeking
jurisdictional determinations after the
rule is published should expect the
determination will be made consistent
with this rule. The agencies recognize
there are a number of requests for
permit applications and requests for
jurisdictional determinations pending at
any time. The agencies expect only a
small portion of those pending actions
will require additional information from
or work by the requester. As described
in the Economic Analysis, the vast
majority of requests address streams and
adjacent wetlands, and the agencies do
not expect new information or work will
be needed to complete those requests. If
any additional information is needed to
assess these requests, the agencies will
work proactively with permit applicants
to reduce potential short-term
disruptions in the permit process that
may be associated with the rule.
B. Traditional Navigable Waters
The existing regulations include
within the definition of ‘‘waters of the
United States’’ all waters that are
currently used, or were used in the past,
or may be susceptible to use in
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interstate or foreign commerce,
including all waters which are subject to
the ebb and flow of the tide. See, e.g.,
33 CFR 328.3(a)(1); 40 CFR 230.3(s)(1);
40 CFR 122.2 (‘‘waters of the U.S.’’).
This paragraph of the regulation
encompasses those waters that are often
referred to as ‘‘traditional navigable
waters.’’ The rule does not make any
changes to this paragraph of the
regulation.
For purposes of CWA jurisdiction,
waters will be considered traditional
navigable waters, and jurisdictional
under (a)(1) of the rule, if they:
• Are subject to section 9 or 10 of the
Rivers and Harbors Appropriations Act
of 1899;
• Have been determined by a Federal
court to be navigable-in-fact under
Federal law;
• Are waters currently being used for
commercial navigation, including
commercial waterborne recreation (for
example, boat rentals, guided fishing
trips, or water ski tournaments);
• Have historically been used for
commercial navigation, including
commercial waterborne recreation; or
• Are susceptible to being used in the
future for commercial navigation,
including commercial waterborne
recreation.
See Technical Support Document;
‘‘U.S. Army Corps of Engineers
Jurisdictional Determination Form
Instructional Guidebook Appendix D,
‘Traditional Navigable Waters,’’’
available at: https://
www.usace.army.mil/Portals/2/docs/
civilworks/regulatory/cwa_guide/app_
d_traditional_navigable_waters.pdf.
The agencies received several
comments on the scope of traditional
navigable waters. Some commenters
observed that ‘‘traditional navigable
waters’’ as a jurisdictional category is
not based in science. Several
commenters thought that the final rule
should specify considerations to be
taken into account when determining if
a water is susceptible to being used in
future commercial navigation. The
agencies have not revised the regulation
to address susceptibility, but observe
that case law has provided a number of
considerations and examples that are
described further in the Technical
Support Document and are reflected in
longstanding agencies’ practice.
C. Interstate Waters
The existing regulations define
‘‘waters of the United States’’ to include
interstate waters, including interstate
wetlands. The rule does not change that
provision of the regulations. Therefore,
interstate waters are ‘‘waters of the
United States’’ even if they are not
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navigable for purposes of Federal
regulation under (a)(1) and do not
connect to such waters. Moreover, the
rule protects impoundments of
interstate waters, tributaries to interstate
waters, waters adjacent to interstate
waters, and waters adjacent to covered
tributaries of interstate waters because
they have a significant nexus to
interstate waters. Protection of these
waters is thus critical to protecting
interstate waters.
The language of the CWA indicates
that Congress intended the term
‘‘navigable waters’’ to include interstate
waters without imposing a requirement
that they be traditional navigable waters
themselves or be connected to
traditional navigable waters. The
precursor statutes to the CWA subjected
interstate waters and their tributaries to
Federal jurisdiction. The text of the
CWA, specifically CWA section 303,
which establishes ongoing requirements
for interstate waters, in conjunction
with the definition of navigable waters,
provides clear indication of Congress’
intent to protect interstate waters that
were previously subject to Federal
regulation. Other provisions of the
statute provide additional textual
evidence of the scope of the primary
jurisdictional term of the CWA.
The agencies also have a longstanding
regulatory interpretation that interstate
waters fall within the scope of CWA
jurisdiction. The agencies’
interpretation was promulgated
contemporaneously with the passage of
the CWA and is consistent with the
statutory and legislative history of the
CWA. Furthermore, the Supreme Court
has never addressed the CWA’s
coverage of interstate waters, and it is
not reasonable to read its decisions in
SWANCC and Rapanos to question the
jurisdictional status of interstate waters
or to impose additional jurisdictional
requirements on interstate waters. The
assertion of jurisdiction over interstate
waters is based on the statute and under
predecessor statutes where ‘‘interstate
waters’’ were defined as all rivers, lakes,
and other waters that flow across, or
form a part of, state boundaries. Pub. L.
80–845, sec. 10, 62 Stat. 1155, at 1161
(1948). The agencies will continue to
implement the provision consistent
with the intent of Congress. For
additional discussion of the agencies’
interpretation of the CWA with respect
to interstate waters, see Appendix B of
the proposed rule and the Technical
Support Document.
It is reasonable to assert jurisdiction
over tributaries, adjacent waters, and
waters that have a significant nexus to
interstate waters consistent with the
framework set forth in Justice Kennedy’s
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opinion in Rapanos for establishing
jurisdiction over waters with a
significant nexus to traditional
navigable waters. Waters and wetlands
with a significant nexus to traditional
navigable waters and interstate waters
have important beneficial effects on
those waters, and by recognizing that
polluting or destroying waters with a
significant nexus can harm downstream
jurisdictional waters. Traditional
navigable waters and interstate waters
cannot be protected without also
protecting the waters that have a
significant nexus to those waters as
identified in the rule. The rule thus
defines ‘‘waters of the United States’’ to
include tributaries to interstate waters,
waters adjacent to interstate waters,
waters adjacent to tributaries of
interstate waters, and other waters that
have a significant nexus to interstate
waters.
The agencies received a number of
comments on interstate waters. Some
commenters asserted that interstate
waters required a significant nexus to a
traditional navigable water in order to
be jurisdictional after Rapanos. The
agencies disagree for the reasons
described above, in Appendix B to the
proposed rule, and in the Technical
Support Document.
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D. Territorial Seas
The CWA and its existing regulations
include ‘‘the territorial seas’’ as a ‘‘water
of the United States.’’ The rule makes no
changes to that provision of the
regulation other than to change the
ordering to earlier in the regulation. The
CWA defines ‘‘navigable waters’’ to
include ‘‘the territorial seas’’ at section
502(7). The CWA goes on to define the
‘‘territorial seas’’ in section 502(8) as
‘‘the belt of the seas measured from the
line of ordinary low water along that
portion of the coast which is in direct
contact with the open sea and the line
marking the seaward limit of inland
waters, and extending seaward a
distance of three miles.’’ The territorial
seas establish the seaward limit of
‘‘waters of the United States.’’ The
territorial seas are clearly covered by the
CWA (they are also traditional navigable
waters), and it is reasonable to protect
their covered tributaries and covered
adjacent waters.
Although some comments addressed
the definition of ‘‘territorial seas’’
provided in the CWA suggesting that the
distance thresholds be revised to reflect
other resource statutes, the agencies do
not have authority to revise statutory
language.
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E. Impoundments
The existing regulations provide that
impoundments of ‘‘waters of the United
States’’ remain ‘‘waters of the United
States,’’ and the rule does not make any
changes to the existing regulatory
language.
Impoundments are jurisdictional
because an impoundment of a ‘‘water of
the United States’’ remains a ‘‘water of
the United States,’’ and because
scientific literature demonstrates that
impoundments continue to significantly
affect the chemical, physical, or
biological integrity of downstream
traditional navigable waters, interstate
waters, and the territorial seas. See
Technical Support Document. The
Supreme Court has confirmed that
damming or impounding a ‘‘water of the
United States’’ does not make the water
non-jurisdictional. See S. D. Warren Co.
v. Maine Bd. of Envtl. Prot., 547 U.S.
370, 379 n.5 (2006) (‘‘[N]or can we agree
that one can denationalize national
waters by exerting private control over
them.’’). Similarly, when presented with
a tributary to the Snake River which
flows only about two months per year
because of an irrigation diversion
structure installed upstream, the Ninth
Circuit noted ‘‘it is doubtful that a mere
man-made diversion would have turned
what was part of the waters of the
United States into something else and,
thus, eliminated it from national
concern.’’ U.S. v. Moses, 496 F.3d 984,
988 (9th Cir. 2007), cert. denied, 554
U.S. 918 (2008). As a matter of policy
and law, impoundments do not defederalize a water, even where there is
no longer flow below the impoundment.
The agencies have analyzed stream
networks, above and below
impoundments, for connection to
downstream traditional navigable
waters, interstate waters, or the
territorial seas. Scientific literature, as
well as the agencies’ scientific and
technical expertise and experience
confirm that impoundments have
chemical, physical, and biological
effects on downstream waters. See
Technical Support Document.
The agencies also note that an
impoundment of a water that is not a
‘‘water of the United States’’ can become
jurisdictional if, for example, the
impounded waters become navigable-infact and covered under paragraph (a)(1)
of the rule.
By their nature, impoundments of
jurisdictional waters would also often
meet the definition of ‘‘adjacent
waters,’’ as they are typically bordering
or contiguous. Impoundments of
‘‘waters of the United States’’ are per se
jurisdictional under paragraph (a)(4) of
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the rule without the need to determine
if they are also adjacent under
paragraph (a)(6). However, as described
in section IV.G below, ‘‘adjacent
waters,’’ as defined, have a significant
nexus to traditional navigable waters,
interstate waters, or the territorial seas,
which bolsters the agencies’
determination that impoundments of
‘‘waters of the United States’’ remain
‘‘waters of the United States.’’
Impoundments also may be one of the
waters through which tributaries
indirectly contribute flow to a
traditional navigable water, interstate
water, or territorial sea. As a matter of
law and science, an impoundment does
not cut off a connection between
upstream tributaries and a downstream
traditional navigable water, interstate
water, or territorial sea, so covered
tributaries above the impoundment are
still considered a tributary to
downstream traditional navigable
waters, interstate waters, or the
territorial seas even where the flow of
water might be impeded due to the
impoundment. See paragraph (a)(5).
The agencies received comments on
impoundments, which generally
explored the impacts of impoundments
on connectivity to downstream waters.
For the reasons described above and in
the Technical Support Document, the
agencies concluded that impoundments
of ‘‘waters of the United States’’ remain
‘‘waters of the United States.’’
F. Tributaries
The existing definition of ‘‘waters of
the United States’’ regulates all
tributaries without qualification. The
final rule protects only waters that have
a significant effect on the integrity of
traditional navigable waters, interstate
waters, or the territorial seas. The rule
establishes a definition of ‘‘tributary,’’
and provides that a water meeting the
definition of tributary, unless it is
excluded under paragraph (b), is a
‘‘water of the United States’’ without the
need for a separate case-specific
significant nexus evaluation. As
explained in Section III above, covered
tributaries and the functions they
provide, alone or in combination with
other tributaries in the watershed,
significantly affect the chemical,
physical, and biological integrity of
traditional navigable waters, interstate
waters, or the territorial seas. See also
Technical Support Document. This
section describes the provisions of the
rule addressing tributaries and changes
made to the provisions in the proposed
rule based on public comments.
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1. What are the provisions in the rule?
The rule defines ‘‘tributary’’ by
emphasizing the physical characteristics
created by sufficient volume, frequency
and duration of flow, and that the water
contributes flow, either directly or
through another water, to a traditional
navigable water, interstate water, or the
territorial seas. This definition is based
on the best available science, intent of
the CWA, and case law, and is
consistent with current practice. As
mentioned above in Section III, the
Science Report concludes that ‘‘[t]he
scientific literature unequivocally
demonstrates that streams, individually
or cumulatively, exert a strong influence
on the integrity of downstream waters.’’
Science Report at ES–2.
First, to meet the rule’s definition of
‘‘tributary,’’ a water must flow directly
or through another water or waters to a
traditional navigable water, interstate
water, or the territorial seas. Waters
through which a tributary may
contribute flow indirectly include, for
example, impoundments, wetlands,
lakes, and other tributaries. A tributary
may contribute flow through any
number of downstream waters,
including non-jurisdictional features,
such as a ditch excluded under
paragraph (b) of the rule, and
jurisdictional waters that are not
tributaries, such as an adjacent
wetland—but it must be part of a
tributary system that eventually flows to
a traditional navigable water, an
interstate water, or the territorial seas.
This limitation on what constitutes a
tributary for purposes of this rule is
fundamental. If a water is not part of the
tributary system of a traditional
navigable water, interstate water, or the
territorial seas, it does not meet the
definition of ‘‘tributary’’ and is not
jurisdictional under this provision of
the rule. For example, an intermittent
stream that exists wholly within one
state, is not itself a traditional navigable
water, and whose flows eventually ends
without connecting to a traditional
navigable water, interstate water, or the
territorial seas is not a ‘‘water of the
United States’’ as a ‘‘tributary’’ for
purposes of this rule. To determine
whether a water meets this aspect of the
definition, the connection can be traced
using direct observation, U.S. Geological
Survey (USGS) data, stream datasets
such as the National Hydrography
Dataset, aerial photography or other
reliable remote sensing information, or
other appropriate information.
Under the rule, flow in the tributary
may be perennial, intermittent, or
ephemeral. The agencies received
comments suggesting that the final rule
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provide definitions for the terms
ephemeral flow, intermittent flow, and
perennial flow. The agencies considered
the request and determined that there
was no need to include a definition
since they are commonly used scientific
terms. Longstanding agencies’ practice
considers perennial streams as those
with flowing water year-round during a
typical year, with groundwater or
contributions of flow from higher in the
stream or river network as primary
sources of water for stream flow.
Intermittent streams are those that have
both precipitation and groundwater
providing part of the stream’s flow, and
flow continuously only during certain
times of the year (e.g., during certain
seasons such as the rainy season).
Ephemeral streams have flowing water
only in response to precipitation events
in a typical year, and are always above
the water table. Precipitation can
include rainfall as well as snowmelt.
Science shows that tributaries regardless
of flow duration are very effective at
transporting pollutants downstream,
such as excess nutrients and sediment,
which impact the integrity and
character of traditional navigable
waters, interstate waters, and the
territorial seas. See Technical Support
Document.
Second, the rule requires two physical
indicators of flow: There must be a bed
and banks and an indicator of ordinary
high water mark. This definition of
‘‘tributary’’ includes only those waters
the agencies have concluded are the
type of waters that the CWA was
intended to protect and which either
individually or in combination with
other covered tributaries in the
watershed have a significant nexus to a
traditional navigable water, interstate
water, or the territorial seas. Thus, the
agencies are not defining ‘‘waters of the
United States’’ to include all streams
that might be considered ‘‘tributaries’’
in the general scientific literature. To
provide additional clarity and for ease
of use for the public, the agencies are
including the Corps’ existing definition
of ordinary high water mark in EPA’s
regulations as well. Under that existing
Corps regulation, ordinary high water
mark indicators include characteristics
such as shelving, scour, changes in soil
characteristics, and destruction of
terrestrial vegetation, among others.
A bed and banks and other indicators
of ordinary high water mark are
physical indicators of water flow and
are only created by sufficient and
regular intervals of flow. These physical
indicators can be created by perennial,
intermittent, and ephemeral flows. See
Technical Support Document. For
purposes of the rule, ‘‘bed and banks’’
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means the substrate and sides of a
channel between which flow is
confined. The banks constitute a break
in slope between the edge of the bed
and the surrounding terrain, and may
vary from steep to gradual. Existing
Corps regulations define ordinary high
water mark as the line on the shore
established by the fluctuations of water
and indicated by physical
characteristics such as a clear, natural
line impressed on the banks, shelving,
changes in the character of soil,
destruction of terrestrial vegetation, the
presence of litter and debris, or other
appropriate means that consider the
characteristics of the surrounding areas.
33 CFR 328.3(e). That definition is not
changed by the rule and is added to
EPA’s regulations.
Current Corps regulations and
guidance identify bed and banks as
indicators of the ordinary high water
mark. The definition of ‘‘tributary’’ in
this rule requires the presence of a bed
and banks and an additional indicator of
ordinary high water mark such as
staining, debris deposits, or other
indicator identified in the rule or agency
guidance. In many tributaries, the bed is
that part of the channel below the
ordinary high water mark, and the banks
often extend above the ordinary high
water mark. For other tributaries, such
as those that are incised, changes in
vegetation, changes in sediment
characteristics, staining, or other
ordinary high water mark indicators
may be found within the banks. In
concrete-lined channels, the concrete
acts as the bed and banks and can have
other ordinary high water mark
indicators such as staining and debris
deposits. Indicators of an ordinary high
water mark may vary from region to
region across the country. See Technical
Support Document.
Other evidence, besides direct field
observation, may establish the presence
of bed and banks and another indicator
of ordinary high water mark. The
agencies currently use many tools in
identifying tributaries and will continue
to rely on their experience and expertise
in identifying the presence of a bed and
banks and ordinary high water mark.
For example, several reliable, wellestablished remote sensing sources of
information or mapping can assist to
establish the presence of water that
contributes flow to a traditional
navigable water, interstate water, or the
territorial seas and provide evidence
regarding the presence of a bed and
banks and another indicator of ordinary
high water mark. Among the types of
remote sensing or mapping information
that can assist in establishing the
presence of water are USGS topographic
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data, the USGS National Hydrography
Dataset (NHD), Natural Resources
Conservation Service (NRCS) Soil
Surveys, and State or local stream maps,
as well as the analysis of aerial
photographs, and light detection and
ranging (also known as LIDAR) data,
and desktop tools that provide for the
hydrologic estimation of a discharge
sufficient to create an ordinary high
water mark, such as a regional
regression analysis or hydrologic
modeling. These sources of information
can sometimes be used independently
to infer the presence of a bed and banks
and another indicator of ordinary high
water mark, or where they correlate, can
be used to reasonably conclude the
presence of a bed and banks and
ordinary high water mark.
Both the USGS topographic data and
the NHD data assist to delineate
tributaries to traditional navigable
waters, interstate waters, or the
territorial seas. Where one or both of
these sources have indicated a ‘‘blue
line stream,’’ there is an indication that
the tributary could exhibit a bed and
banks and another indicator of ordinary
high water mark. Where this
information is combined with stream
order,11 more certainty can result. For
example, a water that is a second-order
stream will be more likely to exhibit a
bed and banks and another indicator of
ordinary high water mark as compared
to a first-order stream. This information
will vary in validity in different parts of
the country, so care will be taken to
evaluate additional information prior to
reasonably concluding a bed and banks
or other indicators of ordinary high
water mark are associated with the
stream. This will be particularly true for
first-order streams and for many streams
in the arid portions of the country.
Supporting information that can be used
to conclude the presence of a bed and
banks and another indicator of ordinary
high water mark would be the presence
of USGS stream data on the NRCS
county Soil Survey or local stream maps
which are mapped independently of the
USGS, aerial photography
interpretation, or digital terrain
depictions created from LIDAR. See
Technical Support Document.
Tributaries are observable in aerial
photography by their topographic
expression, characteristic linear and
11 Stream order is a method for stream
classification based on relative position within a
river network, when streams lacking upstream
tributaries (i.e., headwater streams) are first-order
streams and the junction of two streams of the same
order results in an increase in stream order (i.e., two
first-order streams join to form a second-order
stream, and so on). When streams of different orders
join, the order of the larger stream is retained. See
Science Report and Technical Support Document.
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curvilinear patterns, dark photographic
tones, and the presence and pattern of
riparian vegetation. The characteristic
linear and curvilinear patterns and dark
photographic tones observed on aerial
photography can be caused by shadow
cast from the banks of an incised stream
or from water in the stream channel
itself. In some cases stream channel
morphology is visible, providing
evidence of scour, materials sorting, and
deposition, all characteristics of an
ordinary high water mark. Visible
persistent water (e.g., multiple dates of
aerial photography showing visible
water) provides strong evidence of the
sufficient frequency and duration of
surface flow to create a bed and banks
and other indicators of ordinary high
water mark. Visible indicators of
running water such as rapids, riffles,
and pools all indicate the presence of a
bed and banks and other indicators of
ordinary high water mark. Other
physical characteristics of an ordinary
high water mark that may be visible on
aerial photography include the
destruction of terrestrial vegetation and
the absence of vegetation in a channel.
These indicators gleaned from aerial
photography interpretation can be
correlated with the presence of USGS
streams data in reasonably concluding
that a bed and banks and another
indicator of ordinary high water mark
are present. See Technical Support
Document.
Additional desktop tools can assist in
the identification of bed and banks and
other indicators of ordinary high water
mark. For instance, field staff use other
methods for estimating ordinary high
water mark, including, but not limited
to, lake and stream gage data, flood
predictions, historic records of water
flow, and statistical evidence. Some
desktop tools, such as a regional
regression analysis and the Hydrologic
Modeling System (HEC–HMS), provide
for the hydrologic estimation of stream
discharge sufficient to create an
ordinary high water mark in tributaries
under regional conditions. Such desktop
tools are particularly useful for
identifying presence of bed and banks
and another indicator of ordinary high
water mark when supported by
additional remote sensing tools that
indicate the presence of such physical
features.
LIDAR is a powerful tool to analyze
the characteristics of the land surface,
including tributary identification and
characterization. LIDAR data are
becoming more and more widespread
for engineering and land use planning
purposes. Where LIDAR data have been
processed to create a bare earth model,
detailed depictions of the land surface
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are available. Bare earth models reveal
subtle elevation changes and can clearly
show a tributary’s bed and banks and
channel morphology. In many cases
LIDAR can help delineate tributaries
that would exhibit a bed and banks and
another indicator of an ordinary high
water mark in greater detail than aerial
photography interpretation alone can.
Visible linear and curvilinear incisions
on a bare earth model are strong
evidence that a tributary with a bed and
banks and another indicator of an
ordinary high water mark is present.
LIDAR-indicated tributaries can be
correlated with aerial photography
interpretation and USGS stream data, to
reasonably conclude the presence of a
bed and banks and another indicator of
an ordinary high water mark in the
absence of a field visit. See Technical
Support Document. The agencies have
been using such remote sensing and
desktop tools to delineate tributaries for
many years where data from the field
are unavailable or a field visit is not
possible.
In addition, such desktop tools are
critical in circumstances where physical
characteristics of bed and banks and
another indicator of ordinary high water
mark are absent in the field, often due
to unpermitted alteration of streams. In
such cases where physical
characteristics of bed and banks and
another indicator of ordinary high water
mark no longer exist, they may be
determined by using other appropriate
means that consider the characteristics
of the surrounding areas. Such reliable
methods that can indicate prior
existence of bed and banks and other
indicators of ordinary high water mark
include, but are not limited to, lake and
stream gage data, elevation data,
spillway height, historic water flow
records, flood predictions, statistical
evidence, the use of reference
conditions, or through the remote
sensing and desktop tools described
above.
The upper limit of the tributary is the
point where a bed and banks and
another indicator of ordinary high water
mark cease to be identifiable. The
ordinary high water mark establishes
the lateral limits of a water, and its
absence generally determines when a
tributary’s channel or bed and banks has
ended, representing the upper limit of
the tributary. However, a natural or
constructed break in bed and banks or
other indicator of ordinary high water
mark does not constitute the upper limit
of a tributary where bed and banks or
other indicator ordinary high water
mark can be found farther upstream.
Note that waters, including wetlands,
which are adjacent to a tributary at the
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upper limit of the channel are
jurisdictional as ‘‘adjacent waters.’’
The definition of ‘‘tributary’’ includes
tributaries that flow directly or
indirectly through impoundments that
are jurisdictional under paragraph (a)(4)
of the rule. Tributaries to
impoundments of ‘‘waters of the United
States’’ are jurisdictional for the same
reasons the impoundments themselves
are jurisdictional. As discussed in
section IV. E., under case law, an
impoundment of a ‘‘water of the United
States’’ remains a ‘‘water of the United
States,’’ and scientific literature
demonstrates that impoundments
continue to significantly affect the
chemical, physical, or biological
integrity of downstream waters
traditional navigable waters, interstate
waters, and the territorial seas.
Therefore, tributaries to such
impoundments continue to have a
significant nexus, alone or in
combination with other covered
tributaries in the watershed, to the
downstream traditional navigable water,
interstate water, or the territorial seas.
Waters that meet the rule definition of
tributary remain tributaries even if there
is a manmade or natural break at some
point along the connection to the
traditional navigable water, interstate
water, or the territorial seas. In many
tributaries, there are often natural or
constructed breaks in the presence of a
bed and banks or ordinary high water
mark while hydrologic connectivity
remains. For example, in some regions
of the country where there is a very low
gradient, the banks of a tributary may be
very low or may even disappear at
times. Many tributaries lose their
ordinary high water mark when adjacent
wetlands are contiguous with the stream
channel. The definition of ‘‘tributary’’
addresses these circumstances and
states that waters that meet the
definition of tributary remain tributaries
even if such breaks occur, so long as bed
and banks and an ordinary high water
mark are present upstream of the break.
Under the rule, when a covered
tributary flows through a wetland into
another tributary (sometimes called a
‘‘run-of-stream’’ wetland), the covered
tributary remains jurisdictional even
though it lost its ordinary high water
mark through the wetland. By looking to
the presence of a bed and banks and an
ordinary high water mark upstream, the
rule ensures that a mere break in the
ordinary high water mark does not
render tributaries with a significant
nexus to downstream waters not
jurisdictional. Other breaks that do not
sever jurisdiction include constructed
breaks such as bridges, culverts, pipes,
dams, or waste treatment systems, or
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natural breaks such as debris piles,
boulder fields, or a stream that flows
underground so long as a bed and banks
and an ordinary high water mark can be
identified upstream of the break. Site
specific conditions will continue to
determine the distance up valley that
needs to be evaluated to see if the break
in bed and banks and ordinary high
water mark is temporary or the start of
the stream system.
The rule also clarifies that a water
meets the definition of tributary if the
water contributes flow through an
excluded feature such as a ditch with
ephemeral flow. While the water above
and below the excluded feature is
jurisdictional if it meets the definition
of tributary, the excluded feature does
not become jurisdictional. A water also
continues to meet the definition of
tributary if at some point the water
contributes flow through a jurisdictional
water that is not a tributary, such as an
adjacent wetland or impoundment.
The agencies’ longstanding
interpretation of the CWA has included
tributaries that are natural, modified, or
constructed waters. While this rule at
paragraph (b) excludes specific types of
constructed waters from jurisdiction, it
continues to interpret constructed
tributaries as jurisdictional unless
expressly excluded in paragraph (b).
Natural, modified, and constructed
tributaries provide many of the same
functions, especially as conduits for the
movement of water and pollutants to
other tributaries or directly to
traditional navigable waters, interstate
waters, or the territorial seas. The
discharge of a pollutant into a tributary
generally has the same effect
downstream whether the tributary
waterway is natural, modified, or
constructed. See discussion in section
III.C. above and the Technical Support
Document. Given the extensive human
modification of watercourses and
hydrologic systems throughout the
country, it is often difficult to
distinguish between natural
watercourses and watercourses that are
wholly or partly modified or
constructed. For example, tributaries
that have been channelized in concrete
or otherwise have been modified may
still meet the definition of tributaries
under the rule so long as they have bed
and banks and an ordinary high water
mark, contribute flow to a traditional
navigable water, interstate water, or the
territorial seas, and are not excluded
under paragraph (b). The important
consideration for a modified or
constructed water is whether it meets
the definition of ‘‘tributary’’ and is not
excluded under paragraph (b).
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Ditches are one important example of
constructed features that in many
instances can meet the definition of
tributary. Ditches are jurisdictional
under the rule only if they both meet the
definition of ‘‘tributary’’ and are not
excluded under paragraph (b)(3) in the
rule. Not all ditches meet the definition
of a tributary, and others—as discussed
in Section I—are expressly excluded
from jurisdiction.
Ditches protected by the rule must
meet the definition of tributary, having
a bed and banks and ordinary high
water mark, and contributing flow
directly or indirectly through another
water to a traditional navigable water,
interstate water, or the territorial seas.
Jurisdictional ditches include ditches
such as the following:
• Ditches with perennial flow,
• Ditches with intermittent flow that
are a relocated tributary, or are
excavated in a tributary, or drain
wetlands,
• Ditches, regardless of flow, that are
excavated in or relocate a tributary.
The definition of tributary includes
natural, undisturbed waters and those
that have been man-altered or
constructed, but which science shows
function as a tributary. In addition,
alteration or modification of natural
streams and rivers for purposes such as
flood control, erosion control, and other
reasons does not convert the tributary to
a ditch. A stream or river that has been
channelized or straightened because its
natural sinuosity has been altered,
cutting off the meanders, is not a ditch.
A stream that has banks stabilized
through use of concrete or rip-rap (e.g.,
rocks or stones) is not a ditch. The Los
Angeles River, for example, is a ‘‘water
of the United States’’ (and, indeed, a
traditional navigable water) and remains
a ‘‘water of the United States’’ and is not
excluded under paragraph (b)(3) even
where it has been ditched, channelized,
or concreted.
A ditch that relocates a stream is not
an excluded ditch under paragraph
(b)(3), and a stream is relocated either
when at least a portion of its original
channel has been physically moved, or
when the majority of its flow has been
redirected. A ditch that is a relocated
stream is distinguishable from a ditch
that withdraws water from a stream
without changing the stream’s aquatic
character. The latter type of ditch is
excluded from jurisdiction where it
meets the listed characteristics of
excluded ditches under paragraph
(b)(3). Agency staff can determine
historical presence of tributaries using a
variety of resources, such as historical
maps, historic aerial photographs, local
surface water management plans, street
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maintenance data, wetlands and
conservation programs and plans, as
well as functional assessments and
monitoring efforts. A ditch with
intermittent flow that drains a wetland
and otherwise meets the definition of
‘‘tributary’’ is a ‘‘tributary’’ and is not
excluded under paragraph (b)(3). See
IV.I. below.
Evidence, such as current or historic
photographs, prior delineations, or
USGS, state and local topographic maps,
may be used to determine whether a
ditch is an excluded ditch. Site
characteristics may also be present to
inform the determination of whether the
water body is a ditch, such as shape,
sinuosity, flow indications, etc., as
ditches are often created in a linear
fashion with little sinuosity and may or
may not connect to another ‘‘water of
the United States.’’
2. What changes did the Agencies make
from the proposed rule based on public
comments?
The rule’s definition of ‘‘tributary’’
retains many elements from the
proposed rule, but reflects public
comments in several important ways. In
particular, the rule emphasizes flow.
The rule defines ‘‘tributary’’ by
emphasizing physical characteristics
created by water flow and requiring that
the water contributes flow, either
directly or through another water, to a
traditional navigable water, interstate
water, or the territorial seas. The rule
also is clearer regarding the
jurisdictional status of certain ditches,
and clarifies that wetlands and waters
such as ponds and lakes that contribute
flow to a traditional navigable water,
interstate water, or the territorial seas
but typically lack a bed and banks and
ordinary high water mark are
considered ‘‘adjacent’’ but not a
‘‘tributary.’’
A number of commenters suggested
that the agencies should exclude
ephemeral streams from the definition
of tributary, expressing concern that
ephemeral waters that flow very rarely
would be considered a jurisdictional
tributary. The rule definition of
‘‘tributary’’ requires that flow must be of
sufficient volume, frequency, and
duration to create the physical
characteristics of bed and banks and an
ordinary high water mark. If a water
lacks sufficient flow to create such
characteristics, it is not considered a
‘‘tributary’’ under this rule. While some
commenters expressed concern that a
feature that flowed very rarely could
meet the proposed definition of
‘‘tributary,’’ it is the agencies’ judgment
that such a feature is not a tributary
under the rule because it would not
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form the physical indicators required
under the definitions of ‘‘ordinary high
water mark’’ and ‘‘tributary.’’
The rule includes ephemeral streams
that meet the definition of tributary as
‘‘waters of the United States’’ because
the agencies determined that such
streams provide important functions for
downstream waters, and in combination
with other covered tributaries in a
watershed significantly affect the
chemical, physical, and biological
integrity of traditional navigable waters,
interstate waters, and the territorial seas.
As noted by the SAB, and consistent
with the scientific literature, tributaries
as a group exert strong influence on the
chemical, physical, and biological
integrity of downstream waters, even
though the degree of connectivity is a
function of variation in the frequency,
duration, magnitude, predictability, and
consequences of chemical, physical, and
biological processes. See, e.g., SAB
2014b. These significant effects on
traditional navigable waters, interstate
waters, and the territorial seas occur
even when the tributary is small,
intermittent, or ephemeral.
In addition, the Science Report
concludes that, ‘‘[a]lthough less
abundant, the available evidence for
connectivity and downstream effects of
ephemeral streams was strong and
compelling, particularly in context with
the large body of evidence supporting
the physical connectivity and
cumulative effects of channelized flows
that form and maintain stream
networks.’’ Science Report at 6–13. For
example, ephemeral headwater streams
shape river channels in traditional
navigable or interstate waters by
accumulating and gradually or
episodically releasing stored materials
such as sediment and large woody
debris. These materials help structure
traditional navigable and interstate river
channels by slowing the flow of water
through channels and providing
substrate and habitat for aquatic
organisms.
Moreover, the agencies have
historically considered ephemeral
tributaries to be ‘‘waters of the United
States.’’ For example, for many years
EPA has reviewed and approved state
water quality standards for ephemeral
waters under CWA section 303(c),
several Corps’ Nationwide Permits
under CWA section 404 address
discharges of dredged or fill material
into ephemeral waters, and the agencies’
definition of ‘‘waters of the United
States’’ prior to this rule included all
tributaries without reference to flow
regime.
Numerous commenters asked that the
final rule define ‘‘bed and banks,’’
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37079
which are physical characteristics called
for under the definition of tributary.
Such commenters emphasized the
importance of a definition of ‘‘bed and
banks,’’ and some suggested definitional
language. To increase clarity, the
preamble in IV.F.1. above includes a
definition of bed and banks adapted
largely from longstanding agencies’
practice as well as comments. Several
commenters suggested that the rule
should add a definition of ‘‘ordinary
high water mark.’’ In response and to
increase clarity, the rule adds the Corps’
existing regulatory ordinary high water
mark definition to EPA’s regulations.
Corps technical manuals are available to
help identify ordinary high water mark,
referenced above. Several commenters
suggested that the agencies not require
a tributary to have both bed and banks
and ordinary high water mark, because
bed and banks are themselves an
indicator of ordinary high water mark,
and because ordinary high water mark
alone is an appropriate criterion for
many streams in the arid west where the
characteristic of bed and banks is less
common. The agencies based their
significant nexus determination for the
covered tributaries in part on the
amount of flow indicated where a
tributary has both a bed banks and
another indicator of ordinary high water
mark, so the rule continues to require
both physical indicators with the
preamble at IV.F.1. above clarifying the
means to conclude that those indicators
exist.
Several commenters suggested that
the rule exclude all constructed waters
from the definition of ‘‘waters of the
United States.’’ While the rule does
exclude several types of constructed
waters from jurisdiction, it continues to
consider constructed tributaries as
jurisdictional unless expressly excluded
in paragraph (b) for the reasons
described in section IV.I. and the
Technical Support Document.
Many comments recommended that
wetlands, ponds, and lakes that
contribute flow to a traditional
navigable water, interstate water, or the
territorial seas but lack a bed and banks
and ordinary high water mark not be
considered as tributaries, because of the
importance of those physical
characteristics to the definition.
Wetlands typically lack bed and banks
and ordinary high water mark, while
lakes and ponds typically have an
ordinary high water mark and a bed but
may lack banks. The proposed rule
expressly sought comment on whether
such waters should be considered as
tributaries or as ‘‘adjacent waters,’’
recognizing that it might add an element
of uncertainty to the definition of
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‘‘tributary’’ to include waters that lacked
the physical features called for in the
definition. In addition, the SAB
commented that tributaries are not
typically defined to include lentic
systems (still waters), and suggested that
the agencies reconsider including
ponds, lakes, and wetlands as covered
adjacent waters instead of tributaries.
SAB 2014b at 2. In response, the rule
does not consider these waters to be
tributaries, but defines covered adjacent
waters to include wetlands, lakes, and
ponds that connect segments of
tributaries or are at the head of the
tributary system. See section G for
further discussion.
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G. Adjacent Waters
Section III above explains the basis for
the agencies’ conclusion that covered
adjacent waters have a significant nexus
with traditionally navigable waters,
interstate waters, or the territorial seas.
The adjacency provision is based on the
best available science, intent of the
CWA, and case law, and is consistent
with the experience of the agencies in
making case-specific significant nexus
determinations. As discussed above in
Section III, the SAB concludes, ‘‘[t]he
available science supports [the
agencies’] proposal to include adjacent
waters and wetlands as waters of the
United States.’’ SAB 2014b at 2. This
section describes the provisions of the
rule governing adjacent waters, changes
made to the adjacent waters provision
based on comments on the proposed
rule, and, finally, how science and the
law support the agencies’ conclusions in
the final rule.
1. What are the provisions of the rule?
Under the rule, ‘‘adjacent’’ means
bordering, contiguous, or neighboring,
including waters separated from other
‘‘waters of the United States’’ by
constructed dikes or barriers, natural
river berms, beach dunes, and the like.
Waters adjacent to a traditional
navigable water, interstate water,
territorial sea, impoundment, or
tributary, are ‘‘waters of the United
States.’’ For purposes of adjacency, an
adjacent water includes wetlands within
or abutting its ordinary high water mark.
Adjacency is not limited to waters
located laterally to a traditional
navigable water, interstate water, the
territorial seas, an impoundment, or a
tributary. Therefore, waters that connect
segments of a traditional navigable
water, interstate water, the territorial
seas, an impoundment, or a tributary or
are located at the head of a traditional
navigable water, interstate water, the
territorial seas, an impoundment, or a
tributary may be determined to be
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bordering, contiguous, or neighboring,
and thus adjacent. ‘‘Adjacent waters’’
include wetlands, ponds, lakes, oxbows,
impoundments, and similar water
features. ‘‘Adjacent waters’’ do not
include any water excluded under
paragraph (b) of the rule. Note also that
a water that does not meet the definition
of ‘‘adjacent waters’’ may be determined
to be a ‘‘water of the United States’’ on
a case-specific basis under paragraph
(a)(8) of the rule.
Within the definition of ‘‘adjacent,’’
the terms bordering and contiguous are
well understood, and for continuity and
clarity the agencies continue to interpret
and implement those terms consistent
with the current policy and practice.
Waters separated by a berm or other
similar feature remain ‘‘adjacent’’ under
the definition.
Some waters included under the
definition of ‘‘tributary’’ in the proposed
rule, after consideration of public
comment, are ‘‘adjacent’’ in the final
rule. Specifically, waters that connect
segments of, or are at the head of, a
traditional navigable water, interstate
water, the territorial seas, an
impoundment, or a tributary are
adjacent to that water. For example, a
pond that is the source water to a
tributary and borders the tributary at its
uppermost reach is jurisdictional as an
adjacent water. Further, the rule states
that an adjacent water includes
wetlands within or abutting its ordinary
high water mark. This language is
designed to ensure that if there is a
fringe wetland abutting that pond that is
the source water to a tributary, that
wetland is considered part of the pond
under the rule and such pond as a
whole, including any abutting wetlands,
is jurisdictional as an adjacent water.
For purposes of adjacency, including
all three provisions of the definition of
‘‘neighboring,’’ the entire water is
adjacent if any part of the water is
bordering, contiguous or neighboring.
Therefore, the entire wetland is
‘‘adjacent’’ if any part of it is within the
distance thresholds established in the
definition of ‘‘neighboring.’’ For
example, if a tributary has a 1,000 foot
wide 100-year floodplain, then a water
that is located within 1,000 feet of the
ordinary high water mark of a covered
tributary and extends to 2,000 feet is
jurisdictional in its entirety as
‘‘neighboring.’’ In addition, for purposes
of determining whether a water is
‘‘adjacent’’ artificial features (such as
roads) do not divide a water; rather, the
water is treated as one entire water.
The definition of ‘‘adjacent’’ in the
rule does not include those waters in
which established, normal farming,
silviculture, and ranching activities
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occur. Wetlands and farm ponds in
which normal farming activities occur,
as those terms are used in section 404(f)
of the Clean Water Act and its
implementing regulations, are not
jurisdictional under the Act as an
‘‘adjacent’’ water. Waters in which
normal farming, ranching, and
silviculture activities occur instead will
continue to be subject to case-specific
review, as they are today. These waters
may be determined to have a significant
nexus on a case-specific basis under
paragraph (a)(7) or (a)(8). Recognizing
the vital role of farmers in providing the
nation with food, fiber, and fuel, the
Clean Water Act in Section 404(f)
exempts many normal farming activities
such as seeding, harvesting, cultivating,
planting, soil and water conservation
practices, and other activities from the
Section 404 permitting requirement.
‘‘Normal’’ farming, ranching, and
silviculture is clarified in the agencies’
implementing regulations to mean
established and ongoing activities to
distinguish from activities needed to
convert an area to farming, silviculture,
or ranching and activities that convert a
water to a non-water. 40 CFR
232.3(c)(1). The rule reflects this
framework by clarifying the waters in
which the activities Congress exempted
under Section 404(f) occur are not
jurisdictional as ‘‘adjacent.’’ It is
important to recognize that
‘‘tributaries,’’ including those ditches
that meet the tributary definition, are
not ‘‘adjacent’’ waters and are
jurisdictional by rule.
This provision interprets the intent of
Congress and reflects the intent of the
agencies to minimize potential
regulatory burdens on the nation’s
agriculture community, and recognizes
the work of farmers to protect and
conserve natural resources and water
quality on agricultural lands. While
waters in which normal farming,
silviculture, or ranching practices occur
may be determined to significantly
affect the chemical, physical, or
biological integrity of downstream
navigable waters, the agencies believe
that such determination should be made
based on a case-specific basis instead of
by rule. The agencies also recognize that
waters in which normal farming,
silviculture, or ranching practices occur
are often associated with modifications
and alterations including drainage,
changes to vegetation, and other
disturbances the agencies believe
should be specifically considered in
making a significant nexus
determination.
The rule establishes a definition of
‘‘neighboring’’ for purposes of
determining adjacency. In the rule, the
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agencies identify three circumstances
under which waters would be
‘‘neighboring’’ and therefore ‘‘waters of
the United States.’’
First, the term ‘‘neighboring’’ includes
all waters located in whole or in part
within 100 feet of the ordinary high
water mark of a traditional navigable
water, interstate water, the territorial
seas, an impoundment, or a covered
tributary.
Second, the term ‘‘neighboring’’
includes all waters within the 100-year
floodplain of a traditional navigable
water, interstate water, the territorial
seas, an impoundment, or a covered
tributary that is located in whole or in
part within 1,500 feet of the ordinary
high water mark of that jurisdictional
water. In this rule, the agencies interpret
‘‘100-year floodplain’’ to mean ‘‘the area
that will be inundated by the flood
event having a one percent chance of
being equaled or exceeded in any given
year.’’ This is consistent with the
Federal Emergency Management
Agency’s (FEMA) definition of ‘‘100year flood.’’ If the 100-year floodplain is
greater than 1,500 feet from the ordinary
high water mark, only those waters that
are located in whole or in part within
1,500 feet of the ordinary high water
mark are ‘‘neighboring.’’ In addition, if
the 100-year floodplain is less than
1,500 feet from the ordinary high water
mark, only those waters located in
whole or in part within the floodplain
are ‘‘neighboring’’ under this provision.
Third, the rule defines ‘‘neighboring’’
to include all waters located in whole or
in part within 1,500 feet of the high tide
line of a traditional navigable water or
the territorial seas, and all waters
located within 1,500 feet of the ordinary
high water mark of the Great Lakes. This
provision defines waters that begin
within 1,500 feet of a tidally-influence
traditional navigable water or the
territorial seas and waters within 1,500
feet of the ordinary high water mark of
the Great Lakes as ‘‘waters of the United
States.’’ To provide clarity for this
aspect of the definition, the agencies
incorporated the Corps’ existing
definition of high tide line into EPA’s
regulations at paragraph (c)(7) in the
rule.
As noted above, the rule provides that
with respect to the boundaries for
covered adjacent waters the entire water
is jurisdictional as long as the water is
at least partially located within the
distance threshold, and the agencies
interpret the rule to apply to any single
water or wetland that may straddle a
distance threshold. Low-centered
polygonal tundra and patterned ground
bogs (also called strangmoor, string
bogs, or patterned ground fens) are
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considered a single water for purposes
of the rule because their small,
intermingled wetland and non-wetland
components are physically and
functionally integrated. These areas
often have complex micro-topography
with repeated small changes in
elevation occurring over short distances.
Science demonstrates that these
wetlands function as a single wetland
matrix having clearly hydrophytic
vegetation, hydric soils, and wetland
hydrology. As a result, the agencies will
continue to evaluate these wetlands as
a single water under the rule. Where any
portion of these wetland types is
bordering, contiguous or neighboring,
the entire wetland is a ‘‘water of the
United States.’’ Similarly, for purposes
of a case-specific determination under
paragraph (a)(8), wetlands of these types
constitute a single water when making
a significant nexus determination. Other
wetlands may also have intermingled
wetland and non-wetland components
that are so physically and functionally
integrated they can be considered a
single water for purposes of the rule.
Groups of wetlands that are simply part
of a complex of wetlands would not be
considered a single water for purposes
of the rule.
The final rule also makes some
ministerial changes to the definition of
‘‘adjacent.’’ The existing regulation
defined ‘‘adjacent’’ to mean ‘‘bordering,
contiguous, or neighboring,’’ and had a
second sentence that clarified that
wetlands separated by berms and the
like remain adjacent wetlands. The final
rule combines those sentences without
changing the scope of adjacency.
When determining the jurisdictional
boundaries under the CWA for
‘‘adjacent waters,’’ the agencies will rely
on published FEMA Flood Zone Maps
to identify the location and extent of the
100-year floodplain. https://
msc.fema.gov/portal. These maps are
publicly available and provide a readily
accessible and transparent tool for the
public and agencies to use in locating
the 100-year floodplain. It is important
to recognize, however, that much of the
United States has not been mapped by
FEMA and, in some cases, a particular
map may be out of date and may not
accurately represent existing
circumstances on the ground. The
agencies will determine if a particular
map is no longer accurate based on
factors, such as streams or rivers moving
out of their channels with associated
changes in the location of the
floodplain. In the absence of applicable
FEMA maps, or in circumstances where
an existing FEMA map is deemed by the
agencies to be out of date, the agencies
will rely on other available tools to
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identify the 100-year floodplain,
including other Federal, State, or local
floodplain maps, Natural Resources
Conservation Service (NRCS) Soil
Surveys (Flooding Frequency Classes),
tidal gage data, and site-specific
modeling (e.g., Hydrologic Engineering
Centers River System Analysis System
or HEC–RAS). https://
websoilsurvey.sc.egov.usda.gov/App/
HomePage.htm and HEC–RAS and
https://www.hec.usace.army.mil/
software/hec-ras/. Additional
supporting information can include
historical evidence, such as
photographs, prior delineations,
topographic maps, and existing site
characteristics. Because identifying the
100-year floodplain is an important
aspect of establishing jurisdiction under
the rule and the reliable and appropriate
tools for identifying the 100-year
floodplain may vary, the agencies will
coordinate with other federal and state
agencies to develop additional
information for EPA and Corps field
staff to further improve tools for
identifying the 100-year floodplain in a
consistent, predictable, and
scientifically valid manner.
When determining the outer distance
threshold for an ‘‘adjacent water’’ the
line is drawn perpendicular to the
ordinary high water mark or high tide
line of the traditional navigable water,
interstate water, the territorial seas,
impoundment, or covered tributary and
extended landward from that point. If
there are breaks in the ordinary high
water mark, the line should be
extrapolated from the point where the
ordinary high water mark is observed on
the downstream side to the point where
the ordinary high water mark is lost on
the upstream side. Therefore, waters
may meet the definition of neighboring
even where, for example, a tributary
temporarily flows underground.
The agencies emphasize that they
fully support efforts by States and tribes
to protect under their own laws any
additional waters, including locally
special waters that may not be within
the Federal protections of the CWA as
the agencies have interpreted its scope
in this rule. In promulgating the
adjacent water boundaries, the agencies
have balanced protection and clarity,
scientific uncertainties and regulatory
experience, and established boundaries
that are, in their judgment, reasonable
and consistent with the statute and its
goals and objectives.
If waters identified in this section are
determined to be adjacent, no casespecific significant nexus evaluation is
required.
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2. What changes did the agencies make
from the proposed rule based on public
comments?
In the proposal, the agencies sought
comment on a number of ways to
address and clarify jurisdiction over
‘‘adjacent waters,’’ including
establishing a floodplain interval and
providing clarity on reasonable
proximity as an important aspect of
adjacency. In light of the comments, the
science, the agencies’ experience, and
the Supreme Court’s consistent
recognition of the agencies’ discretion to
interpret the bounds of CWA
jurisdiction, the agencies have made
some revisions in the final rule designed
to more clearly establish boundaries on
the scope of ‘‘adjacent waters.’’
Under the proposal and the final rule,
‘‘adjacent waters’’ are jurisdictional
based on the conclusion that they have
a significant nexus to traditional
navigable waters, interstate waters, or
the territorial seas, and there is no need
for additional analysis. Some
commenters wanted a case-specific
analysis for all ‘‘adjacent waters’’ as
they believed that the waters would not
individually have a significant nexus to
an adjacent ‘‘water of the United
States,’’ while others noted that their
functional relationship to the
downstream traditional navigable
waters, interstate waters, or the
territorial seas warranted the conclusion
that they were all jurisdictional. Based
on a review of the science, the agencies’
expertise and experience, and the law,
the agencies determined that ‘‘adjacent
waters,’’ as defined, alone or in
combination with other covered
‘‘adjacent waters’’ in a watershed have
a significant nexus to a traditional
navigable water, interstate water or the
territorial seas and therefore are ‘‘waters
of the United States’’ without the need
for any additional analysis. However,
the rule also provides for case-specific
analysis of some waters that do not meet
the definition of ‘‘neighboring’’
established by the rule. See section
IV.H.
The proposal included wetlands,
ponds, lakes, and impoundments that
contribute flow, directly or indirectly, to
the downstream traditional navigable
waters, interstate waters, or the
territorial seas in the definition of
‘‘tributary.’’ Some commenters
expressed concern that since such
waters generally do not have both an
ordinary high water mark and a bed and
banks, the definition of tributary was
contradictory and confusing. The
agencies sought comment on whether to
treat these waters as ‘‘adjacent waters’’
instead of tributaries, since they not
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only contribute flow, but they also
border or are contiguous to the waters
to which they contribute flow. The SAB
in particular commented that the
agencies ‘‘may want to consider whether
flow-through lentic systems should be
included as ‘‘adjacent waters’’ and
wetlands, rather than as tributaries.’’
SAB 2014b at 2. In light of the
comments and to provide additional
clarity, the agencies revised the
definitions of ‘‘adjacent’’ and
‘‘tributary’’ to include these waters as
‘‘adjacent.’’
Under the existing rule, there is no
definition for the term ‘‘neighboring,’’
and the public commented that not
having a definition created a lack of
clarity and inconsistent field practices
across the nation. In the proposal,
‘‘neighboring’’ was defined to include
waters located within the riparian area
or floodplain of a traditional navigable
water, interstate water, territorial sea,
impoundment, or tributary; waters with
a shallow subsurface hydrologic
connection to a jurisdictional water; and
waters with a confined surface
hydrologic connection to a
jurisdictional water. Although the
definitions were scientifically-based for
the terms ‘‘riparian area’’ and
‘‘floodplain’’ to define the lateral reach
of the term ‘‘neighboring,’’ some
commenters indicated that the proposed
definitions to clarify neighboring were
not clear. Those commenters requested
that a specific floodplain interval or
other limitation should be established to
more clearly identify the outer limit of
neighboring. Some commenters stated
that the proposed definition of
‘‘neighboring’’ was unclear, while other
commenters found the definition helped
clarify CWA jurisdiction and were
supportive of including a broad
definition, based on ecological
interconnectedness.
Some commenters stated that the
proposed definitions of ‘‘riparian area’’
and ‘‘floodplain’’ were vague or
ambiguous, broad or effectively
limitless, beyond the agencies’ authority
or difficult or impossible to implement
in the field. Other commenters were
supportive of using the riparian area as
a basis for adjacency. Some commenters
asked why the agencies were proposing
a new definition of ‘‘floodplain’’ that
was inconsistent with the definition
used by other Federal agencies like
NRCS or FEMA. Some commenters
suggested that if the agencies use
floodplains as a means to define
‘‘neighboring,’’ it should be limited to
the area inundated by the 2-year, 5-year,
10-year, or 20-year flood, while other
commenters supported the use of the
100-year floodplain as a component of
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‘‘neighboring.’’ Some commenters
supported including all wetlands and
other waters in the 100-year floodplain
as categorically jurisdictional. Other
commenters requested that floodplain
size be based on tributary size, while
others suggested that it should be based
on soil and geologic features, and some
suggested the use of the FEMA flood
zone maps. Some commenters stated
that ‘‘reasonable proximity’’ was neither
defined nor clarified adjacency, noting
that adjacency should not apply to
waters separated from a ‘‘water of the
United States’’ by great distances.
In response to comments and to
provide greater clarity and consistency,
in the rule the agencies establish a
definition of neighboring which
provides additional specificity
requested by some commenters,
including establishing a floodplain
interval and providing specific
boundaries from traditional navigable
waters, interstate waters, the territorial
seas, impoundments, and tributaries. In
the proposal, the agencies requested
comment on whether the rule should
provide greater specificity with regard
to how the agencies will determine if a
water is located in the floodplain of a
jurisdictional water. 79 FR 22209. As
recommended by the public and based
on science, the agencies’ boundaries for
‘‘neighboring’’ are based largely on use
of the 100-year floodplain. The agencies
concluded that the use of the riparian
area was unnecessarily complicated and
that as a general matter, waters in the
riparian area will also be in the 100-year
floodplain. Further, should the riparian
area on occasion extend beyond the 100year floodplain, the agencies have the
ability to perform a case-specific
significant nexus analysis on a water out
to 4,000 feet from the ordinary high
water mark or high tide line of a
traditional navigable water, interstate
water, the territorial sea, impoundment,
or tributary. The agencies have drawn
these lines based on their technical
expertise and experience in order to
provide a rule that is practical to
understand and implement and protects
those waters that significantly affect the
chemical, physical, or biological
integrity of traditional navigable waters,
interstate waters, or the territorial seas.
Because science indicates that
connectivity is on a gradient, the
agencies have also identified limited
circumstances in which waters that do
not meet the definition of ‘‘neighboring’’
may be determined on a case-specific
basis to have a significant nexus. See
section IV.I.
First, the rule establishes as
‘‘neighboring’’ waters that occur within
100 feet from traditional navigable
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waters, interstate waters, the territorial
seas, impoundments, and tributaries.
Second, the rule utilizes a specific
floodplain and also establishes
maximum distances for purposes of
‘‘neighboring.’’ Studies have found that
waters within the floodplain are
dynamically connected and frequently
interact with the downstream traditional
navigable water, interstate water,
territorial sea, impoundment, or
tributary. Some commenters indicated
that a specific floodplain or other
designation should be set to define the
outer boundary of ‘‘neighboring.’’
Further, some commenters requested
that the 100-year floodplain designation
be used to define the outer boundary of
adjacency because the public
understands this concept. Several
commenters recommended that FEMA
or NRCS maps be used to support the
analysis as these maps are easily
accessible to the public. Because FEMA
maps exist for many areas of the country
and the NRCS Soil Survey maps do as
well, the agencies decided that defining
‘‘neighboring’’ based in part on a
particular floodplain or recurrence
interval was a reasonable means of
ensuring the consistency and certainty
that is important to the public and for
implementation of the CWA. In drawing
lines, the agencies chose the 100-year
floodplain in part because FEMA and
NRCS together have generally mapped
large portions of the United States, and
these maps are publicly available, wellknown and well-understood.
Because the 100-year floodplain can
be very wide in some areas of the
country, particularly near large rivers,
the agencies chose to provide increased
clarity and certainty while ensuring that
waters that provide important functions
significantly affecting the chemical,
physical, and biological integrity of the
downstream traditional navigable
waters, interstate waters, or the
territorial seas are protected by
establishing a 1,500 foot maximum
distance for neighboring waters in the
rule. Waters within the 100-year
floodplain to a maximum of 1,500 feet
of the ordinary high water mark are
adjacent without regard to the presence
of berms or other barriers. However,
because the science demonstrates that
floodplain waters provide important
functions for downstream waters, the
agencies have established a provision
under paragraph (a)(8) for case-specific
significant nexus evaluations of waters
located in the 100-year floodplain of a
traditional navigable water, interstate
water, or the territorial seas beyond
1,500 feet.
The rule also establishes a separate
bright line for including as
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jurisdictional those waters that occur
within 1,500 feet of tidally-influenced
traditional navigable waters or the
territorial seas.
The proposal defined ‘‘neighboring’’
to include waters with a surface
connection to jurisdictional waters and
some commenters recommended
eliminating surface hydrologic
connectivity as a basis for adjacency.
The definition of neighboring does not
include a provision defining
‘‘neighboring’’ based on a surface
hydrologic connection. However, waters
with confined surface hydrologic
connections are considered adjacent
where they are bordering, contiguous, or
neighboring a traditional navigable
water, interstate water, the territorial
seas, impoundment, or covered
tributary. For example, a water with a
confined surface hydrologic connection
to a traditional navigable water that is
1,200 feet from the high tide line of that
water would meet the definition of
neighboring and be considered an
adjacent water. In circumstances where
a water does not meet the definition of
neighboring but is located within the
100-year floodplain of a traditional
navigable water, interstate water, or the
territorial seas, or within 4,000 feet of a
jurisdictional water, a confined surface
hydrologic connection may be an
important factor in evaluating a casespecific significant nexus under
paragraph (a)(8). See section H. below.
The proposal defined ‘‘neighboring’’
to include waters connected with a
shallow subsurface connection, and
some commenters recommended
eliminating subsurface hydrologic
connectivity as a basis for adjacency.
For example, some commenters asserted
that, because the CWA does not apply
to groundwater, the agencies do not
have the authority to assert jurisdiction
over waters connected to other ‘‘waters
of the United States’’ via a shallow
subsurface hydrologic connection. Some
commenters were concerned that the
distinction between ‘‘groundwater’’ and
a ‘‘shallow subsurface connection’’ was
unclear and questioned whether using a
shallow subsurface connection as a
basis for adjacency is contradictory to
excluding groundwater—including
groundwater drained through
subsurface drainage systems—as a
‘‘water of the United States.’’ Some
commenters supported use of shallow
subsurface connectivity for adjacency,
since the significant nexus test would be
employed to make the determination of
jurisdiction. Several commenters
suggested that the rule should protect
groundwater and shallow subsurface
flow, due to its connectivity to other
‘‘waters of the United States’’ and
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particularly since altering it could affect
the downstream waters. A few
commenters simply requested
clarifications regarding issues such as
how to determine whether a subsurface
connection exists; the meaning of
‘‘shallow;’’ distinguishing between
‘‘shallow’’ and ‘‘deep;’’ whether there
were any boundaries on adjacency via
hydrologic connectivity; and
determining whether the connection
was ‘‘sufficient’’ to establish adjacency.
In order to provide more certainty to the
public, the rule does not include a
provision defining neighboring based on
shallow subsurface flow, though such
flow may be an important factor in
evaluating a water on a case-specific
basis under paragraph (a)(8), as
appropriate.
Some commenters expressed concern
that the agencies’ proposed definition of
‘‘neighboring,’’ ‘‘riparian area,’’ and
‘‘floodplain’’ would mean that all land
within the floodplain or riparian area
would become regulated. In fact, only
waters, not land, in the floodplain or
riparian area would have been
considered adjacent under the proposed
rule. Similarly, under the final rule,
only waters, not land, are adjacent. In
response, the agencies have eliminated
the definitions of floodplain and
riparian area and have provided a
definition of neighboring which is clear
that only waters in specified
circumstances may be ‘‘waters of the
United States.’’
The agencies also eliminated a
parenthetical from the existing
‘‘adjacent wetlands’’ regulatory
provision. The phrase ‘‘other than
waters that are themselves wetlands’’
was intended to preclude asserting
CWA jurisdiction over wetlands that
were simply adjacent to a nonjurisdictional wetland. Such waters do
not meet the definition of ‘‘adjacent’’
under the rule since waters must be
adjacent to a traditional navigable water,
interstate water, the territorial seas,
impoundment, or covered tributary, so
the phrase is unnecessary and
confusing. With this change, the
agencies are protecting all waters that
meet the definition of ‘‘adjacent’’ as
‘‘waters of the United States,’’ and
eliminating confusion caused by the
parenthetical. For example, where the
100-year floodplain is greater than 1,500
feet, all wetlands within 1,500 feet of
the tributary’s ordinary high water mark
are jurisdictional because they are
‘‘neighboring’’ to the tributary,
regardless of the wetlands’ position
relative to each other.
Some commenters stated that the
proposed rule was an expansion of
jurisdiction because it would change the
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provision from ‘‘adjacent wetlands’’ to
‘‘adjacent waters.’’ The agencies
acknowledge that under the existing
regulation, the adjacency provision
applied only to wetlands adjacent to
‘‘waters of the United States.’’ However,
also under the existing regulation,
‘‘other waters’’ (such as intrastate rivers,
lakes and wetlands that are not
otherwise jurisdictional under other
sections of the rule) could be
determined to be jurisdictional if the
use, degradation or destruction of the
water could affect interstate or foreign
commerce. This provision of the
existing regulation reflected the
agencies’ interpretation at the time of
the jurisdiction of the CWA to extend to
the maximum extent permissible under
the Commerce Clause of the
Constitution. Therefore, while the
language of the specific adjacency
provision in the final rule may have
changed from wetlands to waters, that
does not represent an expansion of
jurisdiction as a whole in comparison to
the existing regulation, since adjacent
non-wetland waters would have been
subject to jurisdiction under the ‘‘other
waters’’ provision. The final rule does
not protect all waters that were
protected under the ‘‘other waters’’
provision of the existing regulation, and
therefore the inclusion of adjacent
ponds, for example, in the ‘‘adjacent
waters’’ provision of the final rule does
not reflect an overall expansion of
jurisdiction when compared to the
existing regulation.
3. How do science and law support the
rule?
Based on a review of the scientific
literature and the agencies’ expertise
and experience the agencies determined
that the categories of waters discussed
below are integrally linked to the
chemical, physical, or biological
functions of waters to which they are
adjacent and downstream to the
traditional navigable waters, interstate
waters or the territorial seas. Therefore,
the agencies determined that the waters
defined as adjacent have a significant
nexus with traditional navigable waters,
interstate waters or the territorial seas
and are thus ‘‘waters of the United
States.’’ Additional information,
including citations, can be found in
section III of the preamble, the Science
Report, and the Technical Support
Document for the rule.
a. Waters that are Bordering or
Contiguous
As discussed in section III above,
wetlands, ponds, lakes, oxbows,
impoundments, and similar water
features that are bordering or contiguous
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perform a myriad of critical chemical
and biological functions associated with
the downstream traditional navigable
waters, interstate waters, or the
territorial seas. Such waters are
integrally linked with the jurisdictional
waters to which they are adjacent.
Because of their close physical
proximity to nearby jurisdictional
waters, bordering or contiguous waters
readily exchange their waters through
the saturated soils surrounding the
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary or
through surface exchange. This
commingling of waters allows bordering
or contiguous waters to both provide
chemically transformed waters to
streams and to absorb excess stream
flow, which in turn can significantly
affect downstream traditional navigable
waters, interstate waters, or the
territorial seas. The close proximity also
allows for the direct exchange of
biological materials, including organic
matter that serves as part of the food
web of downstream traditional
navigable waters, interstate waters, or
the territorial seas. Waters that are
bordering or contiguous are often
located on the floodplain or within the
riparian area of the waters to which they
are adjacent. Bordering or contiguous
waters include those that directly abut
a traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary. The
Science Report and the Technical
Support Document demonstrate that
such waters are physically, chemically,
and biologically integrated with
downstream traditional navigable
waters, interstate waters, or the
territorial seas and significantly affect
their integrity.
b. Waters Separated From Other
‘‘Waters of the United States’’ by
Constructed Dikes or Barriers, Natural
River Berms, Beach Dunes and the Like
Adjacent waters separated from a
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary by
constructed dikes or barriers, natural
river berms, beach dunes, and the like
continue to have a significant effect on
downstream traditional navigable
waters, interstate waters, or the
territorial seas, either alone or in
combination with other ‘‘adjacent
waters.’’ Such waters continue to have
a hydrologic connection to downstream
waters. This is because constructed
dikes or barriers, natural river berms,
beach dunes, and the like typically do
not block all water flow. This
hydrologic connection can occur via
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seepage, or the flow of water through
the soil pores, or via over-topping,
where water from the nearby traditional
navigable water, interstate water, the
territorial seas, impoundment, or
covered tributary periodically overtops
the berm or other similar feature. Bermlike landforms known as natural levees
occur naturally and do not isolate
adjacent wetlands from the streams that
form them. Natural levees and the
wetlands and waters behind them are
part of the floodplain. Natural levees are
discontinuous, which allows for a
hydrologic connection to the stream or
river via openings in the levees and thus
the periodic mixing of river water and
backwater. Man-made levees and
similar structures also do not isolate
‘‘adjacent waters.’’ Waters, including
wetlands, separated from a
jurisdictional water by a natural or manmade berm serve many of the same
functions as other ‘‘adjacent waters.’’
Furthermore, even in cases where a
hydrologic connection may not exist,
there are other important
considerations, such as chemical and
biological functions, that result in a
significant nexus between the adjacent
wetlands or waters and the nearby
‘‘waters of the United States,’’ and
traditional navigable waters, interstate
waters, or the territorial seas. On this
point, Justice Kennedy stated: ‘‘In many
cases, moreover, filling in wetlands
separated from another water by a berm
can mean that floodwater, impurities, or
runoff that would have been stored or
contained in the wetlands will instead
flow out to major waterways. With these
concerns in mind, the Corps’ definition
of adjacency is a reasonable one, for it
may be the absence of an interchange of
waters prior to the dredge and fill
activity that makes protection of the
wetlands critical to the statutory
scheme.’’ Rapanos at 775. For instance,
covered adjacent waters behind berms
can still serve important water quality
functions, serving to filter pollutants
and sediment before they reach
downstream waters. Wetlands and open
waters behind berms, where the system
is extensive, can help reduce the
impacts of storm surges caused by
hurricanes. Such ‘‘adjacent waters,’’
including wetlands, separated from
waters by berms and the like maintain
ecological connection with those waters.
It is not the existence of the dike, levee,
and the like that makes these waters
jurisdictional. Adjacent waters
separated from the tributary network by
constructed dikes or barriers, natural
river berms, beach dunes, and the like
continue to have a hydrologic
connection to downstream waters.
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Waters behind berms and the like can
significantly affect the chemical,
physical, and biologic integrity of
traditional navigable waters, interstate
waters, or the territorial seas.
c. Waters Within 100 Feet
All wetlands, ponds, lakes, oxbows,
impoundments, and similar water
features that are located in whole or in
part within 100 feet of the ordinary high
water mark of a jurisdictional water
perform a myriad of critical chemical,
physical, and biological functions
associated with the downstream
traditional navigable water, interstate
water or the territorial seas and
therefore the agencies have determined
that they are ‘‘neighboring’’ and thus
‘‘waters of the United States.’’ Waters
within 100 feet of a jurisdictional water
are often located within the riparian
area and are often connected via surface
and shallow subsurface hydrology to the
water to which they are adjacent. While
the SAB was clear that distance is not
the only factor that influences
connections and their effects
downstream, due to their close
proximity to jurisdictional waters,
waters within 100 feet are often located
within a landscape position that allows
for them to receive and process surface
and shallow subsurface flows before
they reach streams and rivers. These
waters individually and collectively
affect the integrity of downstream
waters by acting primarily as sinks that
retain floodwaters, sediments, nutrients,
and contaminants that could otherwise
negatively impact the condition or
function of downstream waters.
Wetlands and open waters within close
proximity of jurisdictional waters
improve water quality through
assimilation, transformation, or
sequestration of nutrients, sediment,
and other pollutants that can affect the
integrity of downstream traditional
navigable waters, interstate waters, or
the territorial seas. These waters,
including wetlands, also provide
important habitat for aquatic-associated
species to forage, breed, and rest.
In order to provide greater clarity and
consistency and based on a review of
the science and the agencies’ expertise
and experience, the agencies identified
a 100 foot threshold for neighboring
waters to a traditional navigable water,
interstate water, territorial sea, tributary,
or impoundment. Further, the agencies
determined that there is a significant
nexus with the downstream traditional
navigable waters, interstate waters, or
the territorial seas, and these ‘‘adjacent
waters’’ are ‘‘waters of the United
States.’’ With respect to provision of
water quality benefits downstream, non-
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floodplain waters within close
proximity of the stream network often
are able to have more water quality
benefits than those located at a distance
from the stream. Many studies indicate
that the primary water quality and
habitat benefits will generally occur
within a several hundred foot zone of a
water. In addition, the scientific
literature indicates that to be effective,
contaminant removal needs to occur at
a reasonable distance prior to entry into
the downstream traditional navigable
waters, interstate waters, or the
territorial seas. Some studies also
indicate that fish, amphibians (e.g.,
frogs, toads), reptiles (e.g., turtles), and
small mammals (e.g., otters, beavers,
etc.) will use at least a 100 foot zone for
foraging, breeding, nesting, and other
life cycle needs.
Based on a review of the scientific
literature and the agencies’ expertise
and experience, there is clear evidence
that the identified waters within 100
feet of the ordinary high water mark of
a jurisdictional water, even when
located outside the floodplain, perform
critical processes and functions
discussed in section III above. All
waters within 100 feet of a jurisdictional
water significantly affect the chemical,
physical, or biological integrity of the
waters to which they are adjacent, and
those waters in turn significantly affect
the chemical, physical, or biological
integrity of the downstream traditional
navigable waters, interstate waters, or
the territorial seas. The agencies
established a 100 foot threshold from
the water’s lateral limit in the definition
of neighboring because, based on the
agencies’ expertise and experience
implementing the CWA and in light of
the science, the agencies concluded this
was a reasonable and practical boundary
within which to conclude the waters
clearly significantly affected the
integrity of traditional navigable waters,
interstate waters, or the territorial seas,
and these ‘‘adjacent waters’’ are ‘‘waters
of the United States.’’
d. Floodplain Waters Within 1,500 Feet
As discussed in section III above,
wetlands and open waters that are
neighboring perform a myriad of critical
chemical and biological functions
associated with the downstream
traditional navigable waters, interstate
waters, or the territorial seas. The
scientific literature supports that
wetlands and open waters in
floodplains are chemically, physically,
and biologically connected to
downstream traditional navigable
waters, interstate waters, or the
territorial seas and significantly affect
the integrity of such waters. The Science
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Report concludes that wetlands and
open waters located in ‘‘floodplains are
physically, chemically and biologically
integrated with rivers via functions that
improve downstream water quality,
including the temporary storage and
deposition of channel-forming sediment
and woody debris, temporary storage of
local ground water that supports
baseflow in rivers, and transformation
and transport of stored organic matter.’’
Science Report at ES–2 to ES–3. Such
waters act as the most effective buffer to
protect downstream waters from
nonpoint source pollution (such as
nitrogen and phosphorus), provide
habitat for breeding fish and aquatic
insects that also live in streams, and
retain floodwaters, sediment, nutrients,
and contaminants that could otherwise
negatively impact the condition or
function of downstream waters.
For waters in the 100-year floodplain
within 1,500 feet of the ordinary high
water mark of a traditional navigable
water, interstate water, the territorial
seas, impoundment, or covered
tributary, the agencies determine there
is a significant nexus with the
downstream traditional navigable
waters, interstate waters, or the
territorial seas and these waters are
critical to protect the downstream
waters. Based on a review of the
scientific literature, the agencies’
technical expertise and experience, and
the implementation value of drawing
clear lines, the rule establishes a
boundary for floodplain waters to meet
the definition of ‘‘neighboring’’ and be
‘‘waters of the United States’’ by rule.
This boundary was established in order
to protect vitally important waters
within a watershed while at the same
time providing a practical and
implementable rule. The agencies are
not determining that waters in the
floodplain farther than 1,500 feet from
the ordinary high water mark never
have a significant nexus. Rather, the
agencies are using their technical
expertise to promulgate a practical rule
that draws reasonable boundaries in
order to protect the waters that most
clearly have a significant nexus while
minimizing uncertainty about the scope
of ‘‘waters of the United States.’’
Because waters beyond these
boundaries may have a significant
nexus, the rule also establishes areas in
which a case-specific significant nexus
determination must be made. See
section IV.H.
e. Waters Within 1,500 Feet of TidallyInfluenced Traditional Navigable Waters
or the Territorial Seas or the Great Lakes
Many tidally-influenced waters do not
have floodplains, so the agencies
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include a separate provision within the
definition of ‘‘neighboring’’ to protect
the ‘‘adjacent’’ waters that have a
significant nexus to tidally-influenced
traditional navigable waters or the
territorial seas or the Great Lakes. Under
Riverside Bayview and Justice
Kennedy’s opinion in Rapanos, waters
adjacent to traditional navigable waters,
including the territorial seas, are
‘‘waters of the United States.’’ Because
the connection to a tidally-influenced
traditional navigable water, the
territorial seas, or the Great Lakes is so
close, the rule defines ‘‘neighboring’’ to
include waters within 1,500 feet of the
high tide line or the ordinary high water
mark of the Great Lakes. Wetlands,
ponds, lakes, oxbows, impoundments,
and similar water features within 1,500
feet of these waters are physically
connected to such waters by surface and
shallow subsurface flow. As
demonstrated in section III above, these
waters perform a myriad of critical
chemical and biological functions
associated with these nearby waters to
which they are adjacent.
These waters in combination
significantly affect the integrity of the
connected tidally influenced traditional
navigable water or the territorial seas or
the Great Lakes by acting primarily as
sinks that retain floodwaters, sediments,
nutrients, and contaminants that could
otherwise negatively impact the
condition or function of those waters.
Like floodplain waters, the scientific
literature supports that wetlands and
other similar waters within close
proximity improve water quality
through assimilation, transformation, or
sequestration of nutrients, sediment,
and other pollutants that can affect
downstream water quality. These waters
also provide important habitat for
aquatic-associated species to forage,
breed, and rest in.
For example, wetlands dominated by
grass-like vegetation that occur in
depressional areas between sand dunes
or beach ridges along the territorial seas
and the Great Lakes shoreline are
dependent upon these waters for their
water source. The waters, including
wetlands, generally form when water
levels of the territorial seas fall or the
Great Lakes drop, creating swales that
support a diverse mix of wetland
vegetation and many endangered and
threatened species. Many studies
demonstrate that these waters have been
shown to act in concert with the rising
and lowering of the tide, and that the
critical functions provided by these
waters are similar and play an important
role in maintaining the chemical,
physical, or biological integrity of the
nearby traditional navigable waters,
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interstate waters, or the territorial seas
because of the hydrological and
ecological connections to and
interactions with those waters.
Science demonstrates that distance is
a factor in the connectivity and the
strength of connectivity of wetlands and
open waters to downstream waters.
Thus, waters that are more distant
generally have less opportunity to be
connected to downstream waters.
Wetlands and open waters closer to the
stream network generally will have
greater hydrologic and biological
connectivity than waters located farther
from the same network. For instance,
waters that are more closely proximate
have a greater opportunity to contribute
flow. Via their hydrologic connectivity,
they also have chemical connectivity to
and effects on these downstream waters
and are more likely to impact water
quality due to their close distance.
Waters more closely located to these
waters are also more likely to be
biologically connected to such waters
more frequently and by more species,
including amphibians and other aquatic
animals. Because tidally-influenced
traditional navigable waters, the
territorial seas, and the Great Lakes are
generally much larger in size than other
jurisdictional waters, the agencies
believe that a 1,500 foot threshold is a
reasonable distance to capture most
wetlands and open waters that are so
closely linked to these waters that they
can properly be considered adjacent as
neighboring waters.
Based on a review of the scientific
literature and the agencies’ expertise
and experience, there is clear evidence
waters within 1,500 feet of these waters,
even when located outside the
floodplain, perform critical processes
and functions discussed in section III
above. The agencies established a 1,500
foot threshold from the water’s lateral
limit, which would be either the high
tide line or the ordinary high water
mark, in the definition of neighboring
because, based on the agencies’
expertise and experience implementing
the CWA and in light of the science, the
agencies concluded this was a
reasonable and practical boundary
within which to conclude the waters
most clearly significantly affected the
integrity of the traditional navigable
water or the territorial seas, and these
covered adjacent waters are ‘‘waters of
the United States.’’ Waters located
within the 100-year floodplain of a
traditional navigable water, interstate
water, or the territorial seas, and waters
located more than 1,500 feet and less
than 4,000 feet from the ordinary high
water mark of a traditional navigable
water, interstate water, the territorial
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seas, an impoundment, or a tributary,
may still be determined to have a
significant nexus on a case-specific
basis under paragraph (a)(8) of the rule
and therefore be a ‘‘water of the United
States.’’ See section IV.H.
H. Case-Specific ‘‘Waters of the United
States’’
The rule establishes two exclusive
circumstances under which casespecific determinations will be made for
whether a water has a ‘‘significant
nexus’’ and is therefore a ‘‘water of the
United States.’’ The proposed rule
included a broad provision that allowed
for a case-specific determination of
significant nexus for any water that was
not categorically jurisdictional or
excluded. Many commenters expressed
concern that such a broad opportunity
for case-specific ‘‘waters of the United
States’’ determinations would lead to
too much uncertainty about the
jurisdictional status of waters in broad
areas throughout the country. The
agencies have greatly reduced the extent
of waters subject to this individual
review by carefully incorporating the
scientific literature and by utilizing
agency expertise and experience to draw
boundaries. The rule provides for casespecific determinations under more
narrowly targeted circumstances based
on the agencies’ assessment of the
importance of certain specified waters
to the chemical, physical, and biological
integrity of traditional navigable waters,
interstate waters, and the territorial seas.
First, the rule identifies at paragraph
(a)(7) five subcategories of waters
(Prairie potholes, Carolina and
Delmarva bays, pocosins, western vernal
pools in California, and Texas coastal
prairie wetlands) that the agencies have
determined are ‘‘similarly situated’’ for
purposes of a significant nexus
determination. Second, the rule
identifies at paragraph (a)(8) specific
circumstances under which waters will
be subject to a case-specific significant
nexus determination but for which the
agencies have not made a ‘‘similarly
situated’’ determination: Waters within
the 100-year floodplain of a traditional
navigable water, interstate water, or the
territorial seas, and waters within 4,000
feet of the high tide line or the ordinary
high water mark of a traditional
navigable water, interstate water, the
territorial seas, impoundments, or
tributaries, as defined. If any water
meets the definition of ‘‘adjacent’’
waters it is jurisdictional under
paragraph (a)(6) and no case-specific
significant nexus is required. Waters
that do not fall within the six
categorically jurisdictional waters
identified in paragraph (a)(1) through
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(a)(6) of the rule or within these two
case-specific provisions are not ‘‘waters
of the United States.’’
This section first discusses the five
subcategories of waters that the agencies
determine are ‘‘similarly situated’’ for
purposes of a significant nexus
determination; second, the 100-year
floodplain and 4,000 foot boundaries
under which waters will be subject to a
case-specific significant nexus
determination but for which the
agencies have not made a ‘‘similarly
situated’’ determination; third, the
definition of ‘‘significant nexus’’ and
how the case-specific significant nexus
determinations will be made under
these two provisions; and, finally, the
revisions made to the rule with respect
to case-specific determinations and
major comments.
1. Waters Determined To Be ‘‘Similarly
Situated’’ by Rule for Which a CaseSpecific Significant Nexus
Determinations Is Required
In the rule, paragraph (a)(7) specifies
the subcategories of waters (Prairie
potholes, Carolina and Delmarva bays,
pocosins, western vernal pools in
California, and Texas coastal prairie
wetlands) that, if they are not otherwise
jurisdictional under paragraphs (a)(1)
through (a)(6), the agencies determine to
be ‘‘similarly situated’’ by rule. In the
proposal the agencies sought comment
on a number of options to address
remaining waters that did not fit within
the jurisdictional categories, including
whether to conclude that other waters
were ‘‘similarly situated’’ in certain
areas of the country or whether to
conclude that specified subcategories of
waters were jurisdictional. 79 FR 22215,
22216. The agencies concluded that
waters within the five subcategories
were ‘‘similarly situated’’ in the areas of
the country in which they are located.
The rationale for this determination is
discussed above in Section III. Under
paragraph (a)(7), Prairie potholes,
Carolina and Delmarva bays, pocosins,
western vernal pools in California, and
Texas coastal prairie wetlands are
jurisdictional when they have a
significant nexus to a traditional
navigable water, interstate water, or the
territorial seas. Waters subject to normal
farming, silviculture, and ranching
activities that are within these
subcategories will be assessed
consistent with this provision of the
rule. Waters in these subcategories are
not jurisdictional as a class under the
rule. However, because the agencies
determined that these subcategories of
waters are ‘‘similarly situated,’’ the
waters within the specified
subcategories that are not otherwise
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jurisdictional under paragraph (a)(6) of
the rule must be assessed in
combination with all waters of the same
subcategory in the region identified by
the watershed that drains to the nearest
point of entry of a traditional navigable
water, interstate water, or the territorial
seas (hereinafter referred to as the point
of entry watershed).
When performing a case-specific
significant nexus evaluation for a water
in the paragraph (a)(7) subcategories, the
rule establishes which waters must be
considered in combination. The
similarly situated waters identified in
the subparagraphs will be combined
with other waters in the same
subparagraph located in a single point
of entry watershed. For example, under
paragraph (a)(7) only western vernal
pools can be analyzed with other
western vernal pools in the same point
of entry watershed. Waters identified in
the subparagraphs that are otherwise
jurisdictional under the rule cannot be
considered in combination with
paragraph (a)(7) waters for purposes of
a case-specific significant nexus
determination under paragraph (a)(7).
Individual waters of the specified
subcategories may be jurisdictional
under other paragraphs of this rule (e.g.,
a Prairie pothole that sits on a state
border is an interstate water under
paragraph (a)(2) or a western vernal pool
that meets the definition of adjacent
under paragraph (a)(6)). Where those
individual waters are jurisdictional
under paragraph (a)(1) through (a)(6) by
rule, no case-specific significant nexus
analysis is required. The rule also states
that waters in paragraph (a)(7) shall not
be combined with waters jurisdictional
under paragraph (a)(6). Essentially,
while Prairie potholes are an identified
subcategory under paragraph (a)(7), that
identification does not affect a Prairie
pothole that borders a covered tributary
and is jurisdictional as an adjacent
water under paragraph (a)(6).
Additionally, a Prairie pothole that is
jurisdictional under paragraph (a)(6)
cannot be combined with Prairie
potholes that require a case-specific
jurisdictional analysis under paragraph
(a)(7) since ‘‘adjacent waters’’ have
already been determined to have a
significant nexus by rule. Finally,
waters within the specified
subcategories in paragraph (a)(7) are
assessed under paragraph (a)(7) not
under paragraph (a)(8); waters within
the specified subcategories that are
within the 100-year flood plain of a
traditional navigable water, interstate
water, or the territorial seas or within
the 4,000 foot boundary established for
case-specific determinations under
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paragraph (a)(8) remain ‘‘similarly
situated’’ waters under paragraph (a)(7).
These similarly situated waters are
evaluated in combination for their effect
on the chemical, physical, or biological
integrity of traditional navigable waters,
interstate waters, or the territorial seas.
Additional details about the casespecific significant nexus analysis are
found in section 4 below.
2. Waters Within the 100-Year
Floodplain of a Traditional Navigable
Water, Interstate Water, or the
Territorial Seas and Waters Within
4,000 Foot Boundary for Which a CaseSpecific Significant Nexus
Determination Is Required
Paragraph (a)(8) in the rule specifies
that a water that does not otherwise
meet the definition of adjacency is
evaluated on a case-specific basis for
significant nexus under this paragraph
where it is located within the 100-year
floodplain of a traditional navigable
water, interstate water, or the territorial
seas or within 4,000 feet of the high tide
line or ordinary high water mark of a
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary.
Although these waters are not
considered similarly situated by rule,
waters under this paragraph can be
determined on a case-specific basis to be
similarly situated. This is a change from
the proposal which would have allowed
for a similarly situated analysis and
significant nexus determination for any
water, anywhere in the region. Under
the rule, the waters specified in
paragraph (a)(7) and waters that meet
the requirements in paragraph (a)(8) are
the only waters for which a case-specific
significant nexus determination may be
made.
Under paragraph (a)(8), only waters
that are within the 100-year floodplain
of a traditional navigable water,
interstate water, or the territorial seas or
within the 4,000 foot boundary can be
evaluated on a case-specific basis for
significant nexus to a traditional
navigable water, interstate water, or the
territorial seas. If a portion of the water
is located within the 100-year
floodplain of a traditional navigable
water, interstate water, or the territorial
seas or 4,000 feet of the ordinary high
water mark or high tide line of a
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary, the
entire water will be considered to be
within the boundaries for paragraph
(a)(8) and will undergo a case-specific
significant nexus determination. Under
this provision, if the 100-year floodplain
of a traditional navigable water,
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interstate water, or the territorial seas
extends beyond 4,000 feet of the
ordinary high water mark, a water, that
is not otherwise jurisdictional under the
rule, within that floodplain will be
evaluated under the 100-year floodplain
boundary of paragraph (a)(8). A water
within the boundaries must be
evaluated on a case-specific basis for not
only a significant nexus but also for a
determination of whether there are any
waters with which the waters is
similarly situated. Waters identified in
paragraph (a)(8) may not be combined
with waters identified in paragraph
(a)(6) for purposes of the significant
nexus analysis, but may be combined
with similarly situated waters located in
the same point of entry watershed. If
waters identified in paragraph (a)(8) also
meet the definition of adjacency under
paragraph (a)(6), they are jurisdictional
as ‘‘adjacent waters’’ and do not need a
case-specific significant nexus analysis.
Under paragraph (a)(8), for example, the
agencies would evaluate on a casespecific basis whether a low-centered
polygonal tundra and patterned ground
bog in an area with a small floodplain
and located beyond the 1,500 foot
boundary but within the 100-year
floodplain of a traditional navigable
water, interstate water, or the territorial
seas or within the 4,000 foot boundary,
or a wetland in which normal farming,
ranching, or silviculture activities occur,
as those terms are used in section 404(f)
of the Clean Water Act and its
implementing regulations, has a
significant nexus as defined in the rule.
Waters identified in the subcategories
in paragraph (a)(7) are evaluated under
paragraph (a)(7) only; the provisions of
paragraph (a)(8), including the
boundaries in paragraph (a)(8), do not
apply to paragraph (a)(7) waters. The
significant nexus analysis for waters
under paragraph (a)(8) will then
consider the waters individually or, if it
is determined that there are similarly
situated waters, as a group of waters
within a point of entry watershed for
their effect on the chemical, physical, or
biological integrity of traditional
navigable waters, interstate waters, or
the territorial seas.
Some commenters asked how
wetlands underlain by permafrost
would be treated under this rule. Waters
subject to case-specific review under
paragraph (a)(8) will include areas
determined to meet the technical
definition of ‘‘wetlands’’ because they
have the required hydrology, vegetation,
and soils. The presence of permafrost is
not itself determinative of whether a
particular area satisfies the three
parameter requirement needed to be
wetlands under the rule. This is true
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under existing regulations and remains
unchanged in this rule. Because the
definition of wetland does not change
under the rule, the agencies do not
anticipate the rule will alter the current
scope of CWA jurisdiction over
wetlands underlain by permafrost.
a. Summary of Rationale for CaseSpecific Significant Nexus Analysis
Within 100-Year Floodplain of a
Traditional Navigable Water, Interstate
Water, or the Territorial Seas
As discussed in Section III, above, the
scientific literature supports that
wetlands and open waters in
floodplains are physically, chemically,
and biologically connected to
downstream traditional navigable
waters, interstate waters, or the
territorial seas and significantly affect
the integrity of such waters. The Science
Report concludes that wetlands and
open waters located in ‘‘floodplains are
physically, chemically and biologically
integrated with rivers via functions that
improve downstream water quality,
including the temporary storage and
deposition of channel-forming sediment
and woody debris, temporary storage of
local ground water that supports
baseflow in rivers, and transformation
and transport of stored organic matter.’’
Science Report at ES–2 to ES–3. As
described in the Science Report and the
Technical Support Document, such
waters act as the most effective buffer to
protect downstream waters from
nonpoint source pollution (such as
nitrogen and phosphorus), provide
habitat for breeding fish and aquatic
insects that also live in streams, and
retain floodwaters, sediment, nutrients,
and contaminants that could otherwise
negatively impact the condition or
function of downstream waters. As
discussed above, in defining waters as
adjacent, and therefore categorically
jurisdictional, the agencies established a
1,500 foot boundary for waters located
within the 100-year floodplain of a
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary in
order to protect vitally important waters
while at the same time providing a
practical and implementable rule. In
light of the science on the functions
provided by floodplain waters and
wetlands, waters and wetlands within
the 100-year floodplain of traditional
navigable waters, interstate waters, or
the territorial seas are likely to provide
those functions for traditional navigable
waters, interstate waters, or the
territorial seas. However, because the
100-year floodplain of a traditional
navigable water can, in some case be
quite large, the agencies concluded it
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was reasonable to subject waters and
wetlands in the 100-year floodplain that
are beyond 1,500 feet of the ordinary
high water mark, and therefore do not
meet the definition of ‘‘neighboring,’’ to
a case-specific significant nexus
analysis rather than concluding that
such waters are categorically
jurisdictional. This inclusion of a casespecific analysis for such floodplain
waters is supported by the SAB. The
SAB concluded that ‘‘distance should
not be the sole indicator used to
evaluate the connection of ‘other waters’
to jurisdictional waters.’’ SAB 2014b at
3. In allowing the case-specific
evaluation of waters within the 100-year
floodplain of a traditional navigable
water, interstate water, or the territorial
seas that do not meet the definition of
adjacency, the agencies are allowing for
the functional relationship of those
floodplain waters to be considered
regardless of distance. The SAB also
supported the Science Report’s
conclusion that ‘‘the scientific literature
strongly supports the conclusions that
streams and ‘bidirectional’ floodplain
wetlands are physically, chemically,
and/or biologically connected to
downstream navigable waters; however,
these connections should be considered
in terms of a connectivity gradient.’’
SAB 2014a at 1. In addition, the SAB
noted, ‘‘the literature review does
substantiate the conclusion that
floodplains and waters and wetlands in
floodplain settings support the physical,
chemical, and biological integrity of
downstream waters.’’ Id. at 3.
The agencies do not anticipate that
there will be numerous circumstances
in which this provision will be utilized
because relatively few traditional
navigable waters will have floodplains
larger than 4,000 feet (the other
threshold in paragraph (a)(8) for waters
regardless of floodplain). Further, the
agencies recognize that extensive areas
of the nation’s floodplains have been
affected by levees and dikes which
reduce the scope of flooding. In these
circumstances, the scope of the 100-year
floodplain is also reduced and is
reflected in FEMA mapping used by the
agencies. In circumstances where there
is little or no alteration of the floodplain
and it remains relatively broad, the
agencies will explicitly consider
distance between the water being
evaluated and traditional navigable
water, interstate water, or the territorial
seas when making a case-specific
significant nexus determination. Based
on the science concerning the important
functions provided by floodplain waters
and wetlands, the agencies established
this provision to ensure that truly
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important waters may still be protected
on a case-specific basis. By using the
100-year floodplain and limiting the
provision to traditional navigable
waters, interstate waters, or the
territorial seas, the agencies are
reasonably balancing the protection of
waters that may have a significant nexus
with the goal of providing additional
certainty.
b. Summary of Rationale for CaseSpecific Significant Nexus Analysis
Within 4,000 Foot Boundary
The agencies establish a provision in
the rule for case-specific significant
nexus determinations because the
agencies concluded that some waters
located beyond the distance limitations
established for ‘‘adjacent waters’’ can
have significant chemical, physical, and
biological connections to and effects on
traditional navigable waters, interstate
waters, or the territorial seas. The
agencies reasonably identified the 4,000
foot boundary for these case-specific
significant nexus determinations by
balancing consideration of the science
and the agencies’ expertise and
experience in making significant nexus
determinations with the goal of
providing clarity to the public while
protecting the environment and public
health. The agencies’ experience has
shown that the vast majority of waters
where a significant nexus has been
found, and which are therefore
important to protect to achieve the goals
of the Act, are located within the 4,000
foot boundary. Moreover, because of the
unique status under the CWA of
traditional navigable waters, interstate
waters, and the territorial seas, the 100year floodplain boundary for these
waters provides another means of
identifying on a case-specific basis those
waters that significantly affect
traditional navigable waters, interstate
waters or the territorial seas. The
agencies’ balancing of these
considerations is consistent with the
statute and the Supreme Court opinions.
The agencies decided that it is
important to promulgate a rule that not
only protects the most vital of our
Nation’s waters, but one that is practical
and provides sufficient boundaries so
that the public reasonably understands
where CWA jurisdiction ends.
The agencies’ decision to establish a
provision that authorizes case-specific
significant nexus analysis for waters
within 4,000 feet is based on a number
of factors. These waters may be located
within the floodplain of a traditional
navigable water, interstate water, the
territorial seas, impoundment, or
covered tributary. Section IV.G. and the
Technical Support Document discuss
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the importance of floodplain waters on
the chemical, physical, and biological
integrity of downstream traditional
navigable waters, interstate waters, or
the territorial seas. For purposes of
clarity and to provide regulatory
certainty, the agencies decided to use
distance boundaries within the 100-year
floodplain to define adjacency for
floodplain waters. Under the rule, the
only floodplain waters that are
specifically identified as being
jurisdictional as ‘‘adjacent’’ are those
located in whole or in part within the
100-year floodplain and not more than
1,500 feet of the ordinary high water
mark of jurisdictional waters.
Similarly, due to the many functions
that waters located within 4,000 feet of
the high tide line of a traditional
navigable water or the territorial seas
provide and their often close
connections to the surrounding
traditional navigable waters, science
supports the agencies’ determination
that such waters are rightfully evaluated
on a case-specific basis for significant
nexus to a traditional navigable water or
the territorial seas. Waters within 4,000
feet of the ordinary high water mark of
a traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary may
fall within the riparian areas of such
waters. As discussed in section IV.G., in
response to comments regarding the
uncertainty of the term ‘‘riparian area,’’
the agencies removed the term from the
definition of ‘‘neighboring.’’ However,
the agencies continue to recognize that
science is clear that wetlands and open
waters in riparian areas individually
and cumulatively can have a significant
effect on the chemical, physical, or
biological integrity of downstream
waters. Thus, the rule allows for a casespecific determination of significant
nexus for waters located within 4,000
feet of the high tide line or the ordinary
high water mark of a traditional
navigable water, interstate water, the
territorial seas, impoundment, or
covered tributary.
The agencies have always recognized
that adjacency is bounded by proximity,
and the rule adds additional clarity to
adjacency by bounding what can be
considered neighboring. The science is
clear that a water’s proximity to
downstream waters influences its
impact on those waters. The Science
Report states, ‘‘[s]patial proximity is one
important determinant of the
magnitude, frequency and duration of
connections between wetlands and
streams that will ultimately influence
the fluxes of water, materials and biota
between wetlands and downstream
waters.’’ Science Report at ES–11.
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Generally, waters that are closer to a
jurisdictional water are more likely to be
connected to that water than waters that
are farther away. A case-specific
analysis for waters located within 4,000
feet of the high tide line or the ordinary
high water mark of a traditional
navigable water, interstate water, the
territorial seas, impoundment, or
covered tributary allows such waters to
be considered jurisdictional only where
they meet the significant nexus
requirements. Even where not within a
100-year floodplain, waters within 4,000
feet of the high tide line or the ordinary
high water mark of a traditional
navigable water, interstate water, the
territorial seas, impoundment, or
covered tributary can have significant
chemical, physical, and biological
connections with traditional navigable
waters, interstate waters, or the
territorial seas.
As noted previously, in response to
comments concerned that there were no
bounds in the proposed rule on how far
a surface hydrologic connection could
be for purposes of adjacency, the
agencies did not include surface
hydrologic connections as its own factor
for determining adjacency in the final
rule. Such connections, however, are
relevant in a case-specific significant
nexus determination under paragraph
(a)(8). For example, waters located
within 4,000 feet of the high tide line or
the ordinary high water mark of a
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary that
contribute confined surface flow to a
downstream water can have important
hydrologic connections to and effects on
that downstream water such as the
attenuation and cycling of nutrients that
would otherwise effect downstream
water quality.
The agencies’ decision to establish the
case-specific provision at paragraph
(a)(8), including the boundaries, was
also informed by the knowledge that
waters located within 4,000 feet of the
high tide line or the ordinary high water
mark of a traditional navigable water,
interstate water, the territorial seas,
impoundment, or covered tributary can
have a confined surface or shallow
subsurface connection to such a water.
In order to provide the clarity and
certainty that many commenters
requested regarding ‘‘adjacent waters,’’
the rule does not define ‘‘neighboring’’
to include all waters with confined
surface or shallow subsurface
connections.
However, the agencies recognize that
the science demonstrates that waters
with a confined surface or shallow
subsurface connection to jurisdictional
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waters can have important effects on
downstream waters. For purposes of a
case-specific significant nexus analysis
under the rule, a shallow subsurface
hydrologic connection is lateral water
flow over a restricting layer in the top
soil horizons, or a shallow water table
which fluctuates within the soil profile,
sometimes rising to or near the ground
surface. In addition, water can move
within confined man-made subsurface
conveyance systems such as drain tiles
and storm sewers, and in karst
topography. Confined subsurface
systems can move water, and potential
contaminants, directly to surface waters
and rapidly without the opportunity for
nutrient or sediment reduction along the
pathway.
Shallow subsurface connections move
quickly through the soil and impact
surface water directly within hours or
days rather than the years it may take
long pathways to reach surface waters.
See Technical Support Document. Tools
to assess shallow subsurface flow
include reviewing the soils information
from the NRCS Soil Survey, which is
available for nearly every county in the
United States. When assessing whether
a water within the 4,000 foot boundary
performs any of the functions identified
in the rule’s definition of significant
nexus, the significant nexus
determination can consider whether
shallow subsurface connections
contribute to the type and strength of
functions provided by a water or
similarly situated waters. However,
neither shallow subsurface connections
nor any type of groundwater, shallow or
deep, are themselves ‘‘waters of the
United States.’’
The proposed rule did not set a
distance threshold for case-specific
waters to be evaluated for a significant
nexus. Some commenters argued that
there should be a limitation on areas
subject to case-specific analysis while
others contended that the agencies lack
discretion to set regulatory limits that
would exclude from jurisdiction any
water meeting the significant nexus test.
The agencies disagree that the agencies
lack the authority to establish
reasonable boundaries to determine
what areas are subject to case-specific
significant nexus analysis. Nothing in
the CWA or case law mandates that the
agencies require every water feature in
the nation be subject to analysis for
significant nexus. The Supreme Court
has made clear that the agencies have
the authority and responsibility to
determine the limits of CWA
jurisdiction, and establishing
boundaries based on agency judgment,
expertise and experience in
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administering the statute is at the core
of the agencies authority and discretion.
After weighing the scientific
information about these waters’
connectivity and importance to
protecting downstream waters, the
agencies’ considerable experience
making jurisdictional determinations,
the objective of enhancing regulatory
clarity and consistent with the statute
and the caselaw, the agencies decided to
set a boundary of 4,000 feet for casespecific significant nexus analysis for
waters that do not otherwise meet the
requirements of paragraphs (a)(1)
through (a)(7). Tying this provision for
case-specific significant nexus analysis
to distance informed by the science, and
the agencies’ experience and expertise,
as spatial proximity is a key contributor
to connectivity among waters. Science
Report at ES–11. Distance is by no
means the sole factor, and aquatic
functions will play a prominent role in
determining whether specific waters
covered under this aspect of paragraph
(a)(8) have a significant nexus. In light
of the role spatial proximity plays in
connectivity and the objective of
enhancing regulatory clarity,
predictability and consistency, the
agencies conclude that establishing a
boundary for this aspect of waters
subject to case-specific significant nexus
analysis based on distance is reasonable.
While, for purposes of this national
rule, distance is a reasonable and
appropriate measure for identifying
where this case-specific significant
nexus analysis will be conducted, the
science does not point to any particular
bright line delineating waters that have
a significant nexus from those that do
not. The Science Report concluded that
connectivity of streams and wetlands to
downstream waters occurs along a
gradient. The evidence unequivocally
demonstrates that the stream channels
and floodplain wetlands or open waters
that together form river networks are
clearly connected to downstream waters
in ways that profoundly influence
downstream water integrity. The
connectivity and effects of nonfloodplain wetlands and open waters
are more variable and thus more
difficult to address solely from evidence
available in peer-reviewed studies.
Science Report at ES–5. Because of this
variability, with respect to waters that
are not covered by paragraphs (a)(1)
through (a)(7) of the rule, the science
does not provide a precise point along
the continuum at which waters provide
only speculative or insubstantial
functions to downstream waters.
Like connectivity itself, there is also
a continuum of outcomes associated
with picking a distance threshold. A
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smaller threshold increases the
likelihood that waters that could have a
significant nexus will not be analyzed
and therefore not subject to the Act; a
larger threshold reduces that possibility,
but also means that agency and the
public’s resources are expended
conducting significant nexus analyses
on waters that have a lower likelihood
of meriting the Act’s protection.
Recognizing that there is no optimal
line, in selecting both the 100-year
floodplain for and the 4,000 foot
boundaries the agencies looked
principally to the extensive experience
the Corps has gained in making
significant nexus determinations since
the Rapanos decision. As noted in
Section III above, since the Rapanos
decision, the agencies have developed
extensive experience making significant
nexus determinations, and that
experience and expertise informed the
judgment of the agencies in establishing
both the 100-year floodplain boundary
and the 4,000 foot boundary. The
agencies have made determinations in
every state in the country, for a wide
range of waters in a wide range of
conditions. The vast majority of the
waters that the Corps has determined
have a significant nexus are located
within 4,000 feet of a jurisdictional
tributary, traditional navigable or
interstate water, or the territorial seas.
Therefore, the agencies conclude that
the 100-year floodplain and 4,000 foot
boundaries in the rule will sufficiently
capture for analysis those waters that
are important to protect to achieve the
goals of the Clean Water Act.
The agencies acknowledge that, as
with any meaningful boundary, some
waters that could be found
jurisdictional lie beyond the boundary
and will not be analyzed for significant
nexus. The agencies minimize that risk
by also establishing a provision in
paragraph (a)(8) for case-specific
significant nexus analysis of waters
located within the 100-year floodplain
of a traditional navigable water,
interstate water, or the territorial seas.
While in the agencies’ experience the
vast majority of wetlands with a
significant nexus are located within the
4,000 foot boundary, it is the agencies’
experience that there are a few waters
that have been determined to be
jurisdictional that are located beyond
this boundary, typically due to a surface
or shallow subsurface hydrologic
connections. Nonetheless, the agencies
have weighed these considerations and
concluded that the value of enhancing
regulatory clarity, predictability and
consistency through a distance limit
outweigh the likelihood that a distinct
minority of waters that might be shown
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to meet the significant nexus test will
not be subject to analysis. In the
agencies’ experience, requiring an
evaluation of significant nexus for
waters covered by paragraph (a)(8)
should capture the vast majority of
waters having a significant nexus to the
downstream waters. The agencies
therefore conclude that that adoption of
the 4,000 foot boundary is reasonable.
The rule’s requirements for these
waters, coupled with those for ‘‘adjacent
waters,’’ create an integrated approach
that tailors the regulatory regime based
on the science and the agencies’ policy
objectives. Determining by rule that
covered adjacent waters have a
significant nexus follows the science,
achieves regulatory clarity and
predictability, and avoids expenditure
of agency and public resources on casespecific significant nexus analysis.
Similarly, providing for case-specific
significant nexus analysis for waters
that are not adjacent but within the
4,000 foot distance limit, as well as
those within the 100-year floodplain of
a traditional navigable water, interstate
water, or the territorial seas, is
consistent with science and agency
experience, will ensure protection of the
important waters whose protection will
advance the goals of the Clean Water
Act, and will greatly enhance regulatory
clarity for agency staff, regulated parties,
and the public.
For these reasons, the agencies
decided to allow case-specific
determinations of significant nexus for
waters located within the 100-year
floodplain of a traditional navigable
water, interstate water, or the territorial
seas and for waters located within 4,000
feet of the high tide line or the ordinary
high water mark of a traditional
navigable water, an interstate water, the
territorial seas, an impoundment, or a
covered tributary. Under the rule, these
waters are jurisdictional only where
they individually or cumulatively (if it
is determined that there are other
similarly situated waters) have a
significant nexus to traditional
navigable waters, interstate waters, or
the territorial seas. Additional scientific
and policy rationale for including such
waters as waters that can be evaluated
on a case-specific basis can be find in
the Technical Support Document.
The agencies emphasize that they
fully support efforts by States and tribes
to protect under their own laws any
additional waters, including locally
special waters that may not be within
the jurisdiction of the CWA as the
agencies have interpreted its scope in
this rule. Indeed, the promulgation of
the 100-year floodplain and 4000 foot
boundaries for purposes of a case-
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specific analysis of significant nexus
does not foreclose states from acting
consistent with their state authorities to
establish protection for waters that fall
outside of the protection of the CWA. In
promulgating the 4,000 foot boundary,
the agencies have balanced protection
and clarity, scientific uncertainties and
regulatory experience, and established a
line that is, in their judgment,
reasonable and consistent with the
statute and its goals and objectives.
3. Case-Specific Significant Nexus
Determinations
Only waters identified in paragraphs
(a)(7) or (a)(8) of the rule require a casespecific determination of significant
nexus. This section discusses the
definition of significant nexus in the
rule and how the agencies will make
case-specific significant nexus
determinations under the rule.
a. Definition of Significant Nexus
Paragraph (c)(5) of the rule defines the
term ‘‘significant nexus’’ to mean a
significant effect (more than speculative
or insubstantial) on the chemical,
physical, or biological integrity of a
traditional navigable water, interstate
water, or the territorial seas. Waters,
including wetlands, are evaluated either
alone, or in combination with other
similarly situated waters in the region,
based on the functions the evaluated
waters perform. Functions to be
considered for the purposes of
determining significant nexus are
sediment trapping, nutrient recycling,
pollutant trapping, transformation,
filtering and transport, retention and
attenuation of floodwaters, runoff
storage, contribution of flow, export of
organic matter, export of food resources,
and provision of life-cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in traditional navigable waters,
interstate waters, or the territorial seas.
The agencies’ definition of significant
nexus is based upon the language in
SWANCC and Rapanos. The definition
is also consistent with current practice,
where field staff evaluate the functions
of the waters in question and the effects
of these functions on downstream
waters. In order to add clarity and
transparency to the definition of
significant nexus, the agencies have
listed in the definition the functions
that will be considered in a significant
nexus analysis. These functions are
consistent with the agencies’ scientific
understanding of the functioning of
aquatic ecosystems. A water does not
need to perform all of the functions
listed in paragraph (c)(5) in order to
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have a significant nexus. Depending
upon the particular water and the
functions it provides, if a water, either
alone or in combination with similarly
situated waters, performs just one
function, and that function has a
significant impact on the integrity of a
traditional navigable water, interstate
water, or the territorial seas, that water
would have a significant nexus.
Case-specific determinations of
significant nexus require paragraph
(a)(7) or (a)(8) waters to be evaluated
either alone, or in combination with
other similarly situated waters in the
region. In the rule, the agencies interpret
the phrase ‘‘in the region’’ to mean the
watershed that drains to the nearest
traditional navigable water, interstate
water, or the territorial seas through a
single point of entry. See Section III. In
circumstances where the single point of
entry watershed includes waters that are
identified under paragraph (a)(7) and
waters that are subject to analysis under
paragraph (a)(8), those waters will be
analyzed separately under the
provisions of those paragraphs.
In a case-specific analysis of
significant nexus, the agencies
determine whether the water they are
evaluating, in combination with other
similarly situated waters in the region,
has a significant effect on the chemical,
physical, or biological integrity of the
nearest traditional navigable water,
interstate water, or the territorial seas.
As noted previously, the agencies
evaluate the listed functions in
paragraph (c)(5) as part of that
evaluation to determine if the water has
an impact that is more than speculative
or insubstantial.
b. Conducting Case-Specific Significant
Nexus Determinations Under
Paragraphs (a)(7) and (a)(8)
The significant nexus analysis for
waters assessed under paragraphs (a)(7)
and (a)(8) is a three-step process: First,
the region for the significant nexus
analysis must be identified—under the
rule, it is the watershed which drains to
the nearest traditional navigable water,
interstate water or territorial sea;
second, any similarly situated waters
must be identified—under the rule, that
is waters that function alike and are
sufficiently close to function together in
affecting downstream waters; and third,
the waters are evaluated individually or
in combination with any identified
similarly situated waters in the single
point of entry watershed to determine if
they significantly impact the chemical,
physical or biological integrity of the
traditional navigable water, interstate
water or the territorial seas.
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i. ‘‘In the Region’’—The Point of Entry
Watershed
As discussed in Section III of the
preamble and established in the
definition of ‘‘significant nexus,’’ the
region for purposes of a significant
nexus analysis is the watershed that
drains to the nearest traditional
navigable water, interstate water, or the
territorial seas. The first step of the
analysis is to identify the point of entry
watershed that the water being
evaluated under paragraphs (a)(7) or
(a)(8) drains to. This point of entry
approach identifies the nearest
traditional navigable water, interstate
water, or the territorial seas that the
water being evaluated and any similarly
situated waters flow to and delineates
the watershed of that nearest traditional
navigable water, interstate water, or the
territorial seas. The point of entry
watershed is the area drained by the
nearest traditional navigable water,
interstate water, or the territorial seas
and is typically defined by the
topographic divides between one
traditional navigable water, interstate
water, or the territorial seas and another.
Available mapping tools, such as
those that are based on the NHD,
topographic maps, and elevation data,
can be used to demarcate boundaries of
the single point of entry watershed. As
discussed in Section III and in the
Technical Support Document, the single
point of entry watershed represents the
scientifically appropriate sized area for
conducting a case-specific significant
nexus evaluation in most cases.
In the arid West, the agencies
recognize there may be situations where
the single point of entry watershed is
very large, and it may be reasonable to
evaluate all similarly situated waters in
a smaller watershed. Under those
circumstances, the agencies may
demarcate adjoining catchments
surrounding the water to be evaluated
that, together, are generally no smaller
than a typical 10-digit hydrologic unit
code (HUC–10) watershed in the same
area. The area identified by this
combination of catchments would be
the ‘‘region’’ used for conducting a
significant nexus evaluation under
paragraphs (a)(7) or (a)(8) under those
situations. The basis for such an
approach in very large single point of
entry watersheds in the arid West
should be documented in the
jurisdictional determination.
ii. ‘‘Similarly Situated’’
Second, the agencies determine if the
water or waters to be evaluated are
similarly situated. The waters identified
in paragraph (a)(7) are similarly situated
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by rule and shall be combined with
other waters of the same category
located in the same watershed that
drains to the nearest traditional
navigable water, interstate water, or the
territorial seas with no need for a casespecific similarly situated finding.
Under paragraph (a)(7), only waters of
the same subparagraph in the point of
entry watershed can be considered as
similarly situated. For example, only
pocosins may be evaluated with other
pocosins in the same point of entry
watershed. Pocosins in different point of
entry watersheds cannot be combined,
and pocosins cannot be combined with
Carolina bays under paragraph (a)(7),
even where they occur in the same point
of entry watershed.
Unlike waters evaluated under
paragraph (a)(7), the waters specified at
paragraph (a)(8) require a determination
whether they are similarly situated.
Under this step, the agencies apply
factors in the determination of when
waters evaluated under paragraph (a)(8)
should be considered either
individually or in combination for
purposes of a significant nexus analysis.
A determination of ‘‘similarly situated’’
requires an evaluation of whether a
group of waters in the region that meet
the distance thresholds set out under
paragraph (a)(8) can reasonably be
expected to function together in their
effect on the chemical, physical, or
biological integrity of downstream
traditional navigable waters, interstate
waters, or the territorial seas.
Similarly situated waters can be
identified as sufficiently close together
for purposes of this paragraph of the
regulation when they are within a
contiguous area of land with relatively
homogeneous soils, vegetation, and
landform (e.g., plain, mountain, valley,
etc.). In general, it would be
inappropriate, for example, to consider
waters as ‘‘similarly situated’’ under
paragraph (a)(8) if these waters are
located in different landforms, have
different elevation profiles, or have
different soil and vegetation
characteristics, unless the waters
perform similar functions and are
located sufficiently close to a ‘‘water of
the United States’’ to allow them to
consistently and collectively function
together to affect a traditional navigable
water, interstate water, or the territorial
seas. In determining whether waters
under paragraph (a)(8) are sufficiently
close to each other the agencies will also
consider hydrologic connectivity to
each other or a jurisdictional water.
In determining whether groups of
waters under paragraph (a)(8) perform
‘‘similar functions’’ the agencies will
consider functions such as habitat,
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water storage, sediment retention, and
pollution sequestration. In addition,
consideration of wetland/water type and
landscape location are relevant for
determining if the waters are similarly
situated. For example, Texas coastal
sand sheet wetlands that form a
complex of wetlands with other
wetlands of the same type on the
landscape and are densely located may
very well be similarly situated and
considered in combination with other
Texas coastal sand sheet wetlands in the
same single point of entry watershed.
However, under paragraph (a)(8), waters
do not need to be of the same type (as
they do in paragraph (a)(7)) to be
considered similarly situated. As
described above, waters are similarly
situated under paragraph (a)(8) where
they perform similar functions or are
located sufficiently close to each other,
regardless of type. The agencies will
consider the hydrologic, geomorphic,
and ecological characteristics and
circumstances of the waters under
consideration. Examples include:
Documentation of chemical, physical, or
biological interactions of the similarly
situated waters; aerial photography;
USGS and state and local topographical
or terrain maps and information; NRCS
soil survey maps and data; other
available geographic information
systems (GIS) data; National Wetlands
Inventory maps where wetlands meet
the CWA definition; and state and local
information. The evaluation will use
any available site information and
pertinent field observations where
available, relevant scientific studies or
data, or other relevant jurisdictional
determinations that have been
completed in the region.
Only those waters that do not meet
the requirements in paragraph (a)(1)
through (a)(6) are to be considered in
case-specific significant nexus
determinations; subcategory waters that
meet the provisions in paragraph (a)(1)
through (a)(6) are per se jurisdictional
without the need for a significant nexus
determination. For example, waters that
are identified under paragraph (a)(6) are
adjacent and are not subject to a casespecific significant nexus evaluation
under paragraph (a)(7) or (a)(8). Waters
evaluated under paragraph (a)(7) cannot
be combined with waters identified in
paragraph paragraph (a)(6) or (a)(8), and
waters evaluated under paragraph (a)(8)
cannot be combined with waters
identified in paragraph (a)(6) or (a)(7).
For example, Prairie potholes being
evaluated under paragraph (a)(7) may
not be combined with Prairie potholes
that are per se jurisdictional under
paragraph (a)(6) that meet the definition
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of adjacent. When a water meets the
specifications at both paragraphs (a)(7)
and (a)(8), it can only be evaluated
under paragraph (a)(7). That is, for
example, if a wetland is a Western
vernal pool and is also within 4,000 feet
of the ordinary high water mark of a
covered tributary, it can only be
assessed for significant nexus under
paragraph (a)(7) in combination with
other Western vernal pools in the point
of entry watershed. Unlike paragraph
(a)(8), there is no distance threshold for
waters evaluated under paragraph
(a)(7)—that is, waters in the paragraph
(a)(7) subcategories that are more than
4,000 feet from the high tide line or the
ordinary high water mark of a
traditional navigable water, interstate
water, the territorial seas,
impoundment, or covered tributary or
are beyond the 100-year floodplain of an
traditional navigable water, interstate
water, or the territorial seas are to be
included in combination in a significant
nexus analysis.
iii. Significant Nexus Analysis for
Paragraph (a)(7) and (a)(8) Waters
Third, the agencies evaluate waters
individually or in combination with any
identified similarly situated waters in
the single point of entry watershed to
determine if they significantly impact
the chemical, physical, or biological
integrity of the traditional navigable
water, interstate water, or the territorial
seas. For purposes of determining
significant nexus under paragraph (a)(7),
all waters of the specified subcategory
are to be considered in combination in
the point of entry watershed, as those
waters are similarly situated. For
purposes of determining significant
nexus under paragraph (a)(8),
depending on the results of step two, a
water within the boundaries in
paragraph (a)(8) is evaluated either
alone or in combination with other
similarly situated waters in the region.
For example, in the case where the
agencies have determined that a
particular water under paragraph (a)(8)
is not similarly situated, it is evaluated
individually for significant nexus; the
water cannot be aggregated if it is not
similarly situated with other such
waters.
The analysis will include an
evaluation of the functions listed in
paragraph (c)(5) of the rule, which
defines significant nexus. A water has a
significant nexus when any single
function or combination of functions
performed by the water, alone or
together with similarly situated waters
in the region, contributes significantly
to the chemical, physical, or biological
integrity of the nearest traditional
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navigable water, interstate water, or the
territorial seas. A water may be
determined to have a significant nexus
based on performing any of the
following functions: sediment trapping,
nutrient recycling, pollutant trapping,
transformation, filtering, and transport,
retention and attenuation of
floodwaters, runoff storage, contribution
of flow, export of organic matter, export
of food resources, or provision of life
cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding,
spawning, or use as a nursery area) for
species located in a traditional
navigable water, interstate water, or the
territorial seas.
For purposes of paragraph (c)(5)(ix), a
species is located in a traditional
navigable water, interstate water, or the
territorial seas if such a water is a
typical type of habitat for at least part
of the life cycle of the species. For
example, amphibians and many reptiles
can use a traditional navigable water,
interstate water, or the territorial seas
for part of their life cycle needs.
When evaluating a water individually
or in combination with other similarly
situated waters for the presence of a
significant nexus to a traditional
navigable water, interstate water, or the
territorial seas, a variety of factors will
influence the chemical, physical, or
biological connections the water has
with the downstream traditional
navigable water, interstate water, or the
territorial seas, including distance from
a jurisdictional water, the presence of
surface or shallow subsurface
hydrologic connections, and density of
waters of the same type (if it has been
concluded that such waters can be
evaluated in combination). The
likelihood of a significant connection is
greater with increasing size and
decreasing distance from the identified
traditional navigable water, interstate
water, or the territorial seas, as well as
with increased density of the waters for
such waters that can be considered in
combination as similarly situated
waters. In addition, the presence of a
surface or shallow subsurface
hydrologic connection can influence the
impact that a water has with
downstream waters.
In many cases, the presence of a
hydrologic connection increases the
strength of the impact of the
downstream traditional navigable water,
interstate water, or the territorial seas.
However, a hydrologic connection is not
necessary to establish a significant
nexus, because, as Justice Kennedy
stated, in some cases the lack of a
hydrologic connection would be a sign
of the water’s function in relationship to
the traditional navigable water,
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interstate water, or the territorial seas.
These functional relationships include
retention of floodwaters or pollutants
that would otherwise flow downstream
to the traditional navigable water,
interstate water, or the territorial seas.
See 547 U.S. at 775 (citations omitted)
(J. Kennedy) (‘‘it may be the absence of
an interchange of waters prior to the
dredge and fill activity that makes
protection of the wetlands critical to the
statutory scheme’’). The Science Report
concludes, ‘‘[s]ome effects of nonfloodplain wetlands on downstream
waters are due to their isolation, rather
than their connectivity. Wetland ‘sink’
functions that trap materials and
prevent their export to downstream
waters (e.g., sediment and entrained
pollutant removal, water storage) result
because of the wetland’s ability to
isolate material fluxes.’’ Science Report
at ES–4. For example, a report that
reviewed the results of multiple
scientific studies concluded that
depressional wetlands lacking a surface
outlet functioned together to
significantly reduce or attenuate
flooding. See Science Report and
Technical Support Document. Even
when they lack a surface hydrologic
connection to downstream traditional
navigable waters, interstate waters, or
the territorial seas, Prairie potholes, for
instance, cumulatively can store large
volumes of water, impacting streamflow
and reducing flooding downstream, and
several studies have quantified the large
storage capacity of Prairie pothole
complexes. This water storage function
is estimated to hold tens of millions of
cubic meters of water, including for
example Prairie potholes located in the
watersheds of Devils Lake and the Red
River of the North, which have both had
a long history of flooding. Where Prairie
potholes lack a surface hydrologic
connection, this water storage capacity
is particularly effective in reducing
downstream flooding and can have a
significant effect on downstream
traditional navigable waters, interstate
waters, or the territorial seas. Thus, even
when lacking a surface hydrologic
connection, a water can still have a
significant effect on the chemical or the
biological integrity of downstream
traditional navigable waters, interstate
waters, or the territorial seas.
The rule recognizes that not all waters
have the requisite connection to
traditional navigable waters, interstate
waters, or the territorial seas sufficient
to be determined jurisdictional. Waters
with a significant nexus must
significantly affect the chemical,
physical, or biological integrity of a
downstream traditional navigable water,
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interstate water, or the territorial seas,
and the requisite nexus must be more
than ‘‘speculative or insubstantial.’’
Rapanos at 780.
Evidence of chemical connectivity
and the effect on waters can be found by
identifying the properties of the water in
comparison to the identified traditional
navigable water, interstate water, or the
territorial seas; signs of retention,
release, or transformation of nutrients or
pollutants; and the effect of landscape
position on the strength of the
connection to the nearest ‘‘water of the
United States,’’ and through it to a
traditional navigable water, interstate
water, or the territorial seas. In addition,
relevant factors influencing chemical
connectivity include hydrologic
connectivity (see physical factors,
below), surrounding land use and land
cover, the landscape setting, and
deposition of chemical constituents
(e.g., acidic deposition).
Evidence of physical connectivity and
the effect on traditional navigable
waters, interstate waters, or the
territorial seas can be found by
identifying evidence of physical
connections, such as flood water or
sediment retention (flood prevention).
Presence of indicators of hydrologic
connections between the other water
and jurisdictional water are also
indicators of a physical connection.
Factors influencing physical
connectivity include rain intensity,
duration of rain events or wet season,
soil permeability, and distance of
hydrologic connection between the
paragraph (a)(7) or (a)(8) water and the
traditional navigable water, interstate
water, or the territorial seas, depth from
surface to water table, and any
preferential flowpaths.
Evidence of biological connectivity
and the effect on waters can be found by
identifying: Resident aquatic or semiaquatic species present in the casespecific water and the tributary system
(e.g., amphibians, aquatic and semiaquatic reptiles, aquatic birds); whether
those species show life-cycle
dependency on the identified aquatic
resources (foraging, feeding, nesting,
breeding, spawning, use as a nursery
area, etc.); and whether there is reason
to expect presence or dispersal around
the case-specific water, and if so
whether such dispersal extends to the
tributary system or beyond or from the
tributary system to the case-specific
water. Factors influencing biological
connectivity include species’ life history
traits, species’ behavioral traits,
dispersal range, population size, timing
of dispersal, distance between the casespecific water and a traditional
navigable water, interstate water, or the
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territorial seas, the presence of habitat
corridors or barriers, and the number,
area, and spatial distribution of habitats.
Non-aquatic species or species such as
non-resident migratory birds do not
demonstrate a life cycle dependency on
the identified aquatic resources and are
not evidence of biological connectivity
for purposes of this rule.
For practical administrative purposes,
the rule does not require evaluation of
all similarly situated waters under
paragraph (a)(7) or (a)(8) when
concluding that those waters have a
significant nexus to a traditional
navigable water, interstate water, or
territorial sea. When a subset of
similarly situated waters provides a
sufficient science-based justification to
conclude presence of a significant
nexus, for efficiency purposes a
significant nexus analysis need not
unnecessarily require time and
resources to locate and analyze all
similarly situated waters in the entire
point of entry watershed. For example,
if a single Carolina bay or a group of
Carolina bays in a portion of the point
of entry watershed is determined to
significantly affect the chemical,
physical, or biological integrity of a
traditional navigable water, interstate
water, or the territorial seas, the analysis
does not have to document all of the
similarly situated Carolina bays in the
watershed in order to conduct the
significant nexus analysis. A conclusion
that significant nexus is lacking may not
be based on consideration of a subset of
similarly situated waters because under
the significant nexus standard the
inquiry is how the similarly situated
waters in combination affect the
integrity of the downstream water.
While the rule is clear that waters that
are jurisdictional by rule cannot be
combined with waters subject to a casespecific significant nexus analysis, the
analysis may appropriately include the
evaluation of functions of paragraph
(a)(8) waters that reach covered waters
through paragraph (a)(6) waters without
consideration of the functions
contributed by those paragraph (a)(6)
waters. The hydrologic connections
between paragraph (a)(8) waters and a
covered tributary and eventually to a
traditional navigable water, interstate
water, or the territorial seas, can often
occur through an adjacent water. This
hydrologic connection is an appropriate
part of the case-specific analysis as to
whether the paragraph (a)(8) waters,
alone or in combination with any
similarly situated paragraph (a)(8)
waters in the point of entry watershed,
provide those functions downstream
such that they significantly affect the
chemical, physical or biological
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integrity of the traditional navigable
water, interstate water, or the territorial
seas. For example, when evaluating a
wetland that is 2,500 feet from the
ordinary high water mark of an
paragraph (a)(5) water and that has
surface or shallow subsurface
connections to downstream traditional
navigable waters, interstate waters, or
the territorial seas via a wetland that is
adjacent to an paragraph (a)(4) water,
the existence of those connections is not
ignored. However, while a water’s
connections to the traditional navigable
water, interstate water, or the territorial
seas through paragraph (a)(5) through
(a)(7) waters can be considered in the
significant nexus analysis in order to
determine whether the functions of the
paragraph (a)(8) waters are provided
downstream, only the functions of the
water, along with any similarly situated
waters, being evaluated under paragraph
(a)(8) on downstream water integrity can
be included in the significant nexus
analysis.
The administrative record for a
jurisdictional determination for a water
under paragraph (a)(7) or (a)(8) will
include available information
supporting the determination. In
addition to location and other
descriptive information regarding the
water at issue, the record will include
an explanation of the rationale for the
jurisdictional conclusion and a
description of the information used.
Relevant information can come from
many sources, and need not always be
specific to the water whose
jurisdictional status is being evaluated.
Studies of the same type of water or
similarly situated waters can help to
inform a significant nexus analysis as
long as they are applicable to the water
being evaluated. In the case of
paragraph (a)(8) waters, the
administrative record will include the
rationale behind the similarly situated
analysis, including an explanation of
the data or information examined.
The agencies expect that where waters
are determined to be similarly situated
in a single point of entry watershed,
such similarly situated waters will often
be found jurisdictional through the casespecific analysis of significant nexus.
However, case-specific factors such as
distance to the traditional navigable
water, interstate water, or the territorial
seas; density or number of similarly
situated waters; individual and
cumulative size of the similarly situated
waters; soil permeability; climate; etc.,
may be considered in the determination,
and there could be cases where even
considering these waters in combination
with similarly situated waters will not
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be sufficient for waters to have a
significant nexus.
Within a single point of entry
watershed, over a period of time there
will likely be multiple jurisdictional
determinations. For paragraph (a)(7)
waters, if a case-specific significant
nexus determination has been made in
the point of entry watershed, all waters
in the subcategory in the point of entry
watershed are jurisdictional. For
paragraph (a)(8) waters, the case-specific
significant nexus analyses must use
information used in previous
jurisdictional determinations, and if a
significant nexus has been established
for one water in the watershed, then
other similarly situated waters in the
watershed would also be found to have
a significant nexus. This is because
under Justice Kennedy’s test, similarly
situated waters in the region should be
evaluated together. A positive
significant nexus determination would
then apply to all similarly situated
waters within the point of the
watershed. A negative case-specific
significant nexus evaluation under
paragraph (a)(7) or (a)(8) of all similarly
situated waters in the point of entry
watershed applies to all similarly
situated waters in that watershed.
However, as noted above, a conclusion
that significant nexus is lacking may not
be based on consideration of a subset of
similarly situated waters, because under
the significant nexus standard the
inquiry is how the similarly situated
waters in combination affect the
integrity of the downstream water. The
documentation for each case should be
complete enough to support the specific
jurisdictional determination, including
an explanation of which waters were
considered together as similarly situated
and in the same region.
4. Summary of Revisions to CaseSpecific Determinations of ‘‘Waters of
the United States’’ and Major Comments
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a. Significant Nexus
Some commenters stated concerns
over the potential for inconsistent
application of the significant nexus
analysis in a jurisdictional
determination. To address this concern
within the regulatory framework, the
agencies provide more detail regarding
the definition of significant nexus in the
rule and list the specific functions that
will be considered in the analysis. This
approach provides individual regulators
who conduct the analysis clear and
consistent parameters that they will
consider during their review in making
jurisdictional determinations and
provides transparency to the regulated
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public over which factors will be
considered.
Overall, there was support for the
concept of the single point of entry
watershed as the interpretation of ‘‘in
the region.’’ Several commenters
supported the approach that the single
point of entry watershed was an
appropriate scale to use to measure
effect on traditional navigable waters,
interstate waters, or the territorial seas.
Other commenters felt the single point
of entry watershed was too small to
capture all the benefits that waters that
do not meet the definition of adjacency
contribute. Some of the SAB panel
members thought that because surface
and ground-watershed units may not
align, watersheds might be problematic
for defining ‘‘in the region.’’ These
panel members suggested that a more
scientifically justified approach would
include surface and subsurface waters
in a watershed delineation. The
agencies have retained the single point
of entry watershed from the proposed
rule as the appropriate unit of analysis
for significant nexus in the final rule as
these watersheds are more easily
understood and easier to delineate than
those that map subsurface waters as the
SAB suggested.
With respect to the agencies’
approach to ‘‘similarly situated waters,’’
commenters offered support for
assessing waters in combination based
on their type and function, particularly
waters such as Prairie potholes.
Conversely, several commenters found
that the ability to aggregate waters that
do not meet the definition of adjacency
is over-reaching and causes uncertainty
to the regulated public. Some
commenters also attributed uncertainty
in which waters were regulated to
subjectivity in review by Federal
regulator(s). Similarly, some
commenters were concerned that waters
eligible for protection were based on an
individual analyst’s interpretation and
wanted to know how the agencies
would address consistency and
potential bias. In response, the rule lists
in paragraph (a)(7) a limited number of
subcategories of waters where waters of
the specified types have been
determined by rule to be similarly
situated for a significant nexus analysis.
This will add consistency,
predictability, and clarity, as the rule
explicitly states that such waters are
similarly situated for purposes of the
significant nexus analysis. For waters
identified under paragraph (a)(8), the
agencies have established two
limitations: Waters within the 100-year
floodplain of a traditional navigable
water, interstate water, or the territorial
seas, and waters within 4,000 foot feet
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37095
of a traditional navigable water,
interstate water, the territorial seas,
impoundment, or covered tributary. The
agencies also have established within
the definition of significant nexus at
paragraph (c)(5) criteria for determining
whether waters are similarly situated
and should therefore be analyzed in
combination. Waters identified under
paragraph (a)(8) are similarly situated
when they function alike and are
sufficiently close to function together in
affecting downstream waters. The
agencies have not determined that such
waters are categorically similarly
situated, so the agencies will base their
case-specific determinations of whether
a particular water has any similarly
situated waters on the available
information and science. The rule also
clarifies that paragraph (a)(8) waters
cannot be considered similarly situated
with ‘‘adjacent waters,’’ which are
jurisdictional by rule, and paragraph
(a)(7) waters, which have been
determined to be similarly situated by
rule. These parameters will reduce
inconsistency in reviews and add
clarity.
Similarly, several commenters
expressed concern that landowners
would not know which water bodies on
their property are subject to CWA
jurisdiction due to aggregation, as
waters on their property may be
considered similarly situated with
waters located off-site. While the rule
does not eliminate the use of casespecific significant nexus analyses, and
the concern arises from Justice
Kennedy’s phrase ‘‘similarly situated,’’
the parameters placed on waters
requiring a case-specific determination
and the clearer definition of significant
nexus address the concerns about
uncertainty and inconsistencies in
reviews. In particular, waters that are
not either one of the five identified
subcategories in paragraph (a)(7) or
within the thresholds in paragraph (a)(8)
cannot be subject to a case-specific
significant nexus analysis under the
rule. Generally, jurisdictional
determinations are conducted at the
request of an applicant or landowner for
specific waters. While the agencies
cannot arbitrarily depart from a
determination that waters are ‘‘similarly
situated,’’ landowners may provide new
information to inform subsequent
jurisdictional determinations. In
addition, owners with questions
regarding jurisdiction of waters on their
property may always consult their local
Corps District or EPA Regional Office,
which is not a change from longstanding
practice.
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b. Case-Specific Determinations
The rule provides more regulatory
certainty by narrowing the scope of
waters that can be assessed under a
case-specific significant nexus
evaluation as compared to the proposal.
These changes still allow the scientific
value of specific waters not covered in
paragraph (a)(1) through (a)(6) to be
evaluated on a case-specific basis.
In the proposal, the agencies solicited
comment regarding a variety of
approaches to the category of waters
subject to a case-specific significant
nexus analysis. In addition, the agencies
solicited comment on additional
scientific research and data that might
further inform decisions about these
waters. In particular the agencies
solicited information about whether
current scientific research and data
regarding particular types of waters are
sufficient to support the inclusion of
subcategories of types of waters, either
alone or in combination with similarly
situated waters, that can appropriately
be identified as always lacking or
always having a significant nexus. One
of these alternate approaches in the
preamble to the proposed rule was to
determine by rule that certain additional
subcategories of waters would be
jurisdictional rather than addressed
with a case-specific basis for
determining significant nexus.
Many commenters expressed support
for the agencies’ proposed approach to
case-specific waters, included
additional references to support these
waters being protected by rule, and
supported the treatment of certain
categories of waters as similarly situated
(that is, evaluating them in combination
with similarly situated waters for the
purposes of the significant nexus
analysis). Some suggested the agencies
establish jurisdiction over case-specific
waters by rule and provided detailed
information in support of their position.
Other commenters suggested additional
subcategories of waters be considered as
jurisdictional or as similarly situated by
rule, such as playa lakes, kettle lakes,
and woodland vernal pools.
However, there was a concern raised
by other commenters about what was
termed regulatory overreach and
uncertainty created by the ‘‘other
waters’’ category in the proposal. Some
commenters stated that the ‘‘other
waters’’ category in the proposal would
allow the agencies to regulate virtually
any water. To address this concern, the
rule places limits on which waters
could be subject to a case-specific
significant nexus determination, in
recognition that case-specific analysis of
significant nexus is resource-intensive
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and based on the body of science that
exists. As noted above, the agencies also
establish by rule subcategories of waters
that are ‘‘similarly situated’’ for the
purposes of a significant nexus analysis
because science supports that the
subcategory waters fall within a higher
gradient of connectivity. By not
determining that any one of the waters
available for case-specific analysis is
jurisdictional by rule, the agencies are
recognizing the gradient of connectivity
that exists and will assert jurisdiction
only when that connection and the
downstream effects are significant and
more than speculative and insubstantial.
Waters are covered under the rule
only where they are identified as
jurisdictional in paragraphs (a)(1)
through (a)(6), where they are not
excluded under paragraph (b), or where
they are within the limited number of
subcategories listed in paragraphs (a)(7)
and (a)(8) and have a case-specific
significant nexus to a traditional
navigable water, interstate water, or the
territorial seas. These limits on
jurisdiction reflect the case law and are
in response to comments requesting
greater regulatory certainty. Although
some commenters suggested additional
subcategories of waters for
consideration, such as playa lakes and
kettle lakes, the agencies at this time are
not able to determine that the available
science supports that the suggested
additional subcategories of waters as a
class have a significant nexus to
traditional navigable waters, interstate
waters, or the territorial seas. However,
to be clear, under the rule, individual
waters of the suggested additional
subcategories are jurisdictional where
they meet the requirements of
paragraphs (a)(1) through (a)(6) or (a)(8)
(e.g., a playa lake that is an interstate
water, a kettle lake that is an adjacent
water, or a woodland vernal pool that is
less than 4,000 feet from a jurisdictional
tributary and is determined on a casespecific basis to have a significant nexus
to a traditional navigable water,
interstate water, or the territorial seas).
In consideration of the variety of
views of the commenters, the Science
Report, the input from the SAB, and the
developing state of the science, the
agencies reasonably decided not to
establish jurisdiction over all waters
that do not meet the requirements of
paragraph (a)(1) through (a)(6) by rule.
Instead, the agencies established casespecific provisions for some specified
waters at paragraph (a)(7) and waters
within the boundaries at paragraph
(a)(8). This approach strikes a balance
between requests for clear boundaries
and limited case-specific reviews with
scientific support.
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I. Waters and Features That Are Not
‘‘Waters of the United States’’
In the rule, the agencies identify a
variety of waters and features that are
not ‘‘waters of the United States.’’ Prior
converted cropland and waste treatment
systems have been excluded from this
definition since 1992 and 1979,
respectively, and they remain
substantively and operationally
unchanged. Only ministerial changes to
delete an outdated cross reference are
made to the exclusion for waste
treatment systems. The agencies add
exclusions for all waters and features
identified as generally exempt in
preamble language from Federal
Register documents by the Corps on
November 13, 1986, and by EPA on June
6, 1988. This is the first time these
exclusions have been established by
rule. In addition, under prior preamble
language, the agencies retained the
authority to determine that a particular
feature generally considered nonjurisdictional was in fact a ‘‘water of the
United States.’’ The agencies do not
retain that authority for features
excluded under the rule. The agencies
for the first time also establish by rule
that certain ditches are excluded from
jurisdiction. The agencies add
exclusions for groundwater and
erosional features, as well as exclusions
for some waters that were identified in
public comments as possibly being
found jurisdictional under proposed
rule language where this was never the
agencies’ intent. These exclusions are
reflective of current agencies’ practice,
and their inclusion in the rule furthers
the agencies’ goal of providing greater
clarity over what waters are and are not
protected under the CWA. Importantly,
under the rule all waters and features
identified in paragraph (b) as excluded
will not be ‘‘waters of the United
States,’’ even if they otherwise fall
within one of the categories in
paragraphs (a)(4) through (a)(8). For
example, a ditch that is excluded under
paragraph (b)(3)(i) or (b)(3)(ii) is not
jurisdictional even when the ditch
connects directly or through another
water to a traditional navigable water,
interstate water, or the territorial seas.
The proposed rule referenced
paragraphs (a)(1) through (a)(8), but the
agencies did not intend to exclude any
traditional navigable waters, for
example, and the revision clarifies that.
Finally, nothing in the rule is intended
to change the way in which the Corps
applies individual or nationwide
permits.
The exclusions reflect the agencies’
long-standing practice and technical
judgment that certain waters and
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features are not subject to the CWA. The
exclusions are also guided by Supreme
Court cases. The significant nexus
standard arises from the case law and is
used to interpret the terms of the CWA.
Thus, a significant nexus determination
is not a purely scientific inquiry, but
rather is a determination by the agencies
in light of the statutory language, the
statute’s goals, objectives and policies,
the case law, the relevant science, and
the agencies’ technical expertise and
experience. The plurality opinion in
Rapanos also noted that there were
certain features that were not primarily
the focus of the CWA. See 547 U.S. at
734. In this section of the proposed rule,
the agencies are drawing lines and
concluding that certain waters and
features are not subject to the
jurisdiction of the Clean Water Act. The
Supreme Court has recognized that
clarifying the lines of jurisdiction is a
difficult task: ‘‘Our common experience
tells us that this is often no easy task:
The transition from water to solid
ground is not necessarily or even
typically an abrupt one. Rather, between
open waters and dry land may lie
shallows, marshes, mudflats, swamps,
bogs—in short, a huge array of areas that
are not wholly aquatic but nevertheless
fall far short of being dry land. Where
on this continuum to find the limit of
‘waters’ is far from obvious.’’ Riverside
Bayview at 132–33. The exclusions are
an important aspect of the agencies’
policy goal of providing clarity and
certainty. Just as the categorical
assertions of jurisdiction over covered
tributaries and covered adjacent waters
simplify the jurisdiction issue, the
categorical exclusions will likewise
simplify the process, and they reflect
the agencies’ determinations of the lines
of jurisdiction based on science, the
case law and the agencies’ experience
and expertise.
The existing exclusion for waste
treatment systems moves to paragraph
(b)(1) with no substantive changes. One
ministerial change is the deletion of a
cross-reference in the current language
to an EPA regulation that no longer
exists. Because the agencies are not
addressing the substance of the
exclusion, the agencies do not make
conforming changes to ensure that each
of the existing definitions of the ‘‘waters
of the United States’’ for the various
CWA programs have the exact same
language with respect to the waste
treatment system exclusion, with the
exception of deleting the crossreference.
Many commenters expressed concern
about whether the agencies’ insertion of
a comma following this ministerial
change unintentionally narrowed the
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exclusion such that all excluded waste
treatment systems must be designed to
meet the requirements of the Clean
Water Act. The commenters indicated
concerns that waste treatment systems
built before the Clean Water Act or
primarily for purposes of other
environmental laws could not be
exempt. The agencies do not intend to
change how the waste treatment
exclusion is implemented and have
deleted this proposed comma.
Continuing current practice, any waste
treatment system built in a ‘‘water of the
United States’’ would need a section
404 permit to be constructed and a
section 402 permit for discharges from
the waste treatment system into ‘‘waters
of United States.’’
A number of commenters suggested
the agencies clarify how the waste
treatment system exclusion is currently
implemented. Many comments raised
questions about stormwater systems and
wastewater reuse and whether such
facilities qualified under the waste
treatment system exclusion as part of a
complete waste treatment system. For
clarity, the agencies have identified
related exclusions in paragraphs (b)(6)
and (b)(7). Many commenters also
suggested making substantive changes
to the existing exclusion for waste
treatment systems. Because the agencies
are not making any substantive changes
to the waste treatment system exclusion
and these comments are outside the
scope of the proposed rule, the final rule
does not reflect changes suggested in
public comments.
The existing exclusion for prior
converted cropland moves to paragraph
(b)(2) of the rule and is unchanged. A
number of commenters suggested
changes to the existing exclusion for
prior converted cropland. As with waste
treatment systems, the preamble to the
proposed rule stated this rulemaking
was not making changes to the
exclusion for prior converted cropland.
As a result, comments requesting
changes to the prior converted cropland
exclusion or seeking clarification of how
the exclusion is implemented in the
field are outside the scope of this
rulemaking, and the rule does not reflect
changes or respond to issues raised in
public comments. The agencies will
continue to implement this exclusion
consistent with current policy and
practice.
The agencies identify excluded
ditches in paragraph (b)(3).
Jurisdictional ditches are discussed at
more detail in section IV.F. The rule
excludes all ditches with ephemeral
flow that are not excavated in or
relocate a tributary. The rule also
excludes ditches with intermittent flow
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that are not a relocated tributary,
excavated in a tributary, or drain
wetlands, regardless of whether or not
the wetland is a jurisdictional water.
Finally, ditches that do not connect to
a traditional navigable water, interstate
water, or territorial sea either directly or
through another water are excluded,
regardless of whether the flow is
ephemeral, intermittent, or perennial.
These ditch exclusions are clearer for
the regulated public to identify and
more straightforward for agency staff to
implement than the proposed rule or
current policies. The ditch exclusions
do not affect the possible status of a
ditch as a point source.
Many comments addressed ditches,
and many of these comments are
reflected in the approach to ditches
articulated in the rule. The majority of
commenters requested that the agencies’
ditch exclusion be clarified or
broadened. Many commenters were
confused by the term ‘‘uplands’’ and did
not feel the term had a common
understanding. For example, some
commenters felt the term referred only
to areas at higher elevations in the
landscape. Many expressed concerns
that all ditches would be jurisdictional
under the proposed rule. Many groups
especially called for exclusions of
roadside ditches.
The revised exclusions reflect the
agencies’ careful consideration of these
comments. First, the agencies have
eliminated the term ‘‘uplands’’ in
response to the questions the term
created. Second, the agencies have
instead provided a clearer statement of
the types of ditches that are subject to
exclusion—ditches that are not
excavated in or relocate a tributary and
ditches that do not drain a wetland.
Eliminating the term ‘‘uplands’’ with
this more straightforward description
should improve clarity. Finally, the
agencies have more clearly stated the
flow regimes in ditches that are subject
to the exclusions; these flow regimes are
described earlier and have been used by
the agencies consistently and are readily
understood by field staff and the public.
As noted, the agencies received many
comments asking that roadside ditches
be addressed, and more specifically
excluded, in the final rule. Like the
proposed rule, the final rule does not
include an explicit exclusion for
roadside ditches, but the agencies
believe the exclusions included in the
final rule will address the vast majority
of roadside and other transportation
ditches. Moreover, since the agencies
have focused in the final rule on the
physical characteristics of excluded
ditches, the exclusions will address all
ditches that the agencies have
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concluded should not be subject to
jurisdiction, including certain ditches
on agricultural lands and ditches
associated with modes of transportation,
such as roadways, airports, and rail
lines.
As discussed in Section IV.F.1., the
definition of tributary includes natural,
undisturbed waters and those that have
been man-altered or constructed, but
which science shows function as a
tributary. In addition, natural streams
and rivers that are altered or modified
for purposes as flood control, erosion
control, and other reasons does not
convert the tributary to a ditch. A
stream or river that has been
channelized or straightened because its
natural sinuosity has been altered,
cutting off the meanders, is not a ditch.
A stream that has banks stabilized
through use of concrete or rip-rap (e.g.,
rocks or stones) is not a ditch. The Los
Angeles River, for example, is a ‘‘water
of the United States’’ (and, indeed, a
traditional navigable water) and remains
a ‘‘water of the United States’’ and is not
a excluded under paragraph (b)(3), even
where it has been ditched, channelized,
or concreted.
The rule excludes ditches with
ephemeral flow except where a ditch is
excavated in or relocates a covered
tributary. Under the rule, that portion of
a ditch with ephemeral flow actually
excavated in or relocating the covered
tributary would be considered
jurisdictional. The jurisdictional status
of upstream and downstream portions of
the same ditch would have to be
assessed based on the specific facts and
under the terms of the rule to determine
flow characteristics and whether or not
the ditch is excavated in or relocates a
tributary. This approach reasonably
balances the exclusion with the need to
ensure that covered tributaries, and the
significant functions they provide, are
preserved. A ditch that relocates a
stream is not an excluded ditch under
paragraph (b)(3), and a stream is
relocated either when at least a portion
of its original channel has been
physically moved, or when the majority
of its flow has been redirected. A ditch
that is a relocated stream is
distinguishable from a ditch that
withdraws water from a stream without
changing the stream’s aquatic character.
The latter type of ditch is excluded from
jurisdiction where it meets the listed
characteristics of excluded ditches
under paragraph (b)(3). The agencies
will determine historical presence of
tributaries using a variety of resources,
such as USGS and state and local maps,
historic aerial photographs, local surface
water management plans, street
maintenance data, wetlands and
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conservation programs and plans, as
well as functional assessments and
monitoring efforts.
The rule also excludes ditches with
intermittent flow except where a ditch
is excavated in or relocates a covered
tributary, or drains wetlands. Where an
excluded ditch drains a wetland, the
segment of the ditch that physically
intersects the wetland would be
considered jurisdictional. The
jurisdictional status of upstream and
downstream portions of the same ditch
would have to be assessed based on the
specific facts and under the terms of the
rule to determine flow characteristics
and whether or not the ditch drains a
wetland. The provision of paragraph
(b)(3) addressing draining of wetlands is
specific to ditches with intermittent
flow. As discussed previously, features
that are ephemeral will flow only in
response to precipitation events, such as
rainfall or snowmelt. Ditches with
ephemeral flow, therefore, do not
typically have the flow characteristics
characteristic of ditches that drain
wetlands. The agencies have
accordingly focused on intermittent
ditches that drain wetlands.
In addition, the agencies clarify that a
ditch drains a wetland when it
physically intersects the wetland. If the
ditch has been cut to carry only
ephemeral flows, such as those
following a storm event, the effect of the
ditch is minimal as it carries only that
flow that overtops the wetland during
and immediately following the rain
event. However, if the ditch has been
cut to carry intermittent or perennial
flows from the wetland, the ditch is
serving as a conduit for transferring flow
from the wetland to a downstream
tributary. As a result of the cut ditch,
the wetland’s hydrologic regime is
modified and can generally affect the
natural functions performed by the
wetland. When the ditch has been cut
to carry intermittent or perennial flow
from the wetland to the downstream
tributary, the wetland soils and
vegetation can shift into a community
that supports less hydric soils and a mix
of riparian or upland vegetation.
Consequently, the ditch is draining the
wetland and the wetland quality
degrades and may cease to exist over
time. Therefore, a ditch that carries
intermittent flow and physically
intersects with a wetland is not
excluded under this provision.
A number of commenters expressed
concern that a ditch could be viewed as
both a point source and a ‘‘water of the
United States.’’ However, the approach
that ditches can be considered both
reflects the CWA itself as well as
longstanding agency policy.
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Paragraph (b)(4) of the rule identifies
features and waters that the agencies
have identified as generally not ‘‘waters
of the United States’’ in previous
preambles or guidance documents.
Codifying these longstanding practices
supports the agencies’ goals of
providing greater clarity, certainty, and
predictability for the regulated public
and the regulators. The agencies’ 1986
and 1988 preambles indicated that these
waters could be determined on a casespecific basis to be ‘‘waters of the
United States.’’ This rule does not allow
for this case-specific analysis to be used
to establish jurisdiction—these waters
are categorically excluded from
jurisdiction. Some of the exclusions
have been modified slightly to address
public comments and improve clarity.
The following features are not ‘‘waters
of the United States’’:
• Artificially irrigated areas that
would revert to dry land should
application of irrigation water to that
area cease
• Artificial, constructed lakes or
ponds created by excavating and/or
diking dry land such as farm and stock
watering ponds, irrigation ponds,
settling basins, log cleaning ponds,
cooling ponds, or fields flooded for rice
growing
• Artificial reflecting pools or
swimming pools created by excavating
and/or diking dry land
• Small ornamental waters created by
excavating and/or diking dry land for
primarily aesthetic reasons
• Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand or
gravel that fill with water
• Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways
• Puddles
Several of these exclusions use the
phrase ‘‘dry land.’’ This phrase appears
in the 1986 and 1988 preambles, and the
agencies believe the term is well
understood based on the more than 30
years of practice and implementation.
But in keeping with the goal of
providing greater clarity, the agencies
state that ‘‘dry land’’ refers to areas of
the geographic landscape that are not
water features such as streams, rivers,
wetlands, lakes, ponds and the like.
However, it is important to note that a
‘‘water of the United States’’ is not
considered ‘‘dry land’’ just because it
lacks water at a given time. Similarly, an
area remains ‘‘dry land’’ even if it is wet
after a rainfall event. The agencies
received comments suggesting that the
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final rule provide a definition of ‘‘dry
land’’ as it relates to the exclusion for
stormwater control features. The
agencies considered the request and
determined that there was no agreed
upon definition given geographic and
regional variability. The agencies
concluded that further clarity on this
issue can be provided during
implementation.
In the exclusion for artificial lakes or
ponds, the agencies have removed
language regarding ‘‘use’’ of the ponds,
including the term ‘‘exclusively.’’ In
most cases, the ‘‘use’’ of the pond is
captured in its name. More importantly,
the agencies recognize that artificial
lakes and ponds are often used for more
than one purpose and can have other
beneficial purposes, such as animal
habitat, water retention or recreation.
For example, rice growing is typically
facilitated by land leveling and
inundation that floods vast areas. The
fields are flooded for the purpose of
weed control and to facilitate rice
cultivation, but these rice fields are
often extensively used by waterfowl and
other wildlife. The agencies agree with
commenters who raised concern that
rice fields ‘‘used’’ both for rice growing
and waterfowl habitat should continue
to be excluded even where they are not
used ‘‘exclusively’’ for a single purpose.
The change to the exclusion reflects the
agencies’ practice and ensures that
waters the agencies have historically not
treated as jurisdictional do not become
so because of another incidental
beneficial use.
The agencies have also added farm
ponds, log cleaning ponds, and cooling
ponds to the list of excluded ponds in
the rule based on public comments. The
list of ponds has always been
illustrative rather than exhaustive, and
the additions respond to requests to
clarify that farm ponds, and log cleaning
ponds 12 created in dry land are
excluded. The agencies have also added
cooling ponds created in dry land to the
list of excluded waters. The agencies
also note that cooling ponds that are
created under section 404 in
jurisdictional waters and that have
NPDES permits are subject to the waste
treatment system exclusion, which is
not changing. Cooling ponds created to
serve as part of a cooling water system
with a valid state permit constructed in
waters of the United States prior to
enactment of the Clean Water Act and
currently excluded from jurisdiction
remain excluded under the new rule.
Additional ponds will also likely fall
under the exclusion based on site
12 Log cleaning ponds are used to float logs for
removal of twigs, branches, and large knots.
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specific evaluation, including, for
example, fire control ponds and fishing
ponds excavated from dry land.
Artificial lakes and ponds created in dry
land that do not connect to
jurisdictional waters are covered by this
exclusion. Where these ponds do
connect and discharge to jurisdictional
waters, the agencies will evaluate
factors such as the potential for
introduction of pollutants and coverage
under an issued NPDES permit. As a
general matter, ponds created in dry
land that discharge to ‘‘waters of the
United States’’ are covered by the
exclusion where such discharge is
regulated under a NPDES permit.
Conveyances created in dry land that
are physically connected to and are a
part of the excluded feature are also
excluded. These artificial features are
working together as a system, and it is
appropriate to treat them as one
functional unit. The agencies emphasize
that ponds excluded from ‘‘waters of the
United States’’ can, in some
circumstances, be point sources of
pollution subject to section 301 of the
Act.
The rule includes several refinements
to the exclusion for water-filled
depressions created as a result of certain
activities. In addition to construction
activity, the agencies have also excluded
water-filled depressions created in dry
land incidental to mining activity. This
change is consistent with the agencies’
1986 and 1988 preambles, which
generally excluded pits excavated for
obtaining fill, sand or gravel, and there
is no need to distinguish between
features based on whether they are
created by construction or mining
activity.
The agencies also here clarify their
longstanding view that only the specific
land being directly irrigated that would
revert to dry land should irrigation
cease is exempt; it is not the case that
all waters within watersheds where
irrigation occurs are exempt.
The rule identifies all erosional
features, including gullies and rills, as
non-jurisdictional features. While the
proposed rule specifically identified
gullies and rills, the agencies intended
that all erosional features would be
excluded. The final rule makes this
clear. Erosional features are not
jurisdictional under the terms of
paragraph (a) and the definitions in
paragraph (c), especially the definition
of tributary. These features are
specifically excluded in the rule to
avoid confusion, because preceding
guidance identified them as nonjurisdictional and many commenters
stated these exclusions were important
to maintain in the rule.
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Tributaries can be distinguished from
erosional features by the presence of bed
and banks and an ordinary high water
mark. Concentrated surface runoff can
occur within erosional features without
creating the permanent physical
characteristics associated with bed and
banks and ordinary high water mark.
See Technical Support Document. It
should be noted that some ephemeral
streams are colloquially called ‘‘gullies’’
or the like even when they exhibit a bed
and banks and an ordinary high water
mark; regardless of the name they are
given locally, waters that meet the
definition of tributary are not excluded
erosional features.
The rule also excludes lawfully
constructed grassed waterways. Grassed
waterways are lawfully constructed for
purposes of this rule either where they
are on dry land and replace nonjurisdictional erosional features or, more
commonly, where they have been
lawfully converted from an intermittent
or ephemeral stream under a CWA
permit. Once converted to grassed
waterways, these former streams
segments no longer exhibit a bed and
banks or ordinary high water mark and
are excluded because they do not meet
the definition of ‘‘tributary.’’ However,
such conversion does not sever
jurisdiction over the entire length of the
tributary above and below the grassed
waterway. Instead, the grassed
waterway is considered a constructed
break in the bed and banks and ordinary
high water mark. This is reflected in the
definition of tributary, which
specifically addresses natural or manmade breaks in bed and banks and
ordinary high water mark.
The final rule adds an exclusion for
puddles. The proposed rule did not
explicitly exclude puddles because the
agencies have never considered puddles
to meet the minimum standard for being
a ‘‘water of the United States,’’ and it is
an inexact term. A puddle is commonly
considered a very small, shallow, and
highly transitory pool of water that
forms on pavement or uplands during or
immediately after a rainstorm or similar
precipitation event. However, numerous
commenters asked that the agencies
expressly exclude them in a rule. The
final rule does so.
The agencies include an exclusion for
groundwater, including groundwater
drained through subsurface drainage
systems. As discussed in the preamble
to the proposed rule, the agencies have
never interpreted ‘‘waters of the United
States’’ to include groundwater. The
exclusion does not apply to surface
expressions of groundwater, as some
commenters requested, such as where
groundwater emerges on the surface and
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becomes baseflow in streams or spring
fed ponds.
The final rule includes a new
exclusion in paragraph (b)(6) for
stormwater control features constructed
to convey, treat, or store stormwater that
are created in dry land. The agencies
stated in the proposed rule that the
exclusions were guided by decisions of
the Supreme Court and were intended
to further the agencies’ goal of providing
clarity and certainty. The agencies in
the proposed rule sought to provide a
‘‘full description’’ of the waters that will
not be ‘‘waters of the United States.’’ 79
FR at 22218. In response to the agencies’
proposal, several commenters indicated
additional clarity was needed,
particularly with respect to stormwater
control features and wastewater
recycling facilities. This exclusion
responds to numerous commenters who
raised concerns that the proposed rule
would adversely affect municipalities’
ability to operate and maintain their
stormwater systems, and also to address
confusion about the state of practice
regarding jurisdiction of these features
at the time the rule was proposed.
The agencies’ longstanding practice is
to view stormwater control measures
that are not built in ‘‘waters of the
United States’’ as non-jurisdictional.
Conversely, the agencies view some
waters, such as channelized or piped
streams, as jurisdictional currently even
where used as part of a stormwater
management system. Nothing in the
proposed rule was intended to change
that practice. Nonetheless, the agencies
recognize that the proposed rule brought
to light confusion about which
stormwater control features are
jurisdictional waters and which are not,
and agree that it is appropriate to
address this confusion by creating a
specific exclusion in the final rule for
stormwater controls features that are
created in dry land.
Many commenters, particularly
municipalities and other public entities
that operate storm sewer systems and
stormwater management programs,
expressed concern that various
stormwater control measures—such as
stormwater treatment systems, rain
gardens, low impact development/green
infrastructure, and flood control
systems—could be considered ‘‘waters
of the United States’’ under the
proposed rule, either as part of a
tributary system, an adjacent water, or
as a result of a case-specific significant
nexus analysis. This exclusion should
clarify the appropriate limits of
jurisdiction relating to these systems. A
key element of the exclusion is whether
the feature or control system was built
in dry land and whether it conveys,
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treats, or stores stormwater. Certain
features, such as curbs and gutters, may
be features of stormwater collection
systems, but have never been
considered ‘‘waters of the United
States.’’
Stormwater control features have
evolved considerably over the past
several years, and their nomenclature is
not consistent, so in order to avoid
unintentionally limiting the exclusion,
the agencies have not included a list of
excluded features in the rule. The rule
is intended to exclude the diverse range
of control features that are currently in
place and may be developed in the
future.
Traditionally, stormwater controls
were designed to direct runoff away
from people and property as quickly as
possible. Cities built systems to collect,
convey, or store stormwater, using
structures such as curbs, gutters, and
sewers. Often, cities used existing
stream networks as part of the
stormwater drainage network. Retention
and detention stormwater ponds were
built to store excess stormwater until it
could be more safely released.
Recently, treatment of stormwater has
become more prevalent to remove
harmful pollutants before the
stormwater is discharged. Even more
recently, cities have turned to green
infrastructure, using existing natural
features or creating new features that
mimic natural hydrological processes
that work to infiltrate or evapotranspirate precipitation, to manage
stormwater at its source and keep it out
of the conveyance system. These
engineered components of stormwater
management systems can address both
water quantity and quality concerns, as
well as provide other benefits to
communities. This rule is designed to
avoid disincentives to this
environmentally beneficial trend in
stormwater management practices. This
exclusion does not cover transportation
ditches; those ditches are addressed
under paragraph (b)(3) of the rule. As
discussed above, the exclusion in
paragraph (b)(6) is intended to address
engineered stormwater control
structures in municipal or urban
environments. Stormwater control
features are designed to address runoff
that occurs during and shortly after
precipitation events; as a result,
stormwater features that convey runoff
are expected to only carry ephemeral or
intermittent flow. For ease of
implementation, the agencies want
water features to be dealt with under
only one provision of the rule. However,
the agencies do not expect the scope of
ditches excluded to be different under
paragraphs (b)(3) and (b)(6), so there
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should be little practical need to
distinguish between the two.
Paragraph (b)(7) of the rule clarifies
that wastewater recycling structures
constructed in dry land are excluded.
This new exclusion clarifies the
agencies’ current practice that such
waters and water features used for water
reuse and recycling are not
jurisdictional when constructed in dry
land. The agencies recognize the
importance of water reuse and
recycling, particularly in areas like
California and the Southwest where
water supplies can be limited and
droughts can exacerbate supply issues.
This exclusion responds to numerous
commenters and encourages water reuse
and conservation while still
appropriately protecting the chemical,
physical, and biological integrity of the
nation’s water under CWA.
The agencies specifically exclude
constructed detention and retention
basins created in dry land used for
wastewater recycling as well as
groundwater recharge basins and
percolation ponds built for wastewater
recycling. Many commenters noted the
growing interest in and commitment to
water recycling and reuse projects.
Detention and retention basins can play
an important role in capturing and
storing water prior to beneficial reuse.
Similarly, groundwater recharge basins
and percolation ponds are becoming
more prevalent tools for water reuse and
recycling. These features are used to
collect and store water, which then
infiltrates into groundwater via
permeable soils. Though these features
are often created in dry land, they are
also often located in close proximity to
tributaries or other larger bodies of
water. The exclusion also covers water
distributary structures that are built in
dry land for water recycling. These
features often connect or carry flow to
other water recycling structures, for
example a channel or canal that carries
water to a percolation pond. The
agencies have not considered these
water distributary systems jurisdictional
where they do not have surface
connections back into, and contribute
flow to, ‘‘waters of the United States.’’
In contrast, the agencies have
consistently regulated aqueducts and
canals as ‘‘waters of the United States’’
where they serve as tributaries,
removing water from one part of the
tributary network and moving it to
another. The exclusion in paragraph
(b)(7) codifies long-standing agency
practice and encourages water
management practices that the agencies
agree are important and beneficial.
The agencies also received other
suggestions for new exclusions that
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were not adopted in the final rule. The
agencies determined that it was not
appropriate or necessary to add certain
requested exclusions for one or more
reasons, including: (1) The requested
exclusion was so broadly characterized
as to introduce significant confusion
and potentially have the effect of
excluding waters that the agencies have
consistently determined should be
covered as ‘‘waters of the U.S.,’’ (2) the
requested exclusion was so site-specific
or activity-based as to lack illustrative
value, or (3) the requested exclusion
was likely covered by another exclusion
in the final rule.
It is important to note that while the
waters listed in the exclusions are not
‘‘waters of the United States,’’ they can
serve as a hydrologic connection that
the agencies would consider under a
case-specific significant nexus under
paragraphs (a)(7) and (a)(8). For
example, a wetland may be directly
hydrologically connected to a covered
tributary via flow through an excluded
non-wetland swale. While the swale
itself is excluded from jurisdiction, the
connection of the wetland to the
tributary is relevant for determining
whether the wetland has a significant
nexus to downstream traditional
navigable waters, interstate waters, or
the territorial seas. In addition, these
geographic features may function as
‘‘point sources’’ under CWA section
502(14), such that discharges of
pollutants to waters through these
features would be subject to other CWA
regulations (e.g., CWA section 402).
V. Economic Impacts
This rule establishing the definition of
‘‘waters of the United States,’’ by itself,
imposes no direct costs. The potential
costs and benefits incurred as a result of
this rule are considered indirect,
because the rule involves a definitional
change to a term that is used in the
implementation of CWA programs (i.e.,
sections 303, 305, 311, 401, 402, and
404). Entities currently are, and will
continue to be, regulated under these
programs that protect ‘‘waters of the
United States’’ from pollution and
destruction. Each of these programs may
subsequently impose direct or indirect
costs as a result of implementation of
their specific regulations.
While the rule imposes no direct
costs, the agencies prepared an
economic analysis for informational
purposes. In preparing the economic
analysis to accompany the final rule, the
agencies considered what should be the
appropriate baseline for comparison.
Existing regulations and historic
practice in implementing them
represent one appropriate baseline for
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comparison, and because the final rule
is narrower in jurisdictional scope than
the existing regulations, there would be
no additional costs in comparison to
this baseline. A comparison to recent
field practice following the 2008
guidance is also an appropriate baseline,
and the agencies prepared illustrative
estimates of how the costs and benefits
of various CWA programs may change
with an increase in positive
jurisdictional determinations relative to
that baseline.
To estimate changes in potential costs
and benefits of different CWA programs,
the economic analysis utilizes available
program data to estimate the extent to
which assertion of jurisdiction might
change under the associated final
policies. The proposed rule analysis
utilized CWA Section 404 jurisdictional
determination and permit data from
fiscal years 2009–2010 (post SWANCC
and Rapanos), following issuance of
program guidance in 2008 by the EPA
and the Corps. The analysis for the final
rule has been updated using data from
fiscal years 2013–2014, providing a
comparison to a more recent year of
data, which responds to public
comments. An estimate of how assertion
of jurisdiction may change compared to
the recent practice baseline, developed
using updated data from fiscal years
2013–2014 jurisdictional
determinations, is then applied to cost
and benefit information for affected
CWA programs. Additional updates to
the economic analysis include a refined
approach to calculating benefits from
section 404 compensatory mitigation,
differentiating between emergent and
forested wetlands, as well as presenting
results in ranges to reflect uncertainty.
The agencies’ economic analysis yielded
the following key conclusions:
• Compared to the current regulations
and historic practice of making
jurisdictional determinations, the scope
of jurisdictional waters will decrease, as
would the costs and benefits of CWA
programs.
• Compared to a baseline of recent
practice, the agencies assessed two
scenarios. Those scenarios result in an
estimated increase of between 2.84 and
4.65 percent in positive jurisdictional
determinations annually.
• The agencies’ analysis indicates
that for both scenarios, the change in
benefits of CWA programs exceed the
costs by a ratio of greater than 1:1.
• The economic analysis estimates
that incremental annual costs for
scenario 1 will range from $158M–
$307M and incremental annual benefits
will range from $339M–$350M and, for
scenario 2, costs will range from
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$237M–$465M and benefits will range
from $555M–$572M.
The agencies conducted this economic
analysis to provide the public with
information on the potential changes to
the costs and benefits of various CWA
programs that may result from a change
in the number of positive jurisdictional
determinations. The economic analysis
was done for informational purposes
only, and the final decisions on the
scope of ‘‘waters of the United States’’
in this rulemaking are not based on
consideration of the information in the
economic analysis. The economic
analysis fulfills the requirements of
Executive Orders 13563 and 12866. An
explanation of the data, methods, and
assumptions used to estimate indirect
costs and benefits can be found in the
Economic Analysis for the Clean Water
Rule; Definition of ‘‘Waters of the
United States’’ Under the Clean Water
Act (Final Rule) in the accompanying
docket.
VI. Related Acts of Congress, Executive
Orders, and Agency Initiatives
A. Executive Order 12866: Regulatory
Planning and Review and Executive
Order 13563: Improving Regulation and
Regulatory Review
Under Executive Order 12866 (58 FR
51735, October 4, 1993), this action is a
‘‘significant regulatory action.’’
Accordingly, EPA and the Army
submitted this action to the Office of
Management and Budget (OMB) for
review under Executive Orders 12866
and 13563 (76 FR 3821, January 21,
2011) and any changes made in
response to OMB recommendations
have been documented in the docket for
this action.
In addition, EPA and the Army
prepared an analysis of the potential
costs and benefits associated with this
action. This analysis is contained in
Economic Analysis of the EPA-Army
Clean Water Rule. A copy of the
analysis is available in the docket for
this action.
B. Paperwork Reduction Act
This action does not impose any
information collection burden under the
provisions of the Paperwork Reduction
Act, 44 U.S.C. 3501 et seq. Burden is
defined at 5 CFR 1320.3(b). An agency
may not conduct or sponsor, and a
person is not required to respond to, a
collection of information unless it
displays a currently valid OMB control
number. The OMB control numbers for
the CWA section 402 program may be
found at 40 CFR 9.1. (OMB Control No.
2040–0004, EPA ICR No. 0229.19). For
the CWA section 404 regulatory
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program, the current OMB approval
number for information requirements is
maintained by the Corps of Engineers
(OMB approval number 0710–0003).
However, there are no new approval or
application processes required as a
result of this rulemaking that necessitate
a new Information Collection Request
(ICR).
C. Regulatory Flexibility Act
The Regulatory Flexibility Act (RFA)
generally requires an agency to prepare
a regulatory flexibility analysis of any
rule subject to notice-and-comment
rulemaking requirements under the
Administrative Procedure Act or any
other statute unless the agency certifies
that the rule will not have a significant
economic impact on a substantial
number of small entities. Small entities
include small businesses, small
organizations, and small governmental
jurisdictions.
For purposes of assessing the impacts
of this final action on small entities,
‘‘small entity’’ is defined as: (1) A small
business that is a small industrial entity
as defined in the U.S. Small Business
Administration’s size standards (see 13
CFR 121.201); (2) a small governmental
jurisdiction that is a government of a
city, county, town, school district, or
special district with a population of less
than 50,000; or (3) a small organization
that is any not-for-profit enterprise that
is independently owned and operated
and is not dominant in its field.
After considering the economic
impacts of this rule on small entities, we
certify that this final rule will not have
a significant economic impact on a
substantial number of small entities.
See, e.g., Cement Kiln Recycling
Coalition v. EPA, 255 F.3d 855 (D.C. Cir.
2001); Michigan v. EPA, 213 F.3d 663
(D.C. Cir. 2000); Am. Trucking Ass’n v.
EPA, 175 F.3d 1027 (D.C. Cir. 1999);
Mid-Tex Elec. Co-op, Inc. v. FERC, 773
F.2d 327 (D.C. Cir. 1985).
Under the RFA, the impact of concern
is any significant adverse economic
impact on small entities, because the
primary purpose of the initial regulatory
flexibility analysis is to identify and
address regulatory alternatives ‘‘which
minimize any significant economic
impact of the proposed rule on small
entities.’’ 5 U.S.C. 603. The scope of
jurisdiction in this rule is narrower than
that under the existing regulations. See
40 CFR 122.2 (defining ‘‘waters of the
United States’’). Because fewer waters
will be subject to the CWA under the
rule than are subject to regulation under
the existing regulations, this action will
not affect small entities to a greater
degree than the existing regulations. As
a consequence, this action will not have
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a significant adverse economic impact
on a substantial number of small
entities, and therefore no regulatory
flexibility analysis is required.
This rule is not designed to ‘‘subject’’
any entities of any size to any specific
regulatory burden. Rather, it is designed
to clarify the statutory scope of ‘‘the
waters of the United States, including
the territorial seas,’’ section 502(7),
consistent with Supreme Court
precedent. This question of CWA
jurisdiction is informed by the tools of
statutory construction and the
geographical and hydrological factors
identified in Rapanos v. United States,
547 U.S. 715 (2006), which are not
factors readily informed by the RFA.
Nevertheless, the scope of the term
‘‘waters of the United States’’ is a
question that has continued to generate
substantial interest, particularly within
the small business community, because
permits must be obtained for many
discharges of pollutants into those
waters. In light of this interest, the EPA
and the Army determined to seek wide
input from representatives of small
entities while formulating the proposed
and final definition of this term that
reflects the intent of Congress consistent
with the mandate of the Supreme
Court’s decisions. Such outreach,
although voluntary, is also consistent
with the President’s January 18, 2011
Memorandum on Regulatory Flexibility,
Small Business, and Job Creation, which
emphasizes the important role small
businesses play in the American
economy. This process has enabled the
agencies to hear directly from these
representatives, throughout the rule
development, about how they should
approach this complex question of
statutory interpretation, together with
related issues that such representatives
of small entities may identify for
possible consideration in separate
proceedings. The agencies have
prepared a report summarizing their
small entity outreach, the results of this
outreach, and how these results have
informed the development of this rule.
This report, Report of the Discretionary
Small Entity Outreach for the Revised
Definition of Waters of the United States
(Docket Id. No. EPA–HQ–OW–2011–
0880–1927), is available in the docket.
D. Unfunded Mandates Reform Act
This action does not contain any
unfunded mandate under the regulatory
provisions of Title II of the Unfunded
Mandates Reform Act of 1995 (UMRA)
(2 U.S.C. 1531–1538), and does not
significantly or uniquely affect small
governments. The action imposes no
enforceable duty on any state, local, or
tribal governments, or the private sector,
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and does not contain regulatory
requirements that might significantly or
uniquely affect small governments. The
definition of ‘‘waters of the United
States’’ applies broadly to CWA
programs.
E. Executive Order 13132: Federalism
This rule does not have federalism
implications. It will not have substantial
direct effects on the states, on the
relationship between the national
government and the states, or on the
distribution of power and
responsibilities among the various
levels of government.
Keeping with the spirit of Executive
Order 13132 and consistent with the
agencies’ policy to promote
communications with state and local
governments, the agencies consulted
with state and local officials throughout
the process and solicited their
comments on the proposed action and
on the development of the rule.
For this rule state and local
governments were consulted at the
onset of rule development in 2011, and
following the publication of the
proposed rule in 2014. In addition to
engaging key organizations under
federalism, the agencies sought feedback
on this rule from a broad audience of
stakeholders through extensive outreach
to numerous state and local government
organizations.
Early in the rulemaking process, EPA
held two in-person meetings and two
phone calls in the fall and winter of
2011. Organizations involved include
the National Governors Association, the
National Conference of State
Legislatures, the Council of State
Governments, the National Association
of Counties, the National League of
Cities, the U.S. Conference of Mayors,
the County Executives of America, the
National Associations of Towns and
Townships, the International City/
County Management Association, and
the Environmental Council of the States.
Additionally, the National Association
of Clean Water Agencies and the
Association of Clean Water
Administrators were invited to
participate. The agencies held many
additional calls and meetings with state
and local governments and their
associations, in preparation for the
development of a proposed rule.
Similarly to the outreach conducted
prior to the development of the rule, the
agencies committed themselves to
providing a transparent, comprehensive,
and effective process for taking public
comment on the proposed rule. As part
of this consultation, EPA held a meeting
on May 13, 2014 to seek technical input
on the proposed rule from the largest
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national representative organizations for
State and local governments. During this
process the agencies also extended its
focused outreach to include a series of
meetings with the Local Government
Advisory Committee, and the
Environmental Council of the States in
conjunction with the Association of
Clean Water Administrators and the
Association of State Wetland Managers.
In addition to engaging these key
organizations, the agencies sought
additional feedback on the proposed
rule through broader public outreach to
state and local government
organizations during the public
comment period.
During the consultation process, some
participants expressed concern that the
proposed changes may impose a
resource burden on state and local
governments. Some participants urged
EPA to ensure that states are not unduly
burdened by the regulatory revisions.
The agencies have prepared a report
summarizing their voluntary
consultation and extensive outreach to
State, local, and county governments,
the results of this outreach, and how
these results have informed the
development of today’s rule. This
report, Report on the Discretionary
Consultation and Outreach to State,
Local, and County Governments on the
Clean Water Rule: Definition of ‘‘Waters
of the United States;’’ Final Rule
(Docket Id. No. EPA–HQ–OW–2011–
0880) is available in the docket for this
rule.
F. Executive Order 13175: Consultation
and Coordination With Indian Tribal
Governments
Subject to the Executive Order (E.O.)
13175 (65 FR 67249, November 9, 2000),
agencies generally may not issue a
regulation that has tribal implications,
(1) that imposes substantial direct
compliance costs, and that is not
required by statute, unless the Federal
government provides the funds
necessary to pay the direct compliance
costs incurred by tribal governments, or
the agencies consult with tribal officials
early in the process of developing the
proposed regulation and develop a tribal
summary impact statement, or (2) that
preempts tribal law unless the agencies
consult with tribal officials early in the
process of developing the proposed
regulation and develops a tribal
summary impact statement.
This action does not have tribal
implications as specified in E.O. 13175.
In compliance with the EPA Policy on
Consultation and Coordination with
Indian Tribes (May 4, 2011), the
agencies consulted with tribal officials
throughout the rulemaking process to
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gain an understanding of tribal views
and solicited their comments on the
proposed action and on the
development of this rule. In the course
of this consultation, EPA and the Corps
jointly participated in aspects of the
process.
The agencies began consultation with
federally-recognized Indian tribes on the
Clean Water Rule defining ‘‘waters of
the United States’’ in October 2011. The
consultation and coordination process,
including providing information on the
development of an accompanying
science report on the connectivity of
streams and wetlands, continued, in
stages, over a four year period, until the
close of the public comment period on
November 14, 2014. EPA invited tribes
to provide written input on the
rulemaking throughout both the tribal
consultation process and public
comment period.
EPA specifically consulted with tribal
officials to gain an understanding of,
and to address, the tribal views on the
proposed rule. In 2011, close to 200
tribal representatives and more than 40
tribes participated in the consultation
process, which included multiple
webinars and national teleconferences
and face-to-face meetings. In addition,
EPA received written comments from
three tribes during the initial
consultation period.
EPA continued to provide status
updates to the National Tribal Water
Council and the National Tribal Caucus
during 2012 through 2014. The final
consultation event was completed on
October 23, 2014 as a national
teleconference with the Office of
Water’s Deputy Assistant Administrator.
Ultimately, EPA received an additional
23 letters from tribes/tribal
organizations by the completion of the
consultation period. The comments
indicated that Tribes, overall, support
increased clarity of waters protected by
the Clean Water Act, but some
expressed concern with the consultation
process and the burden of any expanded
jurisdiction. The agencies considered
the feedback received through
consultation and written comments in
developing today’s rule.
The agencies have prepared a report
summarizing their consultation with
tribal nations, and how these results
have informed the development of this
rule. This report, Final Summary of
Tribal Consultation for the Clean Water
Rule: Definition of ‘‘Waters of the
United States’’ Under the Clean Water
Act; Final Rule (Docket Id. No. EPA–
HQ–OW–2011–0880), is available in the
docket for this rule.
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37103
G. Executive Order 13045: Protection of
Children From Environmental Health
Risks and Safety Risks
This action is not subject to Executive
Order 13045 (62 FR 19885, April 23,
1997) because the environmental health
or safety risks addressed by this action
do not present a disproportionate risk to
children.
H. Executive Order 13211: Actions
Concerning Regulations That
Significantly Affect Energy Supply,
Distribution, or Use
This action is not a ‘‘significant
energy action’’ as defined in Executive
Order 13211 (66 FR 28355, May 22,
2001) because it is not likely to have a
significant adverse effect on the supply,
distribution, or use of energy.
I. National Technology Transfer and
Advancement Act
Section 12(d) of the National
Technology Transfer and Advancement
Act of 1995 (‘‘NTTAA’’), Public Law
104–113, 12(d) (15 U.S.C. 272 note)
directs federal agencies to use voluntary
consensus standards in regulatory
activities unless to do so would be
inconsistent with applicable law or
otherwise impractical. Voluntary
consensus standards are technical
standards (e.g., materials specifications,
test methods, sampling procedures, and
business practices) that are developed or
adopted by voluntary consensus
standards bodies. NTTAA directs
federal agencies to provide Congress,
through OMB, explanations when the
agency decides not to use available and
applicable voluntary consensus
standards.
This rule does not involve technical
standards. Therefore, the agencies are
not considering the use of any voluntary
consensus standards.
J. Executive Order 12898: Federal
Actions To Address Environmental
Justice in Minority Populations and
Low-Income Populations
Executive Order (E.O.) 12898 (59 FR
7629, Feb. 16, 1994) establishes Federal
executive policy on environmental
justice. Its main provision directs
Federal agencies, to the greatest extent
practicable and permitted by law, to
make environmental justice part of their
mission by identifying and addressing,
as appropriate, disproportionately high
and adverse human health or
environmental effects of their programs,
policies, and activities on minority
populations and low-income
populations in the United States.
The agencies have determined that
the rule will not have
disproportionately high and adverse
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human health or environmental effects
on minority or low-income populations,
because it does not adversely affect the
level of protection provided to human
health or the environment.
The rule defines the scope of waters
protected under the CWA. The
increased clarity regarding the
definition of ‘‘waters of the United
States’’ is intended to benefit all
regulators, stakeholders, and interested
parties. In addition, this rule is national
in scope and, therefore, is not specific
to a particular geographic area.
In the spirit of E.O. 12898, input from
environmental justice stakeholders was
requested during the rule development
process, through a series of stakeholder
meetings between April and November
2014. On May 12, 2014, EPA held a
focused teleconference with nontraditional stakeholders, including
environmental justice and faith-based
stakeholders, to solicit their individual
input on the proposed rule. The
agencies have used the feedback from
public outreach as the source of early
guidance and recommendations for
refining the proposed rule. Stakeholder
input received during public outreach
events in combination with the written
comments received during the public
comment period have reshaped each of
the definitions included in today’s rule,
and incorporate increased clarity for
regulators, stakeholders, and the
regulated public to assist them in
identifying waters as ‘‘waters of the
United States.’’
The agencies prepared a report
summarizing their outreach to the
environmental justice community,
analysis of potential impacts, and how
these results informed the development
of the rule. This report, Environmental
Justice Report for the Clean Water Rule:
Definition of ‘‘Waters of the United
States’’ Under the Clean Water Act;
Final Rule (Docket Id. No. EPA–HQ–
OW–2011–0880), is available in the
docket for this rule.
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K. Congressional Review Act
This action is subject to the
Congressional Review Act (CRA), and
the agencies will submit a rule report to
each House of the Congress and to the
Comptroller General of the United
States. This action is a ‘‘major rule’’ as
defined by 5 U.S.C. 804(2) based on
potential indirect costs.
L. Environmental Documentation
In this joint rulemaking, the agencies
establish a definitional rule that clarifies
the scope of the Clean Water Act. The
definition will apply to all provisions of
the Act, and this regulation specifically
amends EPA regulations implementing
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sections 301, 304, 306, 311, 402 and
404, while the Army is making
substantively identical revisions to its
regulations under section 404 of the
CWA. Section 511(c) of the Clean Water
Act provides that, except for certain
actions not relevant here, no action by
EPA constitutes ‘a major federal action
significantly affecting the quality of the
human environment within the meaning
of [NEPA]’’.
The Army has prepared a final
environmental assessment and Findings
of No Significant Impact consistent with
the National Environmental Policy Act
(NEPA). The Army has determined that
the rule is not a major federal action
significantly affecting the quality of the
human environment that would require
the preparation of an environmental
impact statement. The assessment is
contained in the record for this
rulemaking. Furthermore, appropriate
environmental documentation,
including an EIS when required, is
prepared by the Corps for general
permits and specifically for each and
every standard individual permit
application before making final permit
decisions.
M. Judicial Review
Section 509(b)(1) of the CWA
provides for judicial review in the
courts of appeals of specifically
enumerated actions of the
Administrator. The Supreme Court and
lower courts have reached different
conclusions on the types of actions that
fall within section 509. Compare, E.I. du
Pont de Nemours and Co. v. Train, 430
U.S. 112 (1977); NRDC v. EPA, 673 F.2d
400 (D.C. Cir. 1982); National Cotton
Council of Amer. v. EPA, 553 F.3d
927(6th Cir. 2009) cert denied 559 U.S.
936 (2010) with, Northwest
Environmental Advocates v. EPA, 537
F.3d 1006 (9th Cir. 2008); Friends of the
Everglades v. EPA, 699 F.3d 1280 (11th
Cir. 2012) cert denied 559 U.S. 936
(2010).
See DATES section for information
regarding the timing for seeking judicial
review of this rule.
List of Subjects
33 CFR Part 328
Environmental protection,
Administrative practice and procedure,
Intergovernmental relations, Navigation,
Water pollution control, Waterways.
40 CFR Parts 110, 112, 116, 117, 122,
230, 232, 300, 301, and 401
Environmental protection, Water
pollution control.
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Dated: May 27, 2015.
Gina McCarthy,
Administrator, Environmental Protection
Agency.
Dated: May 27, 2015.
Jo-Ellen Darcy,
Assistant Secretary of the Army, (Civil Works),
Department of the Army.
Title 33—Navigation and Navigable
Waters
For the reasons set out in the
preamble, title 33, chapter II of the Code
of Federal Regulations is amended as
follows:
PART 328—DEFINITION OF WATERS
OF THE UNITED STATES
1. The authority citation for part 328
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
2. Section 328.3 is amended by
revising paragraphs (a) through (c),
removing paragraphs (d) and (e), and
redesignating paragraph (f) as paragraph
(d) to read as follows:
■
§ 328.3
Definitions.
*
*
*
*
*
(a) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (b) of this
section, the term ‘‘waters of the United
States’’ means:
(1) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(2) All interstate waters, including
interstate wetlands;
(3) The territorial seas;
(4) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(5) All tributaries, as defined in
paragraph (c)(3) of this section, of
waters identified in paragraphs (a)(1)
through (3) of this section;
(6) All waters adjacent to a water
identified in paragraphs (a)(1) through
(5) of this section, including wetlands,
ponds, lakes, oxbows, impoundments,
and similar waters;
(7) All waters in paragraphs (a)(7)(i)
through (v) of this section where they
are determined, on a case-specific basis,
to have a significant nexus to a water
identified in paragraphs (a)(1) through
(3) of this section. The waters identified
in each of paragraphs (a)(7)(i) through
(v) of this section are similarly situated
and shall be combined, for purposes of
a significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (a)(1)
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through (3) of this section. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (a)(6) of this section when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(a)(6), they are an adjacent water and no
case-specific significant nexus analysis
is required.
(i) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(ii) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(iii) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(iv) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(v) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(8) All waters located within the 100year floodplain of a water identified in
paragraphs (a)(1) through (3) of this
section and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (a)(1) through
(5) of this section where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (a)(1) through
(3) of this section. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (a)(1) through (3) of this
section or within 4,000 feet of the high
tide line or ordinary high water mark.
Waters identified in this paragraph shall
not be combined with waters identified
in paragraph (a)(6) of this section when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(a)(6), they are an adjacent water and no
case-specific significant nexus analysis
is required.
(b) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(a)(4) through (8) of this section.
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(1) Waste treatment systems,
including treatment ponds or lagoons
designed to meet the requirements of
the Clean Water Act.
(2) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(3) The following ditches:
(i) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(ii) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(iii) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (a)(1)
through (3) of this section.
(4) The following features:
(i) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(ii) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(iii) Artificial reflecting pools or
swimming pools created in dry land;
(iv) Small ornamental waters created
in dry land;
(v) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(vi) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(vii) Puddles.
(5) Groundwater, including
groundwater drained through
subsurface drainage systems.
(6) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(7) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(c) Definitions. In this section, the
following definitions apply:
(1) Adjacent. The term adjacent
means bordering, contiguous, or
neighboring a water identified in
paragraphs (a)(1) through (5) of this
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section, including waters separated by
constructed dikes or barriers, natural
river berms, beach dunes, and the like.
For purposes of adjacency, an open
water such as a pond or lake includes
any wetlands within or abutting its
ordinary high water mark. Adjacency is
not limited to waters located laterally to
a water identified in paragraphs (a)(1)
through (5) of this section. Adjacent
waters also include all waters that
connect segments of a water identified
in paragraphs (a)(1) through (5) or are
located at the head of a water identified
in paragraphs (a)(1) through (5) of this
section and are bordering, contiguous,
or neighboring such water. Waters being
used for established normal farming,
ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(2) Neighboring. The term neighboring
means:
(i) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (a)(1)
through (5) of this section. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(ii) All waters located within the 100year floodplain of a water identified in
paragraphs (a)(1) through (5) of this
section and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(iii) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (a)(1) or (a)(3)
of this section, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(3) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (a)(4) of this section), to a
water identified in paragraphs (a)(1)
through (3) of this section that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (b) of this
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section. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if, for
any length, there are one or more
constructed breaks (such as bridges,
culverts, pipes, or dams), or one or more
natural breaks (such as wetlands along
the run of a stream, debris piles, boulder
fields, or a stream that flows
underground) so long as a bed and
banks and an ordinary high water mark
can be identified upstream of the break.
A water that otherwise qualifies as a
tributary under this definition does not
lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (a)(1) through (3) of this
section.
(4) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(5) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (a)(1)
through (3) of this section. The term ‘‘in
the region’’ means the watershed that
drains to the nearest water identified in
paragraphs (a)(1) through (3) of this
section. For an effect to be significant,
it must be more than speculative or
insubstantial. Waters are similarly
situated when they function alike and
are sufficiently close to function
together in affecting downstream waters.
For purposes of determining whether or
not a water has a significant nexus, the
water’s effect on downstream paragraph
(a)(1) through (3) waters shall be
assessed by evaluating the aquatic
functions identified in paragraphs
(c)(5)(i) through (ix) of this section. A
water has a significant nexus when any
single function or combination of
functions performed by the water, alone
or together with similarly situated
waters in the region, contributes
significantly to the chemical, physical,
or biological integrity of the nearest
water identified in paragraphs (a)(1)
through (3) of this section. Functions
relevant to the significant nexus
evaluation are the following:
(i) Sediment trapping,
(ii) Nutrient recycling,
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(iii) Pollutant trapping,
transformation, filtering, and transport,
(iv) Retention and attenuation of flood
waters,
(v) Runoff storage,
(vi) Contribution of flow,
(vii) Export of organic matter,
(viii) Export of food resources, and
(ix) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (a)(1)
through (3) of this section.
(6) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(7) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
Title 40—Protection of Environment
For reasons set out in the preamble,
title 40, chapter I of the Code of Federal
Regulations is amended as follows:
PART 110—DISCHARGE OF OIL
3. The authority citation for part 110
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq., 33 U.S.C.
1321(b)(3) and (b)(4) and 1361(a); E.O. 11735,
38 FR 21243, 3 CFR parts 1971–1975 Comp.,
p. 793.
4. Section 110.1 is amended by
removing the definition of ‘‘wetlands’’
and revising the definition of ‘‘navigable
waters’’ to read as follows:
■
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§ 110.1
Definitions.
*
*
*
*
*
Navigable waters means waters of the
United States, including the territorial
seas.
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
section, the term ‘‘waters of the United
States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
waters identified in paragraphs (1)(i)
through (iii) of this definition;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
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(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi),
they are an adjacent water and no casespecific significant nexus analysis is
required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this section.
(i) Waste treatment systems (other
than cooling ponds meeting the criteria
of this paragraph) are not waters of the
United States.
(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
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(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(1) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
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(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (iii) of
this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this section), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
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(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
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shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 112—OIL POLLUTION
PREVENTION
5. The authority citation for part 112
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
6. Section 112.2 is amended by
removing the definition of ‘‘wetlands’’
and revising the definition of
‘‘Navigable waters’’ to read as follows:
■
§ 112.2
Definitions.
*
*
*
*
*
Navigable waters means waters of the
United States, including the territorial
seas.
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
waters identified in paragraphs (1)(i)
through (iii) of this definition;
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(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this section when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
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100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi),
they are an adjacent water and no casespecific significant nexus analysis is
required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
(ii) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(iii) Groundwater, including
groundwater drained through
subsurface drainage systems.
(iv) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(v) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
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(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (1)(iii)
of this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
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37109
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
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chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
section. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 116—DESIGNATION OF
HAZARDOUS SUBSTANCE
7. The authority citation for part 116
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
8. Section 116.3 is amended by
revising the definition of ‘‘Navigable
waters’’ to read as follows:
■
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§ 116.3
Definitions.
*
*
*
*
*
Navigable waters is defined in section
502(7) of the Act to mean ‘‘waters of the
United States, including the territorial
seas.’’
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
waters identified in paragraphs (1)(i)
through (iii) of this definition;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
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(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi),
they are an adjacent water and no casespecific significant nexus analysis is
required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(ii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
(iii) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
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(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(iv) Groundwater, including
groundwater drained through
subsurface drainage systems.
(v) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vi) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
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water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (1)(iii)
of this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
PO 00000
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37111
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
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the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 117—DETERMINATION OF
REPORTABLE QUANTITIES FOR
HAZARDOUS SUBSTANCES
9. The authority citation for part 117
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq. and
Executive Order 11735, superseded by
Executive Order 12777, 56 FR 54757.
10. Section 117.1 is amended by
revising paragraph (i) to read as follows:
■
§ 117.1
Definitions.
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*
*
*
*
*
(i) Navigable waters is defined in
section 502(7) of the Act to mean
‘‘waters of the United States, including
the territorial seas.’’
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (i)(2) of this
section, the term ‘‘waters of the United
States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (i)(3)(iii) of this section, of
waters identified in paragraphs (i)(1)(i)
through (iii) of this section;
(vi) All waters adjacent to a water
identified in paragraphs (i)(1)(i) through
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(v) of this section, including wetlands,
ponds, lakes, oxbows, impoundments,
and similar waters;
(vii) All waters in paragraphs
(i)(1)(vii)(A) through (E) of this section
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (i)(1)(i) through (iii) of this
section. The waters identified in each of
paragraphs (i)(1)(vii)(A) through (E) of
this section are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (i)(1)(i)
through (iii) of this section. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (i)(1)(vi) of this section when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(i)(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in (i)(1)(i) through (iii) of this section
and all waters located within 4,000 feet
of the high tide line or ordinary high
water mark of a water identified in
paragraphs (i)(1)(i) through (v) of this
section where they are determined on a
case-specific basis to have a significant
nexus to a water identified in
paragraphs (i)(1)(i) through (iii) of this
section. For waters determined to have
a significant nexus, the entire water is
a water of the United States if a portion
is located within the 100-year
floodplain of a water identified in
paragraphs (i)(1)(i) through (iii) of this
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section or within 4,000 feet of the high
tide line or ordinary high water mark.
Waters identified in this paragraph shall
not be combined with waters identified
in paragraph (i)(1)(vi) of this section
when performing a significant nexus
analysis. If waters identified in this
paragraph are also an adjacent water
under paragraph (i)(1)(vi), they are an
adjacent water and no case-specific
significant nexus analysis is required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(i)(1)(iv) through (viii) of this section.
(i) Waste treatment systems, (other
than cooling ponds meeting the criteria
of this paragraph) are not waters of the
United States.
(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (i)(1)(i)
through (iii) of this section.
(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
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(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this paragraph, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (i)(1)(i)
through (v) of this section, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (i)(1)(i) through
(v) of this section. Adjacent waters also
include all waters that connect segments
of a water identified in paragraphs
(i)(1)(i) through (v) or are located at the
head of a water identified in paragraphs
(i)(1)(i) through (v) of this section and
are bordering, contiguous, or
neighboring such water. Waters being
used for established normal farming,
ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (i)(1)(i)
through (v) of this section. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (i)(1)(i) through (v) of this
section and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (i)(1)(i) or (iii)
of this section, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (i)(1)(iv) of this section), to
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a water identified in paragraphs (i)(1)(i)
through (iii) of this section that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (i)(2) of this
section. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if, for
any length, there are one or more
constructed breaks (such as bridges,
culverts, pipes, or dams), or one or more
natural breaks (such as wetlands along
the run of a stream, debris piles, boulder
fields, or a stream that flows
underground) so long as a bed and
banks and an ordinary high water mark
can be identified upstream of the break.
A water that otherwise qualifies as a
tributary under this definition does not
lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (i)(1)(i) through (iii) of
this section.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (i)(1)(i)
through (iii) of this section. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (i)(1)(i) through
(iii) of this section. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (i)(1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
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37113
paragraphs (i)(3)(v)(A) through (I) of this
section. A water has a significant nexus
when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (i)(1)(i) through (iii) of
this section. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs
(i)(1)(i) through (iii) of this section.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
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PART 122—EPA ADMINISTERED
PERMIT PROGRAMS: THE NATIONAL
POLLUTANT DISCHARGE
ELIMINATION SYSTEM
11. The authority citation for part 122
continues to read as follows:
■
Authority: The Clean Water Act, 33 U.S.C.
1251 et seq.
12. Section 122.2 is amended by:
a. Lifting the suspension of the last
sentence of the definition of ‘‘Waters of
the United States’’ published July 21,
1980 (45 FR 48620);
■ b. Removing the definition of
‘‘wetlands’’ and revising the definition
of ‘‘Waters of the United States’’ and
■ c. Suspending the last sentence of the
definition of ‘‘Waters of the United
States’’ published July 21, 1980 (45 FR
48620).
The revision reads as follows:
■
■
§ 122.2
Definitions.
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Waters of the United States or waters
of the U.S. means:
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this section, of
waters identified in paragraphs (1)(i)
through (iii) of this section;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
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identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(v) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in (1)(i) through (iii) of this definition or
within 4,000 feet of the high tide line or
ordinary high water mark. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) Waste treatment systems, including
treatment ponds or lagoons designed to
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meet the requirements of the Clean
Water Act. This exclusion applies only
to manmade bodies of water which
neither were originally created in waters
of the United States (such as disposal
area in wetlands) nor resulted from the
impoundment of waters of the United
States. [See Note 1 of this section.]
(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
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(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (iii) of
this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
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to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
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37115
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 230—SECTION 404(b)(1)
GUIDELINES FOR SPECIFICATION OF
DISPOSAL SITES FOR DREDGED OR
FILL MATERIAL
13. The authority citation for part 230
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
14. Section 230.3 is amended by:
a. Removing paragraph (b) and
reserved paragraphs (f), (g), (j) and (l).
■
■
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Federal Register / Vol. 80, No. 124 / Monday, June 29, 2015 / Rules
b. Redesignating paragraphs (c)
through (e) as paragraphs (b) through
(d).
■ c. Redesignating paragraphs (h) and (i)
as paragraphs (e) and (f).
■ d. Redesignating paragraph (k) as
paragraph (g).
■ e. Redesignating paragraphs (m)
through (q) as paragraphs (h) through (l).
■ f. Redesignating paragraph (q-1) as
paragraph (m).
■ g. Redesignating paragraph (r) as
paragraph (n).
■ h. Redesignating paragraph (s) as
paragraph (o).
■ i. Revising newly redesignated
paragraph (o).
■ j. Removing paragraph (t).
The revision reads as follows:
■
§ 230.3
Definitions.
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(o) The term waters of the United
States means:
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (o)(2) of this
section, the term ‘‘waters of the United
States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (o)(3)(iii) of this section, of
waters identified in paragraphs (o)(1)(i)
through (iii) of this section;
(vi) All waters adjacent to a water
identified in paragraphs (o)(1)(i) through
(v) of this section, including wetlands,
ponds, lakes, oxbows, impoundments,
and similar waters;
(vii) All waters in paragraphs
(o)(1)(vii)(A) through (E) of this section
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (o)(1)(i) through (iii) of this
section. The waters identified in each of
paragraphs (o)(1)(vii)(A) through (E) of
this section are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (o)(1)(i)
through (iii) of this section. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (o)(1)(vi) of this section when
performing a significant nexus analysis.
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If waters identified in this paragraph are
also an adjacent water under paragraph
(o)(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (o)(1)(i) through (iii) of
this section and all waters located
within 4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (o)(1)(i) through
(v) of this section where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (o)(1)(i) through
(iii) of this section. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (o)(1)(i) through (iii) of
this section or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (o)(1)(vi)
of this section when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph
(o)(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(o)(1)(iv) through (viii) of this section.
(i) Waste treatment systems, including
treatment ponds or lagoons designed to
meet the requirements of the Clean
Water Act are not waters of the United
States.
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(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (o)(1)(i)
through (iii) of this section.
(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this paragraph (o), the following
definitions apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (o)(1)(i)
through (v) of this section, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
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adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (o)(1)(i) through
(v) of this section. Adjacent waters also
include all waters that connect segments
of a water identified in paragraphs
(o)(1)(i) through (v) or are located at the
head of a water identified in paragraphs
(o)(1)(i) through (v) of this section and
are bordering, contiguous, or
neighboring such water. Waters being
used for established normal farming,
ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (o)(1)(i)
through (v) of this section. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (o)(1)(i) through (v) of this
section and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (o)(1)(i) or (iii)
of this section, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (o)(1)(iv) of this section), to
a water identified in paragraphs (o)(1)(i)
through (iii) of this section that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (o)(2) of this
section. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if, for
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any length, there are one or more
constructed breaks (such as bridges,
culverts, pipes, or dams), or one or more
natural breaks (such as wetlands along
the run of a stream, debris piles, boulder
fields, or a stream that flows
underground) so long as a bed and
banks and an ordinary high water mark
can be identified upstream of the break.
A water that otherwise qualifies as a
tributary under this definition does not
lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (o)(1)(i) through (iii) of
this section.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (o)(1)(i)
through (iii) of this section. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (o)(1)(i) through
(iii) of this section. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (o)(1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (o)(3)(v)(A) through (I) of
this section. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (o)(1)(i) through (iii) of
this section. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
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(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (o)(1)
through (3) of this section.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 232—404 PROGRAMS
DEFINITIONS; EXEMPT ACTIVITIES
NOT REQUIRING 404 PERMITS
15. The authority citation for part 230
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
16. Section 232.2 is amended by
removing the definition of ‘‘wetlands’’
and revising the definition of ‘‘Waters of
the United States’’ to read as follows:
■
§ 232.2
Definitions.
*
*
*
*
*
Waters of the United States means:
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
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definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
waters identified in paragraphs (1)(i)
through (iii) of this definition;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
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intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi)
of this definition, they are an adjacent
water and no case-specific significant
nexus analysis is required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) Waste treatment systems, including
treatment ponds or lagoons designed to
meet the requirements of the Clean
Water Act are not waters of the United
States.
(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
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rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
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(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (1)(iii)
of this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
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generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
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land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 300—NATIONAL OIL AND
HAZARDOUS SUBSTANCES
POLLUTION CONTINTENCY PLAN
17. The authority citation for part 300
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
18. Section 300.5 is amended by
revising the definition of ‘‘navigable
waters’’ to read as follows:
■
§ 300.5
Definitions.
*
*
*
*
*
Navigable waters means the waters of
the United States, including the
territorial seas.
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
waters identified in paragraphs (1)(i)
through (iii) of this definition;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
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where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
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this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi),
they are an adjacent water and no casespecific significant nexus analysis is
required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) Waste treatment systems (other
than cooling ponds meeting the criteria
of this paragraph) are not waters of the
United States.
(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
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recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (1)(iii)
of this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
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characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
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nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
■ 19. In appendix E to part 300, section
1.5 Definitions is amended by revising
the definition of ‘‘navigable waters’’ to
read as follows:
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Appendix E to Part 300—Oil Spill
Response
*
*
*
*
*
1.5 Definitions. * * *
Navigable waters means the waters of
the United States, including the
territorial seas.
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
waters identified in paragraphs (1)(i)
through (iii) of this definition;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
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found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi),
they are an adjacent water and no casespecific significant nexus analysis is
required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) Waste treatment systems (other
than cooling ponds meeting the criteria
of this paragraph) are not waters of the
United States.
(ii) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
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a water identified in paragraphs (1)(i)
through (iii) of this definition.
(iv) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(v) Groundwater, including
groundwater drained through
subsurface drainage systems.
(vi) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vii) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
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(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (1)(iii)
of this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
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in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
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physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 302—DESIGNATION,
REPORTABLE QUANTITIES, AND
NOTIFICATION
20. The authority citation for part 302
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
21. Section 302.3 is amended by
revising the definition of ‘‘Navigable
waters’’ to read as follows:
■
§ 302.3
Definitions.
*
*
*
*
*
Navigable waters means the waters of
the United States, including the
territorial seas.
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (2) of this
definition, the term ‘‘waters of the
United States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (3)(iii) of this definition, of
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waters identified in paragraphs (1)(i)
through (iii) of this definition;
(vi) All waters adjacent to a water
identified in paragraphs (1)(i) through
(v) of this definition, including
wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(vii) All waters in paragraphs
(1)(vii)(A) through (E) of this definition
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
definition. The waters identified in each
of paragraphs (1)(vii)(A) through (E) of
this definition are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (1)(i)
through (iii) of this definition. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (1)(vi) of this definition when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition and all waters located within
4,000 feet of the high tide line or
ordinary high water mark of a water
identified in paragraphs (1)(i) through
(v) of this definition where they are
determined on a case-specific basis to
have a significant nexus to a water
identified in paragraphs (1)(i) through
(iii) of this definition. For waters
determined to have a significant nexus,
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the entire water is a water of the United
States if a portion is located within the
100-year floodplain of a water identified
in paragraphs (1)(i) through (iii) of this
definition or within 4,000 feet of the
high tide line or ordinary high water
mark. Waters identified in this
paragraph shall not be combined with
waters identified in paragraph (1)(vi) of
this definition when performing a
significant nexus analysis. If waters
identified in this paragraph are also an
adjacent water under paragraph (1)(vi),
they are an adjacent water and no casespecific significant nexus analysis is
required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(1)(iv) through (viii) of this definition.
(i) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (1)(i)
through (iii) of this definition.
(ii) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(iii) Groundwater, including
groundwater drained through
subsurface drainage systems.
(iv) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(v) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
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structures built for wastewater
recycling.
(3) In this definition, the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (1)(i)
through (v) of this definition, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (1)(i) through
(v) of this definition. Adjacent waters
also include all waters that connect
segments of a water identified in
paragraphs (1)(i) through (v) or are
located at the head of a water identified
in paragraphs (1)(i) through (v) of this
definition and are bordering,
contiguous, or neighboring such water.
Waters being used for established
normal farming, ranching, and
silviculture activities (33 U.S.C. 1344(f))
are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (1)(i)
through (v) of this definition. The entire
water is neighboring if a portion is
located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (1)(i) through (v) of this
definition and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (1)(i) or (iii) of
this definition, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (1)(iv) of this definition), to
a water identified in paragraphs (1)(i)
through (iii) of this definition that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
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physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (2) of this
definition. A water that otherwise
qualifies as a tributary under this
definition does not lose its status as a
tributary if, for any length, there are one
or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one
or more natural breaks (such as
wetlands along the run of a stream,
debris piles, boulder fields, or a stream
that flows underground) so long as a bed
and banks and an ordinary high water
mark can be identified upstream of the
break. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (1)(i)
through (iii) of this definition. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (1)(i) through
(iii) of this definition. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (3)(v)(A) through (I) of this
definition. A water has a significant
nexus when any single function or
combination of functions performed by
the water, alone or together with
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similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (1)(i) through (iii) of this
definition. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs (1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
PART 401—GENERAL PROVISIONS
22. The authority citation for part 401
is revised to read as follows:
■
Authority: 33 U.S.C. 1251 et seq.
23. Section 401.11 is amended by
revising paragraph (l) to read as follows:
■
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§ 401.11
General definitions.
*
*
*
*
*
(l) The term navigable waters means
the waters of the United States,
including the territorial seas.
(1) For purposes of the Clean Water
Act, 33 U.S.C. 1251 et seq. and its
implementing regulations, subject to the
exclusions in paragraph (l)(2) of this
section, the term ‘‘waters of the United
States’’ means:
(i) All waters which are currently
used, were used in the past, or may be
susceptible to use in interstate or foreign
commerce, including all waters which
are subject to the ebb and flow of the
tide;
(ii) All interstate waters, including
interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters
otherwise identified as waters of the
United States under this section;
(v) All tributaries, as defined in
paragraph (l)(3)(iii) of this section, of
waters identified in paragraphs (l)(1)(i)
through (iii) of this section;
(vi) All waters adjacent to a water
identified in paragraphs (l)(1)(i) through
(v) of this section, including wetlands,
ponds, lakes, oxbows, impoundments,
and similar waters;
(vii) All waters in paragraphs
(l)(1)(vii)(A) through (E) of this section
where they are determined, on a casespecific basis, to have a significant
nexus to a water identified in
paragraphs (1)(i) through (iii) of this
section. The waters identified in each of
paragraphs (l)(1)(vii)(A) through (E) of
this section are similarly situated and
shall be combined, for purposes of a
significant nexus analysis, in the
watershed that drains to the nearest
water identified in paragraphs (l)(1)(i)
through (iii) of this section. Waters
identified in this paragraph shall not be
combined with waters identified in
paragraph (l)(1)(vi) of this section when
performing a significant nexus analysis.
If waters identified in this paragraph are
also an adjacent water under paragraph
(l)(1)(vi), they are an adjacent water and
no case-specific significant nexus
analysis is required.
(A) Prairie potholes. Prairie potholes
are a complex of glacially formed
wetlands, usually occurring in
depressions that lack permanent natural
outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays.
Carolina bays and Delmarva bays are
ponded, depressional wetlands that
occur along the Atlantic coastal plain.
(C) Pocosins. Pocosins are evergreen
shrub and tree dominated wetlands
found predominantly along the Central
Atlantic coastal plain.
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37125
(D) Western vernal pools. Western
vernal pools are seasonal wetlands
located in parts of California and
associated with topographic depression,
soils with poor drainage, mild, wet
winters and hot, dry summers.
(E) Texas coastal prairie wetlands.
Texas coastal prairie wetlands are
freshwater wetlands that occur as a
mosaic of depressions, ridges,
intermound flats, and mima mound
wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the
100-year floodplain of a water identified
in (l)(1)(i) through (iii) of this section
and all waters located within 4,000 feet
of the high tide line or ordinary high
water mark of a water identified in
paragraphs (l)(1)(i) through (v) of this
section where they are determined on a
case-specific basis to have a significant
nexus to a water identified in
paragraphs (l)(1)(i) through (iii) of this
section. For waters determined to have
a significant nexus, the entire water is
a water of the United States if a portion
is located within the 100-year
floodplain of a water identified in
paragraphs (l)(1)(i) through (iii) of this
section or within 4,000 feet of the high
tide line or ordinary high water mark.
Waters identified in this paragraph shall
not be combined with waters identified
in paragraph (l)(1)(vi) of this section
when performing a significant nexus
analysis. If waters identified in this
paragraph are also an adjacent water
under paragraph (l)(1)(vi), they are an
adjacent water and no case-specific
significant nexus analysis is required.
(2) The following are not ‘‘waters of
the United States’’ even where they
otherwise meet the terms of paragraphs
(l)(1)(iv) through (viii) of this section.
(i) Prior converted cropland.
Notwithstanding the determination of
an area’s status as prior converted
cropland by any other Federal agency,
for the purposes of the Clean Water Act,
the final authority regarding Clean
Water Act jurisdiction remains with
EPA.
(ii) The following ditches:
(A) Ditches with ephemeral flow that
are not a relocated tributary or
excavated in a tributary.
(B) Ditches with intermittent flow that
are not a relocated tributary, excavated
in a tributary, or drain wetlands.
(C) Ditches that do not flow, either
directly or through another water, into
a water identified in paragraphs (l)(1)(i)
through (iii) of this section.
(iii) The following features:
(A) Artificially irrigated areas that
would revert to dry land should
application of water to that area cease;
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(B) Artificial, constructed lakes and
ponds created in dry land such as farm
and stock watering ponds, irrigation
ponds, settling basins, fields flooded for
rice growing, log cleaning ponds, or
cooling ponds;
(C) Artificial reflecting pools or
swimming pools created in dry land;
(D) Small ornamental waters created
in dry land;
(E) Water-filled depressions created in
dry land incidental to mining or
construction activity, including pits
excavated for obtaining fill, sand, or
gravel that fill with water;
(F) Erosional features, including
gullies, rills, and other ephemeral
features that do not meet the definition
of tributary, non-wetland swales, and
lawfully constructed grassed waterways;
and
(G) Puddles.
(iv) Groundwater, including
groundwater drained through
subsurface drainage systems.
(v) Stormwater control features
constructed to convey, treat, or store
stormwater that are created in dry land.
(vi) Wastewater recycling structures
constructed in dry land; detention and
retention basins built for wastewater
recycling; groundwater recharge basins;
percolation ponds built for wastewater
recycling; and water distributary
structures built for wastewater
recycling.
(3) In this paragraph (l), the following
terms apply:
(i) Adjacent. The term adjacent means
bordering, contiguous, or neighboring a
water identified in paragraphs (l)(1)(i)
through (v) of this section, including
waters separated by constructed dikes or
barriers, natural river berms, beach
dunes, and the like. For purposes of
adjacency, an open water such as a
pond or lake includes any wetlands
within or abutting its ordinary high
water mark. Adjacency is not limited to
waters located laterally to a water
identified in paragraphs (l)(1)(i) through
(v) of this section. Adjacent waters also
include all waters that connect segments
of a water identified in paragraphs
(l)(1)(i) through (v) or are located at the
head of a water identified in paragraphs
(l)(1)(i) through (v) of this section and
are bordering, contiguous, or
neighboring such water. Waters being
used for established normal farming,
ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term
neighboring means:
(A) All waters located within 100 feet
of the ordinary high water mark of a
water identified in paragraphs (l)(1)(i)
through (v) of this section. The entire
water is neighboring if a portion is
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located within 100 feet of the ordinary
high water mark;
(B) All waters located within the 100year floodplain of a water identified in
paragraphs (l)(1)(i) through (v) of this
section and not more than 1,500 feet
from the ordinary high water mark of
such water. The entire water is
neighboring if a portion is located
within 1,500 feet of the ordinary high
water mark and within the 100-year
floodplain;
(C) All waters located within 1,500
feet of the high tide line of a water
identified in paragraphs (l)(1)(i) or (iii)
of this section, and all waters within
1,500 feet of the ordinary high water
mark of the Great Lakes. The entire
water is neighboring if a portion is
located within 1,500 feet of the high tide
line or within 1,500 feet of the ordinary
high water mark of the Great Lakes.
(iii) Tributary and tributaries. The
terms tributary and tributaries each
mean a water that contributes flow,
either directly or through another water
(including an impoundment identified
in paragraph (l)(1)(iv) of this section), to
a water identified in paragraphs (l)(1)(i)
through (iii) of this section that is
characterized by the presence of the
physical indicators of a bed and banks
and an ordinary high water mark. These
physical indicators demonstrate there is
volume, frequency, and duration of flow
sufficient to create a bed and banks and
an ordinary high water mark, and thus
to qualify as a tributary. A tributary can
be a natural, man-altered, or man-made
water and includes waters such as
rivers, streams, canals, and ditches not
excluded under paragraph (l)(2) of this
section. A water that otherwise qualifies
as a tributary under this definition does
not lose its status as a tributary if, for
any length, there are one or more
constructed breaks (such as bridges,
culverts, pipes, or dams), or one or more
natural breaks (such as wetlands along
the run of a stream, debris piles, boulder
fields, or a stream that flows
underground) so long as a bed and
banks and an ordinary high water mark
can be identified upstream of the break.
A water that otherwise qualifies as a
tributary under this definition does not
lose its status as a tributary if it
contributes flow through a water of the
United States that does not meet the
definition of tributary or through a nonjurisdictional water to a water identified
in paragraphs (l)(1)(i) through (iii) of
this section.
(iv) Wetlands. The term wetlands
means those areas that are inundated or
saturated by surface or groundwater at
a frequency and duration sufficient to
support, and that under normal
circumstances do support, a prevalence
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of vegetation typically adapted for life
in saturated soil conditions. Wetlands
generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term
significant nexus means that a water,
including wetlands, either alone or in
combination with other similarly
situated waters in the region,
significantly affects the chemical,
physical, or biological integrity of a
water identified in paragraphs (l)(1)(i)
through (iii) of this section. The term
‘‘in the region’’ means the watershed
that drains to the nearest water
identified in paragraphs (l)(1)(i) through
(iii) of this section. For an effect to be
significant, it must be more than
speculative or insubstantial. Waters are
similarly situated when they function
alike and are sufficiently close to
function together in affecting
downstream waters. For purposes of
determining whether or not a water has
a significant nexus, the water’s effect on
downstream (1)(i) through (iii) waters
shall be assessed by evaluating the
aquatic functions identified in
paragraphs (l)(3)(v)(A) through (I) of this
section. A water has a significant nexus
when any single function or
combination of functions performed by
the water, alone or together with
similarly situated waters in the region,
contributes significantly to the
chemical, physical, or biological
integrity of the nearest water identified
in paragraphs (l)(1)(i) through (iii) of
this section. Functions relevant to the
significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation,
filtering, and transport,
(D) Retention and attenuation of flood
waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent
aquatic habitat (such as foraging,
feeding, nesting, breeding, spawning, or
use as a nursery area) for species located
in a water identified in paragraphs
(l)(1)(i) through (iii) of this section.
(vi) Ordinary high water mark. The
term ordinary high water mark means
that line on the shore established by the
fluctuations of water and indicated by
physical characteristics such as a clear,
natural line impressed on the bank,
shelving, changes in the character of
soil, destruction of terrestrial vegetation,
the presence of litter and debris, or
other appropriate means that consider
the characteristics of the surrounding
areas.
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(vii) High tide line. The term high tide
line means the line of intersection of the
land with the water’s surface at the
maximum height reached by a rising
tide. The high tide line may be
determined, in the absence of actual
data, by a line of oil or scum along shore
objects, a more or less continuous
deposit of fine shell or debris on the
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foreshore or berm, other physical
markings or characteristics, vegetation
lines, tidal gages, or other suitable
means that delineate the general height
reached by a rising tide. The line
encompasses spring high tides and other
high tides that occur with periodic
frequency but does not include storm
surges in which there is a departure
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from the normal or predicted reach of
the tide due to the piling up of water
against a coast by strong winds such as
those accompanying a hurricane or
other intense storm.
*
*
*
*
*
[FR Doc. 2015–13435 Filed 6–26–15; 8:45 am]
BILLING CODE 6560–50–P
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Agencies
[Federal Register Volume 80, Number 124 (Monday, June 29, 2015)]
[Unknown Section]
[Pages 37053-37127]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: 2015-13435]
[[Page 37053]]
Vol. 80
Monday,
No. 124
June 29, 2015
Part II
Department of Defense
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Department of the Army, Corps of Engineers
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33 CFR Part 328
Environmental Protection Agency
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40 CFR Parts 110, 112, 116, et al.
Clean Water Rule: Definition of ``Waters of the United States''; Final
Rule
Federal Register / Vol. 80 , No. 124 / Monday, June 29, 2015 /
Rules
[[Page 37054]]
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DEPARTMENT OF DEFENSE
Department of the Army, Corps of Engineers
33 CFR Part 328
ENVIRONMENTAL PROTECTION AGENCY
40 CFR Parts 110, 112, 116, 117, 122, 230, 232, 300, 302, and 401
[EPA-HQ-OW-2011-0880; FRL-9927-20-OW]
RIN 2040-AF30
Clean Water Rule: Definition of ``Waters of the United States''
AGENCY: U.S. Army Corps of Engineers, Department of the Army,
Department of Defense; and Environmental Protection Agency (EPA).
ACTION: Final rule.
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SUMMARY: The Environmental Protection Agency (EPA) and the U.S. Army
Corps of Engineers (Corps) are publishing a final rule defining the
scope of waters protected under the Clean Water Act (CWA or the Act),
in light of the statute, science, Supreme Court decisions in U.S. v.
Riverside Bayview Homes, Solid Waste Agency of Northern Cook County v.
U.S. Army Corps of Engineers (SWANCC), and Rapanos v. United States
(Rapanos), and the agencies' experience and technical expertise. This
final rule reflects consideration of the extensive public comments
received on the proposed rule. The rule will ensure protection for the
nation's public health and aquatic resources, and increase CWA program
predictability and consistency by clarifying the scope of ``waters of
the United States'' protected under the Act.
DATES: This rule is effective on August 28, 2015. In accordance with 40
CFR part 23, this regulation shall be considered issued for purposes of
judicial review at 1 p.m. Eastern time on July 13, 2015.
FOR FURTHER INFORMATION CONTACT: Ms. Donna Downing, Office of Water
(4502-T), Environmental Protection Agency, 1200 Pennsylvania Avenue
NW., Washington, DC 20460; telephone number 202-566-2428; email
address: CWAwaters@epa.go v. Ms. Stacey Jensen, Regulatory Community of
Practice (CECW-CO-R), U.S. Army Corps of Engineers, 441 G Street NW.,
Washington, DC 20314; telephone number 202-761-5856; email address:
USACE_CWA_Rule@usace.army.mil.
SUPPLEMENTARY INFORMATION: This final rule does not establish any
regulatory requirements. Instead, it is a definitional rule that
clarifies the scope of ``waters of the United States'' consistent with
the Clean Water Act (CWA), Supreme Court precedent, and science.
Programs established by the CWA, such as the section 402 National
Pollutant Discharge Elimination System (NPDES) permit program, the
section 404 permit program for discharge of dredged or fill material,
and the section 311 oil spill prevention and response programs, all
rely on the definition of ``waters of the United States.'' Entities
currently are, and will continue to be, regulated under these programs
that protect ``waters of the United States'' from pollution and
destruction.
State, tribal, and local governments have well-defined and
longstanding relationships with the Federal government in implementing
CWA programs and these relationships are not altered by the final rule.
Forty-six states and the U.S. Virgin Islands have been authorized by
EPA to administer the NPDES program under section 402, and two states
have been authorized by the EPA to administer the section 404 program.
All states and forty tribes have developed water quality standards
under the CWA for waters within their boundaries. A federal advisory
committee has recently been announced to assist states in identifying
the scope of waters assumable under the section 404 program.
The scope of jurisdiction in this rule is narrower than that under
the existing regulation. Fewer waters will be defined as ``waters of
the United States'' under the rule than under the existing regulations,
in part because the rule puts important qualifiers on some existing
categories such as tributaries. In addition, the rule provides greater
clarity regarding which waters are subject to CWA jurisdiction,
reducing the instances in which permitting authorities, including the
states and tribes with authorized section 402 and 404 CWA permitting
programs, would need to make jurisdictional determinations on a case-
specific basis.
Table of Contents
I. General Information
A. How can I get copies of this document and related
information?
B. Under what legal authority is this rule issued?
II. Executive Summary
III. Significant Nexus Determinations
A. The Significant Nexus Standard
B. Science Report
C. Significant Nexus Conclusions
1. Scope of Significant Nexus Analysis
2. Categories of Waters Determined to Have a Significant Nexus
3. Case-Specific Significant Nexus Determinations
IV. Definition of ``Waters of the United States''
A. Summary of Rule
B. Traditional Navigable Waters
C. Interstate Waters
D. Territorial Seas
E. Impoundments
F. Tributaries
G. Adjacent Waters
H. Case-Specific ``Waters of the United States''
I. Waters and Features That Are Not ``Waters of the United
States''
V. Economic Impacts
VI. Related Acts of Congress, Executive Orders, and Agency
Initiatives
A. Executive Order 12866: Regulatory Planning and Review and
Executive Order 13563: Improving Regulation and Regulatory Review
B. Paperwork Reduction Act
C. Regulatory Flexibility Act
D. Unfunded Mandates Reform Act
E. Executive Order 13132: Federalism
F. Executive Order 13175: Consultation and Coordination With
Indian Tribal Governments
G. Executive Order 13045: Protection of Children From
Environmental Health and Safety Risks
H. Executive Order 13211: Actions Concerning Regulations That
Significantly Affect Energy Supply, Distribution, or Use
I. National Technology Transfer and Advancement Act
J. Executive Order 12898: Federal Actions To Address
Environmental Justice in
Minority Populations and Low-Income Populations
K. Congressional Review Act
L. Environmental Documentation
M. Judicial Review
I. General Information
A. How can I get copies of this document and related information?
1. Docket. An official public docket for this action has been
established under Docket Id. No. EPA-HQ-OW-2011-0880. The official
public docket consists of the documents specifically referenced in this
action, any public comments received, and other information related to
this action. The official public docket also includes a Technical
Support Document that provides additional legal and scientific
discussion for issues raised in this rule, and the Response to Comments
document. Although a part of the official docket, the public docket
does not include Confidential Business Information or other information
whose disclosure is restricted by statute. The official public docket
is the collection of materials that is available for public viewing at
the OW Docket, EPA West, Room 3334, 1301 Constitution Ave. NW.,
Washington, DC 20004. This Docket Facility is open from 8:30 a.m.
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to 4:30 p.m., Monday through Friday, excluding legal holidays. The OW
Docket telephone number is 202-566-2426. A reasonable fee will be
charged for copies.
2. Electronic Access. You may access this Federal Register document
electronically under the ``Federal Register'' listings at https://www.regulations.gov. An electronic version of the public docket is
available through EPA's electronic public docket and comment system,
EPA Dockets. You may access EPA Dockets at https://www.regulations.gov
to view public comments, access the index listing of the contents of
the official public docket, and access those documents in the public
docket that are available electronically. For additional information
about EPA's public docket, visit the EPA Docket Center homepage at
https://www.epa.gov/epahome/dockets.htm. Although not all docket
materials may be available electronically, you may still access any of
the publicly available docket materials through the Docket Facility.
B. Under what legal authority is this rule issued?
The authority for this rule is the Federal Water Pollution Control
Act, 33 U.S.C. 1251, et seq., including sections 301, 304, 311, 401,
402, 404 and 501.
II. Executive Summary
In this final rule, the agencies clarify the scope of ``waters of
the United States'' that are protected under the Clean Water Act (CWA),
based upon the text of the statute, Supreme Court decisions, the best
available peer-reviewed science, public input, and the agencies'
technical expertise and experience in implementing the statute. This
rule makes the process of identifying waters \1\ protected under the
CWA easier to understand, more predictable, and consistent with the law
and peer-reviewed science, while protecting the streams and wetlands
that form the foundation of our nation's water resources.
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\1\ The agencies use the term ``water'' and ``waters'' in
categorical reference to rivers, streams, ditches, wetlands, ponds,
lakes, oxbows, and other types of natural or man-made aquatic
systems, identifiable by the water contained in these aquatic
systems or by their chemical, physical, and biological indicators.
The agencies use the terms ``waters'' and ``water bodies''
interchangeably in this preamble.
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Congress enacted the CWA ``to restore and maintain the chemical,
physical, and biological integrity of the Nation's waters,'' section
101(a), and to complement statutes that protect the navigability of
waters, such as the Rivers and Harbors Act. 33 U.S.C. 401, 403, 404,
407. The CWA is the nation's single most important statute for
protecting America's clean water against pollution, degradation, and
destruction. To provide that protection, the Supreme Court has
consistently agreed that the geographic scope of the CWA reaches beyond
waters that are navigable in fact. Peer-reviewed science and practical
experience demonstrate that upstream waters, including headwaters and
wetlands, significantly affect the chemical, physical, and biological
integrity of downstream waters by playing a crucial role in controlling
sediment, filtering pollutants, reducing flooding, providing habitat
for fish and other aquatic wildlife, and many other vital chemical,
physical, and biological processes.
This final rule interprets the CWA to cover those waters that
require protection in order to restore and maintain the chemical,
physical, or biological integrity of traditional navigable waters,
interstate waters, and the territorial seas. This interpretation is
based not only on legal precedent and the best available peer-reviewed
science, but also on the agencies' technical expertise and extensive
experience in implementing the CWA over the past four decades. The rule
will clarify and simplify implementation of the CWA consistent with its
purposes through clearer definitions and increased use of bright-line
boundaries to establish waters that are jurisdictional by rule and
limit the need for case-specific analysis. The agencies emphasize that,
while the CWA establishes permitting requirements for covered waters to
ensure protection of water quality, these requirements only apply with
respect to discharges of pollutants to the covered water. In the
absence of a discharge of a pollutant, the CWA does not impose
permitting restrictions on the use of such water.
Additionally, Congress has exempted certain discharges, and the
rule does not affect any of the exemptions from CWA section 404
permitting requirements provided by CWA section 404(f), including those
for normal farming, ranching, and silviculture activities. CWA section
404(f); 40 CFR 232.3; 33 CFR 323.4. This rule not only maintains
current statutory exemptions, it expands regulatory exclusions from the
definition of ``waters of the United States'' to make it clear that
this rule does not add any additional permitting requirements on
agriculture. The rule also does not regulate shallow subsurface
connections nor any type of groundwater, erosional features, or land
use, nor does it affect either the existing statutory or regulatory
exemptions from NPDES permitting requirements, such as for agricultural
stormwater discharges and return flows from irrigated agriculture, or
the status of water transfers. CWA section 402(l)(1); CWA section
402(l)(2); CWA section 502(14); 40 CFR 122.3(f); 40 CFR 122.2.
Finally, even where waters are covered by the CWA, the agencies
have adopted many streamlined regulatory requirements to simplify and
expedite compliance through the use of measures such as general permits
and standardized mitigation measures. The agencies will continue to
develop general permits and simplified procedures, particularly as they
affect crossings of covered ephemeral and intermittent tributaries
jurisdictional under this rule to ensure that projects that offer
significant social benefits, such as renewable energy development, can
proceed with the necessary environmental safeguards while minimizing
permitting delays.
The jurisdictional scope of the CWA is ``navigable waters,''
defined in section 502(7) of the statute as ``waters of the United
States, including the territorial seas.'' The term ``navigable waters''
is used in a number of provisions of the CWA, including the section 402
National Pollutant Discharge Elimination System (NPDES) permit program,
the section 404 permit program, the section 311 oil spill prevention
and response program,\2\ the water quality standards and total maximum
daily load programs (TMDL) under section 303, and the section 401 state
water quality certification process. However, while there is only one
CWA definition of ``waters of the United States,'' there may be other
statutory factors that define the reach of a particular CWA program or
provision.\3\
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Existing regulations (last codified in 1986) define ``waters of the
United States'' as traditional navigable waters, interstate waters, all
other waters that could affect interstate or foreign commerce,
impoundments of waters of the United States, tributaries, the
territorial seas, and adjacent wetlands. 33 CFR 328.3; 40 CFR 122.2.\4\
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\2\ While section 311 uses the phrase ``navigable waters of the
United States,'' EPA has interpreted it to have the same breadth as
the phrase ``navigable waters'' used elsewhere in section 311, and
in other sections of the CWA. See United States v. Texas Pipe Line
Co., 611 F.2d 345, 347 (10th Cir. 1979); United States v. Ashland
Oil & Transp. Co., 504 F.2d 1317, 1324-25 (6th Cir. 1974). In 2002,
EPA revised its regulatory definition of ``waters of the United
States'' in 40 CFR part 112 to ensure that the language of the rule
was consistent with the regulatory language of other CWA programs.
Oil Pollution Prevention & Response; Non-Transportation-Related
Onshore & Offshore Facilities, 67 FR 47042, July 17, 2002. A
district court vacated the rule for failure to comply with the
Administrative Procedure Act, and reinstated the prior regulatory
language. American Petroleum Ins. v. Johnson, 541 F. Supp. 2d 165
(D. D.C. 2008). However, EPA interprets ``navigable waters of the
United States'' in CWA section 311(b), in the pre-2002 regulations,
and in the 2002 rule to have the same meaning as ``navigable
waters'' in CWA section 502(7).
\3\ For example, the CWA section 402 (33 U.S.C. 1342) program
regulates discharges of pollutants from ``point sources'' to
``waters of the United States,'' whether these pollutants reach
jurisdictional waters directly or indirectly. The plurality opinion
in Rapanos noted that ``there is no reason to suppose that our
construction today significantly affects the enforcement of Sec.
1342. . . . The Act does not forbid the `addition of any pollutant
directly to navigable waters from any point source,' but rather the
`addition of any pollutant to navigable waters.' '' 547 U.S. at 743.
\4\ There are numerous regulations that utilize the definition
of ``waters of the United States'' and each is codified consistent
with its place in a particular section of the Code of Federal
Regulations. For simplicity, throughout the preamble the agencies
refer to the rule as organized into (a), (b), (c) provisions and
intend the reference to encompass the appropriate cites in each
section of the Code of Federal Regulations. For example, a reference
to (a)(1) is a reference to all instances in the CFR identified as
subject to this rule that state ``All waters which are currently
used, were used in the past, or may be susceptible to use in
interstate or foreign commerce, including all waters which are
subject to the ebb and flow of the tide.''
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However, the Supreme Court has issued three decisions that provide
critical context and guidance in determining the appropriate scope of
``waters of the United States'' covered by the CWA. In United States v.
Riverside Bayview Homes, 474 U.S. 121 (1985) (Riverside), the Court, in
a unanimous opinion, deferred to the Corps' ecological judgment that
adjacent wetlands are ``inseparably bound up'' with the waters to which
they are adjacent, and upheld the inclusion of adjacent wetlands in the
regulatory definition of ``waters of the United States.'' Id. at 134.
The Court observed that the broad objective of the CWA to restore and
maintain the integrity of the Nation's waters ``incorporated a broad,
systemic view of the goal of maintaining and improving water quality. .
. . Protection of aquatic ecosystems, Congress recognized, demanded
broad federal authority to control pollution, for `[w]ater moves in
hydrologic cycles and it is essential that discharge of pollutants be
controlled at the source.' In keeping with these views, Congress chose
to define the waters covered by the Act broadly.'' Id. at 132-33
(citing Senate Report No. 92-414, p. 77 (1972)).
In Solid Waste Agency of Northern Cook County v. U.S. Army Corps of
Engineers, 531 U.S. 159 (2001) (SWANCC), the Supreme Court held that
the use of ``isolated'' non-navigable intrastate ponds by migratory
birds was not by itself a sufficient basis for the exercise of federal
regulatory authority under the CWA. Although the SWANCC decision did
not call into question earlier decisions upholding the CWA's coverage
of wetlands or other waters ``adjacent'' to traditional navigable
waters, it created uncertainty with regard to the jurisdiction of other
waters and wetlands that, in many instances, may play an important role
in protecting the integrity of the nation's waters. The majority
opinion in SWANCC introduced the concept that it was a ``significant
nexus'' that informed the Court's reading of CWA jurisdiction over
waters that are not navigable in fact.
Five years later, in Rapanos v. United States, 547 U.S. 715 (2006)
(Rapanos), all Members of the Court agreed that the term ``waters of
the United States'' encompasses some waters that are not navigable in
the traditional sense. In addition, Justice Kennedy's opinion indicated
that the critical factor in determining the CWA's coverage is whether a
water has a ``significant nexus'' to downstream traditional navigable
waters such that the water is important to protecting the chemical,
physical, or biological integrity of the navigable water, referring
back to the Court's decision in SWANCC. Justice Kennedy's concurrence
in Rapanos stated that to constitute a ``water of the United States''
covered by the CWA, ``a water or wetland must possess a `significant
nexus' to waters that are or were navigable in fact or that could
reasonably be so made.'' Id. at 759 (Kennedy, J., concurring in the
judgment) (citing SWANCC, 531 U.S. at 167, 172). Justice Kennedy
concluded that wetlands possess the requisite significant nexus if the
wetlands ``either alone or in combination with similarly situated
[wet]lands in the region, significantly affect the chemical, physical,
and biological integrity of other covered waters more readily
understood as `navigable.''' 547 U.S. at 780.
In this rule, the agencies interpret the scope of the ``waters of
the United States'' for the CWA using the goals, objectives, and
policies of the statute, the Supreme Court case law, the relevant and
available science, and the agencies' technical expertise and experience
as support. In particular, the agencies looked to the objective of the
CWA ``to restore and maintain the chemical, physical, and biological
integrity of the Nation's waters,'' and the scientific consensus on the
strength of the effects of upstream tributaries and adjacent waters,
including wetlands, on downstream traditional navigable waters,
interstate waters, and the territorial seas. An important element of
the agencies' interpretation of the CWA is the significant nexus
standard. This significant nexus standard was first informed by the
ecological and hydrological connections the Supreme Court noted in
Riverside Bayview, developed and established by the Supreme Court in
SWANCC, and further refined in Justice Kennedy's opinion in Rapanos.
The agencies also utilized the plurality standard in Rapanos by
establishing boundaries on the scope of ``waters of the United States''
and in support of the exclusions from the definition of ``waters of the
United States.'' The analysis used by the agencies has been supported
by all nine of the United States Courts of Appeals that have considered
the issue.
The agencies assess the significance of the nexus in terms of the
CWA's objective to ``restore and maintain the chemical, physical, and
biological integrity of the Nation's waters.'' When the effects are
speculative or insubstantial, the ``significant nexus'' would not be
present. The science demonstrates that the protection of upstream
waters is critical to maintaining the integrity of the downstream
waters. The upstream waters identified in the rule as jurisdictional
function as integral parts of the aquatic environment, and if these
waters are polluted or destroyed, there is a significant effect
downstream.
In response to the Supreme Court opinions, the agencies issued
guidance in 2003 (post-SWANCC) and 2008 (post-Rapanos). However, these
two guidance documents did not provide the public or agency staff with
the kind of information needed to ensure timely, consistent, and
predictable jurisdictional determinations. Many waters are currently
subject to case-specific jurisdictional analysis to determine whether a
``significant nexus'' exists, and this time and resource intensive
process can result in inconsistent interpretation of CWA jurisdiction
and perpetuate ambiguity over where the CWA applies. As a result of the
ambiguity that exists under current regulations and practice following
these recent decisions, almost all waters and wetlands across the
country theoretically could be subject to a case-specific
jurisdictional determination.
Members of Congress, developers, farmers, state and local
governments, energy companies, and many others requested new
regulations to make the process of identifying waters protected under
the CWA clearer, simpler, and faster. Chief Justice Roberts'
concurrence in Rapanos underscores
[[Page 37057]]
the importance of this rulemaking effort.\5\ In this final rule, the
agencies are responding to those requests from across the country to
make the process of identifying waters protected under the CWA easier
to understand, more predictable, and more consistent with the law and
peer-reviewed science.
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\5\ Chief Justice Roberts' concurrence in Rapanos emphasized
that ``[a]gencies delegated rulemaking authority under a statute
such as the Clean Water Act are afforded generous leeway by the
courts in interpreting the statute they are entrusted to
administer.'' Id. at 758. Chief Justice Roberts made clear that, if
the agencies had undertaken such a rulemaking, ``the Corps and the
EPA would have enjoyed plenty of room to operate in developing some
notion of an outer bound to the reach of their authority.'' Id.
(Emphasis in original.)
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The agencies proposed a rule clarifying the scope of waters of the
United States April 21, 2014 (79 FR 22188), and solicited comments for
over 200 days. This final rule reflects the over 1 million public
comments on the proposal, the substantial majority of which supported
the proposed rule, as well as input provided through the agencies'
extensive public outreach effort, which included over 400 meetings
nationwide with states, small businesses, farmers, academics, miners,
energy companies, counties, municipalities, environmental
organizations, other federal agencies, and many others. The agencies
sought comment on a number of approaches to specific jurisdictional
questions, and many of these commenters and stakeholders urged EPA to
improve upon the April 2014 proposal, by providing more bright line
boundaries and simplifying definitions that identify waters that are
protected under the CWA, all for the purpose of minimizing delays and
costs, making protection of clean water more effective, and improving
predictability and consistency for landowners and regulated entities.
The agencies' interpretation of the CWA's scope in this final rule
is guided by the best available peer-reviewed science--particularly as
that science informs the determinations as to which waters have a
``significant nexus'' with traditional navigable waters, interstate
waters, or the territorial seas.
The relevant science on the relationship and downstream effects of
waters has advanced considerably in recent years. A comprehensive
report prepared by the EPA's Office of Research and Development
entitled ``Connectivity of Streams and Wetlands to Downstream Waters: A
Review and Synthesis of the Scientific Evidence'' \6\ (hereafter the
Science Report) synthesizes the peer-reviewed science.
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\6\ U.S. Environmental Protection Agency, Connectivity of
Streams and Wetlands to Downstream Waters: A Review and Synthesis of
the Scientific Evidence (Final Report), EPA/600/R-14/475F,
(Washington, DC: U.S. Environmental Protection Agency, (2015)).
https://www.epa.gov/ncea.
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The Science Report provides much of the technical basis for this
rule. The Science Report is based on a review of more than 1,200 peer-
reviewed publications. EPA's Science Advisory Board (SAB) conducted a
comprehensive technical review of the Science Report and reviewed the
adequacy of the scientific and technical basis of the proposed rule.
The Science Report and the SAB review confirmed that:
Waters are connected in myriad ways, including physical
connections and the hydrologic cycle; however, connections occur on a
continuum or gradient from highly connected to highly isolated.
These variations in the degree of connectivity are a
critical consideration to the ecological integrity and sustainability
of downstream waters.
The critical contribution of upstream waters to the
chemical, physical, and biological integrity of downstream waters
results from the accumulative contribution of similar waters in the
same watershed and in the context of their functions considered over
time.
The Science Report and the SAB review also confirmed that:
Tributary streams, including perennial, intermittent, and
ephemeral streams, are chemically, physically, and biologically
connected to downstream waters, and influence the integrity of
downstream waters.
Wetlands and open waters in floodplains and riparian areas
are chemically, physically, and biologically connected with downstream
waters and influence the ecological integrity of such waters.
Non-floodplain wetlands and open waters provide many
functions that benefit downstream water quality and ecological
integrity, but their effects on downstream waters are difficult to
assess based solely on the available science.
Although these conclusions play a critical role in informing the
agencies' interpretation of the CWA's scope, the agencies' interpretive
task in this rule--determining which waters have a ``significant
nexus''--requires scientific and policy judgment, as well as legal
interpretation. The science demonstrates that waters fall along a
gradient of chemical, physical, and biological connection to
traditional navigable waters, and it is the agencies' task to determine
where along that gradient to draw lines of jurisdiction under the CWA.
In making this determination, the agencies must rely, not only on the
science, but also on their technical expertise and practical experience
in implementing the CWA during a period of over 40 years. In addition,
the agencies are guided, in part, by the compelling need for clearer,
more consistent, and easily implementable standards to govern
administration of the Act, including brighter line boundaries where
feasible and appropriate.
Major Rule Provisions
In this final rule, the agencies define ``waters of the United
States'' to include eight categories of jurisdictional waters. The rule
maintains existing exclusions for certain categories of waters, and
adds additional categorical exclusions that are regularly applied in
practice. The rule reflects the agencies' goal of providing simpler,
clearer, and more consistent approaches for identifying the geographic
scope of the CWA. The rule recognizes jurisdiction for three basic
categories: Waters that are jurisdictional in all instances, waters
that are excluded from jurisdiction, and a narrow category of waters
subject to case-specific analysis to determine whether they are
jurisdictional.
Decisions about waters in each of these categories are based on the
law, peer-reviewed science, and the agencies' technical expertise, and
were informed by public comments. This rule replaces existing
procedures that often depend on individual, time-consuming, and
inconsistent analyses of the relationship between a particular stream,
wetland, lake, or other water with downstream waters. The agencies have
greatly reduced the extent of waters subject to this individual review
by carefully incorporating the scientific literature and by utilizing
agency expertise and experience to characterize the nature and strength
of the chemical, physical, and biological connections between upstream
and downstream waters. The result of applying this scientific analysis
is that the agencies can more effectively focus the rule on identifying
waters that are clearly covered by the CWA and those that are clearly
not covered, making the rule easier to understand, consistent, and
environmentally more protective.
The jurisdictional categories reflect the current state of the best
available science, and are based upon the law and Supreme Court
decisions. The agencies will continue a transparent review of the
science, and learn from on-going
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experience and expertise as the agencies implement the rule. If
evolving science and the agencies' experience lead to a need for action
to alter the jurisdictional categories, any such action will be
conducted as part of a rule-making process.
The first three types of jurisdictional waters, traditional
navigable waters, interstate waters, and the territorial seas, are
jurisdictional by rule in all cases. The fourth type of water,
impoundments of jurisdictional waters, is also jurisdictional by rule
in all cases. The next two types of waters, ``tributaries'' and
``adjacent'' waters, are jurisdictional by rule, as defined, because
the science confirms that they have a significant nexus to traditional
navigable waters, interstate waters, or territorial seas. For waters
that are jurisdictional by rule, no additional analysis is required.
The final two types of jurisdictional waters are those waters found
after a case-specific analysis to have a significant nexus to
traditional navigable waters, interstate waters, or the territorial
seas, either alone or in combination with similarly situated waters in
the region. Justice Kennedy acknowledged the agencies could establish
more specific regulations or establish a significant nexus on a case-
by-case basis, Rapanos at 782, and for these waters the agencies will
continue to assess significant nexus on a case-specific basis.
The major elements of the final rule are briefly summarized here.
Traditional Navigable Waters, Interstate Waters, Territorial Seas, and
Impoundments of Jurisdictional Waters
Consistent with existing regulations and the April 2014 proposed
rule, the final rule includes traditional navigable waters, interstate
waters, territorial seas, and impoundments of jurisdictional waters in
the definition of ``waters of the United States.'' These waters are
jurisdictional by rule.
Tributaries
Previous definitions of ``waters of the United States'' regulated
all tributaries without qualification. This final rule more precisely
defines ``tributaries'' as waters that are characterized by the
presence of physical indicators of flow--bed and banks and ordinary
high water mark--and that contribute flow directly or indirectly to a
traditional navigable water, an interstate water, or the territorial
seas. The rule concludes that such tributaries are ``waters of the
United States.'' The great majority of tributaries as defined by the
rule are headwater streams that play an important role in the transport
of water, sediments, organic matter, nutrients, and organisms to
downstream waters. The physical indicators of bed and banks and
ordinary high water mark demonstrate that there is sufficient volume,
frequency, and flow in such tributaries to a traditional navigable
water, interstate water, or the territorial seas to establish a
significant nexus. ``Tributaries,'' as defined, are jurisdictional by
rule.
The rule only covers as tributaries those waters that science tells
us provide chemical, physical, or biological functions to downstream
waters and that meet the significant nexus standard. The agencies
identify these functions in the definition of ``significant nexus'' at
paragraph (c)(5). Features not meeting this legal and scientific test
are not jurisdictional under this rule. The rule continues the current
policy of regulating ditches that are constructed in tributaries or are
relocated tributaries or, in certain circumstances drain wetlands, or
that science clearly demonstrates are functioning as a tributary. These
jurisdictional waters affect the chemical, physical, and biological
integrity of downstream waters. The rule further reduces existing
confusion and inconsistency regarding the regulation of ditches by
explicitly excluding certain categories of ditches, such as ditches
that flow only after precipitation. Further, the rule explicitly
excludes from the definition of ``waters of the United States''
erosional features, including gullies, rills, and ephemeral features
such as ephemeral streams that do not have a bed and banks and ordinary
high water mark.
Adjacent Waters
The agencies determined that ``adjacent waters,'' as defined in the
rule, have a significant nexus to traditional navigable waters,
interstate waters, and the territorial seas based upon their
hydrological and ecological connections to, and interactions with,
those waters. Under this final rule, ``adjacent'' means bordering,
contiguous, or neighboring, including waters separated from other
``waters of the United States'' by constructed dikes or barriers,
natural river berms, beach dunes and the like. Further, waters that
connect segments of, or are at the head of, a stream or river are
``adjacent'' to that stream or river. ``Adjacent waters'' include
wetlands, ponds, lakes, oxbows, impoundments, and similar water
features. However, it is important to note that ``adjacent waters'' do
not include waters that are subject to established normal farming,
silviculture, and ranching activities as those terms are used in
Section 404(f) of the CWA.
The final rule establishes a definition of ``neighboring'' for
purposes of determining adjacency. In the rule, the agencies identify
three circumstances under which waters would be ``neighboring'' and
therefore ``waters of the United States'':
(1) Waters located in whole or in part within 100 feet of the
ordinary high water mark of a traditional navigable water, interstate
water, the territorial seas, an impoundment of a jurisdictional water,
or a tributary, as defined in the rule.
(2) Waters located in whole or in part in the 100-year floodplain
and that are within 1,500 feet of the ordinary high water mark of a
traditional navigable water, interstate water, the territorial seas, an
impoundment, or a tributary, as defined in the rule (``floodplain
waters'').
(3) Waters located in whole or in part within 1,500 feet of the
high tide line of a traditional navigable water or the territorial seas
and waters located within 1,500 feet of the ordinary high water mark of
the Great Lakes.
The agencies emphasize that the rule has defined as ``adjacent
waters'' those waters that currently available science demonstrates
possess the requisite connection to downstream waters and function as a
system to protect the chemical, physical, or biological integrity of
those waters. The agencies also emphasize that the rule does not cover
``adjacent waters'' that are otherwise excluded. Further, the agencies
recognize the establishment of bright line boundaries in the rule for
adjacency does not in any way restrict states from considering state
specific information and concerns, as well as emerging science to
evaluate the need to more broadly protect their waters under state law.
The CWA establishes both national and state roles to ensure that states
specific circumstances are properly considered to complement and
reinforce actions taken at the national level.
``Adjacent'' waters as defined are jurisdictional by rule. The
agencies recognize that there are individual waters outside of the
``neighboring'' boundaries stated above where the science may
demonstrate through a case-specific analysis that there exists a
significant nexus to a downstream traditional navigable water,
interstate water, or the territorial seas. However, these waters are
not determined jurisdictional by rule and will be evaluated through a
case-specific analysis. The strength of the science and
[[Page 37059]]
the significance of the nexus will be established on a case-specific
basis as described below.
Case-Specific Significant Nexus
The rule identifies particular waters that are not jurisdictional
by rule but are subject to case-specific analysis to determine if a
significant nexus exists and the water is a ``water of the United
States.'' This category of case-specific waters is based upon available
science and the law, and in response to public comments that encouraged
the agencies to ensure more consistent determinations and reduce the
complexity of conducting jurisdictional determinations. Consistent with
the significant nexus standard articulated in the Supreme Court
opinions, waters are ``waters of the United States'' if they
significantly affect the chemical, physical, or biological integrity of
traditional navigable waters, interstate waters, or the territorial
seas. This determination will most typically be made on a water
individually, but can, when warranted, be made in combination with
other waters where waters function together.
In this final rule, the agencies have identified by rule, five
specific types of waters in specific regions that science demonstrates
should be subject to a significant nexus analysis and are considered
similarly situated by rule because they function alike and are
sufficiently close to function together in affecting downstream waters.
These five types of waters are Prairie potholes, Carolina and Delmarva
bays, pocosins, western vernal pools in California, and Texas coastal
prairie wetlands. Consistent with Justice Kennedy's opinion in Rapanos,
the agencies determined that such waters should be analyzed ``in
combination'' (as a group, rather than individually) in the watershed
that drains to the nearest traditional navigable water, interstate
water, or the territorial seas when making a case-specific analysis of
whether these waters have a significant nexus to traditional navigable
waters, interstate waters, or territorial seas.
The final rule also provides that waters within the 100-year
floodplain of a traditional navigable water, interstate water, or the
territorial seas and waters within 4,000 feet of the high tide line or
the ordinary high water mark of a traditional navigable water,
interstate water, the territorial seas, impoundments, or covered
tributary are subject to case-specific significant nexus
determinations, unless the water is excluded under paragraph (b) of the
rule. The science available today does not establish that waters beyond
those defined as ``adjacent'' should be jurisdictional as a category
under the CWA, but the agencies' experience and expertise indicate that
there are many waters within the 100-year floodplain of a traditional
navigable water, interstate water, or the territorial seas or out to
4,000 feet where the science demonstrates that they have a significant
effect on downstream waters.
In circumstances where waters within the 100-year floodplain of a
traditional navigable water, interstate water, or the territorial seas
or within 4,000 feet of the high tide line or ordinary high water mark
are subject to a case-specific significant nexus analysis and such
waters may be evaluated as ``similarly situated,'' it must be first
demonstrated that these waters function alike and are sufficiently
close to function together in affecting downstream waters. The
significant nexus analysis must then be conducted based on
consideration of the functions provided by those waters in combination
in the point of entry watershed. A ``similarly situated'' analysis is
conducted where it is determined that there is a likelihood that there
are waters that function together to affect downstream water integrity.
To provide greater clarity and transparency in determining what
functions will be considered in determining what constitutes a
significant nexus, the final rule lists specific functions that the
agencies will consider.
In establishing both the 100-year floodplain and the 4,000 foot
bright line boundaries for these case-specific significant nexus
determinations in the rule, the agencies are carefully applying the
available science. Consistent with the CWA, the agencies will work with
the states in connection with the prevention, reduction and elimination
of pollution from state waters. The agencies will work with states to
more closely evaluate state-specific circumstances that may be present
within their borders and, as appropriate, encourage states to develop
rules that reflect their circumstances and emerging science to ensure
consistent and effective protection for waters in the states. As is the
case today, nothing in this rule restricts the ability of states to
more broadly protect state waters.
Exclusions
All existing exclusions from the definition of ``waters of the
United States'' are retained, and several exclusions reflecting
longstanding agency practice are added to the regulation for the first
time.
Prior converted cropland and waste treatment systems have been
excluded from the definition of ``waters of the United States''
definition since 1992 and 1979 respectively, and continue to be
excluded. Ministerial changes are made for purposes of clarity, but
these two exclusions remain substantively and operationally unchanged.
The agencies add exclusions for waters and features previously
identified as generally exempt (e.g., exclusion for certain ditches
that are not located in or drain wetlands) in preamble language from
Federal Register documents by the Corps on November 13, 1986, and by
EPA on June 6, 1988. This is the first time these exclusions have been
established by rule. The agencies for the first time also establish by
rule that certain ditches are excluded from jurisdiction, including
ditches with ephemeral flow that are not a relocated tributary or
excavated in a tributary, and ditches with intermittent flow that are
not a relocated tributary, or excavated in a tributary, or drain
wetlands. The agencies add exclusions for groundwater and erosional
features, as well as exclusions for some waters that were identified in
public comments as possibly being found jurisdictional under proposed
rule language where this was never the agencies' intent, such as
stormwater control features constructed to convey, treat, or store
stormwater, and cooling ponds that are created in dry land. These
exclusions reflect the agencies' current practice, and their inclusion
in the rule as specifically excluded furthers the agencies' goal of
providing greater clarity over what waters are and are not protected
under the CWA.
Role of States and Tribes Under the Clean Water Act
States and tribes play a vital role in the implementation and
enforcement of the CWA. Section 101(b) of the CWA states that it is
Congressional policy to preserve the primary responsibilities and
rights of states to prevent, reduce, and eliminate pollution, to plan
the development and use of land and water resources, and to consult
with the Administrator with respect to the exercise of the
Administrator's authority under the CWA.
Of particular importance, states and tribes may be authorized by
the EPA to administer the permitting programs of CWA sections 402 and
404. Forty-six states and the U.S. Virgin Islands are authorized to
administer the NPDES program under section 402, while two states
administer the section 404 program. The CWA identifies the waters over
which states may assume section 404 permitting jurisdiction. See CWA
section 404(g)(1). The scope of waters
[[Page 37060]]
that are subject to state and tribal permitting is a separate inquiry
and must be based on the statutory language in CWA section 404. States
administer approved CWA section 404 programs for ``waters of the United
States'' within the state, except those waters remaining under Corps
jurisdiction pursuant to CWA section 404(g)(1) as identified in a
Memorandum of Agreement between the state and the Corps. 40 CFR 233.14;
40 CFR 233.70(c)(2); 40 CFR 233.71(d)(2). EPA has initiated a separate
process to address how the EPA can best clarify assumable waters for
dredged and fill material permit programs pursuant to the Clean Water
Act section 404(g)(1). 80 FR 13539 (Mar. 16, 2015). Additional CWA
programs that utilize the definition of ``waters of the United States''
and are of importance to the states and tribes include the section 311
oil spill prevention and response program, the water quality standards
and total maximum daily load (TMDL) programs under section 303, and the
section 401 state water quality certification process.
States and federally-recognized tribes, consistent with the CWA,
retain full authority to implement their own programs to more broadly
and more fully protect the waters in their jurisdiction. Under section
510 of the CWA, unless expressly stated, nothing in the CWA precludes
or denies the right of any state to establish more protective standards
or limits than the Federal CWA. Congress has also provided roles for
eligible Indian tribes to administer CWA programs over their
reservations and expressed a preference for tribal regulation of
surface water quality on Indian reservations to ensure compliance with
the goals of the CWA. See 33 U.S.C. 1377; 56 FR 64876, 64878-79 (Dec.
12, 1991)). Tribes also have inherent sovereign authority to establish
more protective standards or limits than the Federal CWA. Where
appropriate, references to states in this document may also include
eligible tribes. Many states and tribes, for example, regulate
groundwater, and some others protect wetlands that are vital to their
environment and economy but outside the jurisdiction of the CWA.
Nothing in this rule limits or impedes any existing or future state or
tribal efforts to further protect their waters. In fact, providing
greater clarity regarding what waters are subject to CWA jurisdiction
will reduce the need for permitting authorities, including the states
and tribes with authorized section 402 and 404 CWA permitting programs,
to make jurisdictional determinations on a case-specific basis.
Overview of the Preamble
The remainder of this preamble is organized as follows. Section III
(Significant Nexus Standard) provides additional background on the
rule, including a discussion of Supreme Court precedent, the science
underpinning the rule, and the agencies' overall interpretive approach
to applying the significant nexus standard. Section IV (Definition of
Waters of the United States) explains the provisions of the final rule,
including subsections on each of the major elements of the rule.
Section V summarizes the economic analysis of the rule and Section VI
addresses Related Acts of Congress, Executive Orders and Agency
Initiatives.
III. Significant Nexus Standard
With this rule, the agencies interpret the scope of the ``waters of
the United States'' for the CWA in light of the goals, objectives, and
policies of the statute, the Supreme Court case law, the relevant and
available science, and the agencies' technical expertise and
experience. The key to the agencies' interpretation of the CWA is the
significant nexus standard, as established and refined in Supreme Court
opinions: Waters are ``waters of the United States'' if they, either
alone or in combination with similarly situated waters in the region,
significantly affect the chemical, physical, or biological integrity of
traditional navigable waters, interstate waters, or the territorial
seas. The agencies interpret specific aspects of the significant nexus
standard in light of the science, the law, and the agencies' technical
expertise: The scope of the region in which to evaluate waters when
making a significant nexus determination; the waters to evaluate in
combination with each other; and the functions provided by waters and
strength of those functions, and when such waters significantly affect
the chemical, physical, or biological integrity of the downstream
traditional navigable waters, interstate waters, or the territorial
seas.
In the rule, the agencies determine that tributaries, as defined
(``covered tributaries''), and ``adjacent waters'', as defined
(``covered adjacent waters''), have a significant nexus to downstream
traditional navigable waters, interstate waters, and the territorial
seas and therefore are ``waters of the United States.'' In the rule,
the agencies also establish that defined sets of additional waters may
be determined to have a significant nexus on a case-specific basis: (1)
Five specific types of waters that the agencies conclude are
``similarly situated'' and therefore must be analyzed ``in
combination'' in the watershed that drains to the nearest traditional
navigable water, interstate water, or the territorial seas when making
a case-specific significant nexus analysis; and (2) waters within the
100-year floodplain of a traditional navigable water, interstate water,
or the territorial seas, or waters within 4,000 feet of the high tide
line or ordinary high water mark of traditional navigable waters,
interstate waters, the territorial seas, impoundments or covered
tributaries. The rule establishes a definition of significant nexus,
based on Supreme Court opinions and the science, to use when making
these case-specific determinations.
Significant nexus is not a purely scientific determination. The
opinions of the Supreme Court have noted that as the agencies charged
with interpreting the statute, EPA and the Corps must develop the outer
bounds of the scope of the CWA, while science does not provide bright
line boundaries with respect to where ``water ends'' for purposes of
the CWA. Therefore, the agencies' interpretation of the CWA is informed
by the Science Report and the review and comments of the SAB, but not
dictated by them. With this context, this section addresses, first, the
Supreme Court case law and the significant nexus standard, second, the
relevant scientific conclusions reached by analysis of existing
scientific literature, and third, the agencies' significant nexus
determinations underpinning the rule. Section IV of the preamble
addresses in more detail the precise definitions of the covered waters
promulgated by the agencies to provide the bright line boundaries
identifying ``waters of the United States.''
A. The Significant Nexus Standard
Congress enacted the CWA ``to restore and maintain the chemical,
physical, and biological integrity of the Nation's waters.'' Section
101(a). The agencies' longstanding regulations define ``waters of the
United States'' for purposes of the Clean Water Act, and the Supreme
Court has addressed the scope of ``waters of the United States''
protected by the CWA in three cases. The significant nexus standard
evolved through those cases.
In United States v. Riverside Bayview Homes, 474 U.S. 121 (1985)
(Riverside), which involved wetlands adjacent to a traditional
navigable water in Michigan, the Court, in a unanimous opinion,
deferred to the Corps' ecological judgment that adjacent wetlands are
``inseparably bound up'' with the waters
[[Page 37061]]
to which they are adjacent, and upheld the inclusion of adjacent
wetlands in the regulatory definition of ``waters of the United
States.'' Id. at 134. The Court observed that the broad objective of
the CWA to restore and maintain the integrity of the Nation's waters
``incorporated a broad, systemic view of the goal of maintaining and
improving water quality . . .. Protection of aquatic ecosystems,
Congress recognized, demanded broad federal authority to control
pollution, for `[w]ater moves in hydrologic cycles and it is essential
that discharge of pollutants be controlled at the source.' In keeping
with these views, Congress chose to define the waters covered by the
Act broadly.'' Id. at 132-33 (citing Senate Report No. 92-414). The
Court also recognized that ``[i]n determining the limits of its power
to regulate discharges under the Act, the Corps must necessarily choose
some point at which water ends and land begins. Our common experience
tells us that this is often no easy task: The transition from water to
solid ground is not necessarily or even typically an abrupt one.
Rather, between open waters and dry land may lie shallows, marshes,
mudflats, swamps, bogs--in short, a huge array of areas that are not
wholly aquatic but nevertheless fall far short of being dry land. Where
on this continuum to find the limit of `waters' is far from obvious.''
Id. The Court then deferred to the agencies' interpretation: ``In view
of the breadth of federal regulatory authority contemplated by the Act
itself and the inherent difficulties of defining precise bounds to
regulable waters, the Corps' ecological judgment about the relationship
between waters and their adjacent wetlands provides an adequate basis
for a legal judgment that adjacent wetlands may be defined as waters
under the Act.'' Id. at 134.
The issue of CWA jurisdiction over ``waters of the United States''
was addressed again by the Supreme Court in Solid Waste Agency of
Northern Cook County v. U.S. Army Corps of Engineers, 531 U.S. 159
(2001) (SWANCC). In SWANCC, the Court (in a 5-4 opinion) held that the
use of ``isolated'' non-navigable intrastate ponds by migratory birds
was not by itself a sufficient basis for the exercise of federal
regulatory authority under the CWA. The SWANCC Court noted that in
Riverside it had ``found that Congress' concern for the protection of
water quality and aquatic ecosystems indicated its intent to regulate
wetlands `inseparably bound up' with the `waters' of the United
States'' and that ``[i]t was the significant nexus between the wetlands
and `navigable waters' that informed our reading of the CWA'' in that
case. Id. at 167. SWANCC did not invalidate any parts of the regulatory
definition of ``waters of the United States.''
Five years after SWANCC, the Court again addressed the term
``waters of the United States'' in Rapanos v. United States, 547 U.S.
715 (2006) (Rapanos). Rapanos involved two consolidated cases in which
the CWA had been applied to wetlands adjacent to non-navigable
tributaries of traditional navigable waters. All Members of the Court
agreed that the term ``waters of the United States'' encompasses some
waters that are not navigable in the traditional sense. A four-Justice
plurality in Rapanos interpreted the term ``waters of the United
States'' as covering ``relatively permanent, standing or continuously
flowing bodies of water . . .,'' id. at 739, that are connected to
traditional navigable waters, id. at 742, as well as wetlands with a
``continuous surface connection . . .'' to such water bodies, id.
(Scalia, J., plurality opinion). The Rapanos plurality noted that its
reference to ``relatively permanent'' waters did ``not necessarily
exclude streams, rivers, or lakes that might dry up in extraordinary
circumstances, such as drought,'' or ``seasonal rivers, which contain
continuous flow during some months of the year but no flow during dry
months. . . .'' Id. at 732 n.5 (emphasis in original).
Justice Kennedy concurred that the cases should be remanded for
further decision making, and stated that ``to constitute `navigable
waters' under the Act, a water or wetland must possess a `significant
nexus' to waters that are or were navigable in fact or that could
reasonably be so made.'' Id. at 759 (citing SWANCC, 531 U.S. at 167,
172). Justice Kennedy concluded that ``The required nexus must be
assessed in terms of the statute's goals and purposes. Congress enacted
the law to `restore and maintain the chemical, physical, and biological
integrity of the Nation's waters,' 33 U.S.C. 1251(a), and it pursued
that objective by restricting dumping and filling in `navigable
waters,' Sec. Sec. 1311(a), 1362(12).'' Id. at 779. He concluded that
wetlands possess the requisite significant nexus if the wetlands
``either alone or in combination with similarly situated [wet]lands in
the region, significantly affect the chemical, physical, and biological
integrity of other covered waters more readily understood as
`navigable.' '' 547 U.S. at 780. Justice Kennedy's opinion notes that
such a relationship with navigable waters must be more than
``speculative or insubstantial.'' Id. at 780.
While Justice Kennedy's opinion focused on adjacent wetlands in
light of the facts of the cases before him, his opinion is clear that a
significant nexus is the basis for jurisdiction to protect non-
navigable waters and wetlands under the CWA (id. at 759), and there is
no indication in his opinion that the analytical framework his opinion
provides for determining significant nexus for adjacent wetlands is
limited to adjacent wetlands. In addition, the four dissenting Justices
in Rapanos, who would have affirmed the court of appeals' application
of the agencies' regulation, also concluded that the term ``waters of
the United States'' encompasses, inter alia, all tributaries and
wetlands that satisfy ``either the plurality's [standard] or Justice
Kennedy's.'' Id. at 810 & n.14 (Stevens, J., dissenting). Neither the
plurality nor the Kennedy opinion invalidated any of the current
regulatory provisions defining ``waters of the United States.''
Chief Justice Roberts' concurrence in Rapanos emphasized that
``[a]gencies delegated rulemaking authority under a statute such as the
Clean Water Act are afforded generous leeway by the courts in
interpreting the statute they are entrusted to administer.'' Id. at
758. Chief Justice Roberts made clear that, if the agencies had
undertaken such a rulemaking, ``the Corps and the EPA would have
enjoyed plenty of room to operate in developing some notion of an outer
bound to the reach of their authority.'' Id. (Emphasis in original.)
The agencies utilize the significant nexus standard, as articulated
by Justice Kennedy's opinion and informed by the unanimous opinion in
Riverside Bayview and the plurality opinion in Rapanos which all
recognize that the Act and the agencies must identify the scope of CWA
jurisdiction ``on this continuum to find the limit of `waters,' ''
Riverside Bayview at 132, to interpret the scope of the statutory term
``waters of the United States.'' While a significant nexus
determination is primarily weighted in the scientific evidence and
criteria, the agencies also consider the statutory language, the
statute's goals, objectives and policies, the case law, and the
agencies' technical expertise and experience when interpreting the
terms of the CWA.
B. Science Report
EPA's Office of Research and Development prepared the Science
Report, a peer-reviewed compilation and analysis of published peer-
reviewed scientific literature summarizing the current scientific
understanding of the
[[Page 37062]]
connectivity of and mechanisms by which streams and wetlands, singly or
in combination, affect the chemical, physical, and biological integrity
of downstream waters. The final Science Report is available in the
docket and at https://cfpub.epa.gov/ncea/cfm/recordisplay.cfm?deid=296414.
The process for developing the Science Report followed standard
information quality guidelines for EPA. In September 2013, EPA released
a draft of the Science Report for an independent SAB review and invited
submissions of public comments for consideration by the SAB panel. In
October 2014, after several public meetings and hearings, the SAB
completed its peer review of the draft Science Report. The SAB was
highly supportive of the draft Science Report's conclusions regarding
streams, riparian and floodplain wetlands, and open waters, and
recommended strengthening the conclusion regarding non-floodplain
waters to include a more definitive statement that reflects how
numerous functions of such waters sustain the integrity of downstream
waters.\7\ The final peer review report is available on the SAB Web
site, as well as in the docket for this rulemaking. EPA revised the
draft Science Report based on comments from the public and
recommendations from the SAB panel.
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\7\ U.S. EPA. 2014. SAB review of the draft EPA report
Connectivity of Streams and Wetlands to Downstream Waters: A Review
and Synthesis of the Scientific Evidence. EPA-SAB-15-001, U.S.
Environmental Protection Agency, Washington, DC. (``SAB 2014a.'')
---------------------------------------------------------------------------
The SAB was established in 1978 by the Environmental Research,
Development, and Demonstration Authorization Act (ERDDAA), to provide
independent scientific and technical advice to the EPA Administrator on
the technical basis for Agency positions and regulations. Advisory
functions include peer review of EPA's technical documents, such as the
Science Report. At the time the peer review was completed, the
chartered SAB was comprised of more than 50 members from a variety of
sectors including academia, non-profit organizations, foundations,
state governments, consulting firms, and industry. To conduct the peer
review, EPA's SAB staff formed an ad hoc panel based on nominations
from the public to serve as the primary reviewers. The panel consisted
of 27 technical experts in an array of relevant fields, including
hydrology, wetland and stream ecology, biology, geomorphology,
biogeochemistry, and freshwater science. Similar to the chartered SAB,
the panel members represented sectors including academia, a federal
government agency, non-profit organizations, and consulting firms. The
chair of the panel was a member of the chartered SAB.
The SAB process is open and transparent, consistent with the
Federal Advisory Committee Act, 5 U.S.C., App 2, and agency policies
regarding Federal advisory committees. Consequently, the SAB has an
approved charter, which must be renewed biennially, announces its
meetings in the Federal Register, and provides opportunities for public
comment on issues before the Board. The SAB staff announced via the
Federal Register that they sought public nominations of technical
experts to serve on the expert panel: SAB Panel for the Review of the
EPA Water Body Connectivity Report (via a similar process the public
also is invited to nominate chartered SAB members). 78 FR 15012 (Mar.
8, 2013). The SAB staff then invited the public to comment on the list
of candidates for the panel. Once the panel was selected, the SAB staff
posted a memo on its Web site addressing the formation of the panel and
the set of determinations that were necessary for its formation (e.g.,
no conflicts of interest). In the public notice of the first public
meetings interested members of the public were invited to submit
relevant comments for the SAB Panel to consider pertaining to the
review materials, including the charge to the Panel. Over 133,000
public comments were received by the Docket. Every meeting was open to
the public, noticed in the Federal Register, and had time allotted for
the public to present their views. In total, the Panel held a two-day
in-person meeting in Washington, DC, in December 2013, and three four-
hour public teleconferences in April, May, and June 2014. The SAB Panel
also compiled four draft versions of its peer review report to inform
and assist the meeting deliberations that were posted on the SAB Web
site. In September 2014, the chartered SAB conducted a public
teleconference to conduct the quality review of the Panel's final draft
peer review report. The peer review report was approved at that
meeting, and revisions were made to reflect the chartered SAB's review.
The culmination of that public process was the release of the final
peer review report in October 2014. All meeting minutes and draft
reports are available on the SAB Web site for public access.
The final Science Report states that connectivity is a foundational
concept in hydrology and freshwater ecology. Connectivity is the degree
to which components of a system are joined, or connected, by various
transport mechanisms and is determined by the characteristics of both
the physical landscape and the biota of the specific system.
Connectivity for purposes of interpreting the scope of ``waters of the
United States'' under the CWA serves to demonstrate the ``nexus''
between upstream water bodies and the downstream traditional navigable
water, interstate water, or the territorial sea. The scientific
literature does not use the term ``significant'' as it is defined in a
legal context, but it does provide information on the strength of the
effects on the chemical, physical, and biological functioning of the
downstream water bodies from the connections among covered tributaries,
covered adjacent waters, and case-specific waters and those downstream
waters. The scientific literature also does not use the terms
traditional navigable waters, interstate waters, or the territorial
seas. However, evidence of strong chemical, physical, and biological
connections to larger rivers, estuaries, and lakes applies to that
subset of rivers, estuaries, and lakes that are traditional navigable
waters, interstate waters, or the territorial seas.
The Science Report presents evidence of those connections from
various categories of waters, evaluated singly or in combination, which
affect downstream waters and the strength of that effect. The
objectives of the Science Report are (1) to provide a context for
considering the evidence of connections between downstream waters and
their tributary waters, and (2) to summarize current understanding
about these connections, the factors that influence them, and the
mechanisms by which the connections affect the function or condition of
downstream waters. The connections and mechanisms discussed in the
Science Report include transport of physical materials and chemicals
such as water, wood, sediment, nutrients, pesticides, and mercury;
functions that covered adjacent waters perform, such as storing and
cleansing water; movement of organisms or their seeds and eggs; and
hydrologic and biogeochemical interactions occurring in and among
surface and groundwater flows, including hyporheic zones \8\ and
alluvial aquifers.
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\8\ The hyporheic zone is the subsurface area immediately below
the bed of intermittent and ephemeral streams that remains wet even
when there is no surface flow. These areas are extremely important
to macro-benthic organisms critical to the bio-chemical integrity of
streams.
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The Science Report presents five major conclusions:
[[Page 37063]]
Conclusion 1: Streams
The scientific literature unequivocally demonstrates that streams,
individually or cumulatively, exert a strong influence on the chemical,
physical, and biological integrity of downstream waters. All tributary
streams, including perennial, intermittent, and ephemeral streams, are
chemically, physically, and biologically connected to downstream rivers
via channels and associated alluvial deposits where water and other
materials are concentrated, mixed, transformed, and transported.
Streams are the dominant source of water in most rivers, and the
majority of tributaries are perennial, intermittent, or ephemeral
headwater streams. Headwater streams also convey water into local
storage compartments such as ponds, shallow aquifers, and floodplains,
and into regional and alluvial aquifers; these local storage
compartments are important sources of water for maintaining baseflow in
rivers. In addition to water, streams transport sediment, wood, organic
matter, nutrients, chemical contaminants, and many of the organisms
found in rivers. The scientific literature provides robust evidence
that streams are biologically connected to downstream waters by the
dispersal and migration of aquatic and semiaquatic organisms, including
fish, amphibians, plants, microorganisms, and invertebrates, that use
both upstream and downstream habitats during one or more stages of
their life cycles, or provide food resources to downstream communities.
In addition to material transport and biological connectivity,
ephemeral, intermittent, and perennial flows influence fundamental
biogeochemical processes by connecting channels and shallow groundwater
with other landscape elements. Chemical, physical, and biological
connections between streams and downstream waters interact via
integrative processes such as nutrient spiraling. This occurs when
stream communities assimilate and chemically transform large quantities
of nitrogen and other nutrients that otherwise would be transported
directly downstream, thereby increasing nutrient loads and associated
impairments due to excess nutrients in downstream waters. Science
Report at ES-2.
Conclusion 2: Riparian/Floodplain Wetlands and Open Waters
The scientific literature clearly shows that wetlands and open
waters in riparian areas and floodplains are chemically, physically,
and biologically integrated with rivers via functions that improve
downstream water quality, including the temporary storage and
deposition of channel-forming sediment and woody debris, temporary
storage of local groundwater that supports baseflow in rivers, and
transformation and transport of stored organic matter. Riparian/
floodplain wetlands and open waters improve water quality through the
assimilation, transformation, and sequestration of pollutants,
including excess nutrients and chemical contaminants such as pesticides
and metals that can degrade downstream water integrity. In addition to
providing effective buffers to protect downstream waters from point
source and nonpoint source pollution, these systems form integral
components of river food webs, providing nursery habitat for breeding
fish and amphibians, colonization opportunities for stream
invertebrates, and maturation habitat for stream insects. Lateral
expansion and contraction of the river in its floodplain result in an
exchange of organic matter and organisms, including fish populations
that are adapted to use floodplain habitats for feeding and spawning
during high water, that are critical to river ecosystem function.
Riparian/floodplain wetlands and open waters also affect the integrity
of downstream waters by subsequently releasing (desynchronizing)
floodwaters and retaining large volumes of stormwater, sediment, and
contaminants in runoff that could otherwise negatively affect the
condition or function of downstream waters. Science Report at ES-2 to
ES-3.
Conclusion 3: Non-Floodplain Wetlands and Open Waters
Wetlands and open waters in non-floodplain landscape settings
(``non-floodplain wetlands'') provide numerous functions that benefit
downstream water integrity. These functions include storage of
floodwater; recharge of groundwater that sustains river baseflow;
retention and transformation of nutrients, metals, and pesticides;
export of organisms or seeds to downstream waters; and habitats needed
for stream species. This diverse group of wetlands (e.g., many Prairie
potholes or vernal pools) can be connected to downstream waters through
surface water, shallow subsurface water, and groundwater flows, and
through biological and chemical connections.
In general, connectivity of non-floodplain wetlands occurs along a
gradient, and can be described in terms of the frequency, duration,
magnitude, timing, and rate of change of water, material, and biotic
fluxes to downstream waters. These descriptors are influenced by
climate, geology, and terrain, which interact with factors such as the
magnitudes of the various functions within wetlands (e.g., amount of
water storage or carbon export) and their proximity to downstream
waters to determine where wetlands occur along the connectivity
gradient. At one end of this gradient, the functions of non-floodplain
wetlands clearly affect the condition of downstream waters if a visible
(e.g., channelized) surface water or a regular shallow subsurface-water
connection to the river network is present. For non-floodplain wetlands
lacking a channelized surface or regular shallow subsurface connection
(i.e., those at intermediate points along the gradient of
connectivity), generalizations about their specific effects on
downstream waters from the available literature are difficult because
information on both function and connectivity is needed. Science Report
at ES-3.
Conclusion 4: Degrees and Determinants of Connectivity
Connectivity of streams and wetlands to downstream waters occurs
along a gradient that can be described in terms of the frequency,
duration, magnitude, timing, and rate of change of water, material, and
biotic fluxes to downstream waters. These terms, which we refer to
collectively as connectivity descriptors, characterize the range over
which streams and wetlands vary and shift along the connectivity
gradient in response to changes in natural and anthropogenic factors
and, when considered in a watershed context, can be used to predict
probable effects of different degrees of connectivity over time. The
evidence unequivocally demonstrates that the stream channels and
riparian/floodplain wetlands or open waters that together form river
networks are clearly connected to downstream waters in ways that
profoundly influence downstream water integrity. The connectivity and
effects of non-floodplain wetlands and open waters are more variable
and thus more difficult to address solely from evidence available in
peer-reviewed studies. Science Report at ES-3 to ES-4.
Conclusion 5: Cumulative Effects
The incremental effects of individual streams and wetlands are
cumulative across entire watersheds, and therefore, must be evaluated
in context with other streams and wetlands. Downstream waters are the
time-integrated result of all waters contributing to them. For example,
the amount of water or biomass contributed by a specific
[[Page 37064]]
ephemeral stream in a given year might be small, but the aggregate
contribution of that stream over multiple years, or by all ephemeral
streams draining that watershed in a given year or over multiple years,
can have substantial consequences on the integrity of the downstream
waters. Similarly, the downstream effect of a single event, such as
pollutant discharge into a single stream or wetland, might be
negligible but the cumulative effect of multiple discharges could
degrade the integrity of downstream waters.
When considering the effect of an individual stream or wetland, all
contributions and functions of that stream or wetland should be
evaluated cumulatively. For example, the same stream transports water,
removes excess nutrients, transports pollutants, mitigates flooding,
and provides refuge for fish when conditions downstream are
unfavorable; if any of these functions is ignored, the overall effect
of that stream would be underestimated. Science Report at ES-5 to ES-6.
SAB Review of the Proposed Rule
In addition to its peer review of the draft Science Report, in a
separate effort the SAB also reviewed the adequacy of the scientific
and technical basis of the proposed rule and provided its advice and
comments on the proposal in September 2014.\9\ The same SAB Panel that
reviewed the draft Science Report met via two public teleconferences in
August 2014 to discuss the scientific and technical basis of the
proposed rule. The Panel submitted comments to the Chair of the
chartered SAB. A work group of chartered SAB members considered
comments provided by panel members, agency representatives, and the
public on the adequacy of the science informing the rule. This work
group then led the September 2014 public teleconference discussion of
the chartered SAB. The public had an opportunity to submit oral or
written comments during these two public meetings. The SAB's final
letter to the EPA Administrator can be found on the SAB Web site and in
the docket for this rule.
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\9\ U.S. EPA. 2014. SAB Consideration of the Adequacy of the
Scientific and Technical Basis of the EPA's Proposed Rule titled
``Definition of Waters of the United States under the Clean Water
Act.'' EPA-SAB-14-007, U.S. Environmental Protection Agency,
Washington, DC. (``SAB 2014b.'')
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The SAB found that the available science provides an adequate
scientific basis for the key components of the proposed rule. The SAB
noted that although water bodies differ in degree of connectivity that
affects the extent of influence they exert on downstream waters (i.e.,
they exist on a ``connectivity gradient''), the available science
supports the conclusion that the types of water bodies identified as
``waters of the United States'' in the proposed rule exert strong
influence on the chemical, physical, and biological integrity of
downstream waters. In particular, the SAB expressed support for the
proposed rule's inclusion of tributaries and ``adjacent waters'' as
categorical waters of the United States and the inclusion of ``other
waters'' on a case-specific basis, though noting that certain ``other
waters'' can be determined as a subcategory to be similarly situated.
Regarding tributaries, the SAB found, ``[t]here is strong
scientific evidence to support the EPA's proposal to include all
tributaries within the jurisdiction of the Clean Water Act.
Tributaries, as a group, exert strong influence on the physical,
chemical, and biological integrity of downstream waters, even though
the degree of connectivity is a function of variation in the frequency,
duration, magnitude, predictability, and consequences of physical,
chemical, and biological processes.'' The Board advised EPA to
reconsider the definition of tributaries because not all tributaries
have ordinary high water marks (e.g., ephemeral streams with arid and
semi-arid environments or in low gradient landscapes where the flow of
water is unlikely to cause an ordinary high water mark). The SAB also
advised EPA to consider changing the wording in the definition to
``bed, bank, and other evidence of flow.'' SAB 2014b at 2. The agencies
did not make this change because this recommendation seemed to suggest
that any hydrologic connection is sufficient for CWA jurisdiction. The
definition of ``tributary'' in the rule better identifies tributaries
that have a significant nexus to downstream traditional navigable
waters, interstate waters, or the territorial seas. In addition, the
SAB suggested that EPA reconsider whether flow-through lentic systems
should be included as ``adjacent waters'' and wetlands, rather than as
tributaries.
Regarding ``adjacent waters'' and wetlands, the SAB stated, ``[t]he
available science supports the EPA's proposal to include ``adjacent
waters'' and wetlands as a waters of the United States. . . . because
[they] have a strong influence on the physical, chemical, and
biological integrity of navigable waters.'' Id. In particular, the SAB
noted, ``the available science supports defining adjacency or
determination of adjacency on the basis of functional relationships,''
rather than ``solely on the basis of geographical proximity or distance
to jurisdictional waters.'' Id. at 2-3. The agencies have determined
which waters are adjacent, and thus jurisdictional under the rule,
based on both functional relationships and proximity because those
factors identify the waters that have a strong influence on the
chemical, physical, or biological integrity of traditional navigable
waters, interstate waters, or the territorial seas. Section C. and IV.F
below. The agencies' determination is informed by the science, and
consideration of proximity is reasonable in interpreting the scope of
adjacency.
In the evaluation of ``other waters,'' the SAB found that
``scientific literature has established that `other waters' can
influence downstream waters, particularly when considered in
aggregate.'' Id. at 3. The SAB thus found it ``appropriate to define
`other waters' as waters of the United States on a case-by-case basis,
either alone or in combination with similarly situated waters in the
same region.'' Id. The SAB found that distance could not be the sole
indicator used to evaluate the connection of ``other waters'' to
jurisdictional waters. The agencies' identification of the areas within
which a water is assessed on a case-specific basis for a significant
nexus is informed by the science and the agencies' experience and
technical expertise, and consideration of proximity is reasonable in
interpreting the scope of the statute. The SAB also expressed support
for language in one of the options discussed in the preamble to the
proposed rule. Specifically, the SAB stated there is ``also adequate
scientific evidence to support a determination that certain
subcategories and types of `other waters' in particular regions of the
United States (e.g., Carolina and Delmarva Bays, Texas coastal prairie
wetlands, prairie potholes, pocosins, western vernal pools) are
similarly situated (i.e., they have a similar influence on the
chemical, physical, and biological integrity of downstream waters and
are similarly situated on the landscape) and thus could be considered
waters of the United States.'' Id. The Board noted that other sets of
wetlands could be identified as ``similarly situated'' as the science
continues to develop and that science does not support excluding groups
of ``other waters'' or subcategories thereof from jurisdiction.
The exclusions paragraph of the proposed rule generated the most
comments from the SAB. The SAB noted, ``[t]he Clean Water Act
exclusions of groundwater and certain other exclusions listed in the
proposed rule and the current regulation do not
[[Page 37065]]
have scientific justification.'' Id. With regard to ditches, the Board
found that there is a lack of scientific knowledge to determine whether
ditches should be categorically excluded. For example, some ditches
that would be excluded in the Midwest may drain Cowardin wetlands and
may provide certain ecosystem services, while gullies, rills, and non-
wetland swales can be important conduits for moving water between
jurisdictional waters. The SAB also noted that artificial lakes or
ponds, or reflection pools, can be directly connected to jurisdictional
waters via either shallow or deep groundwater. The SAB also recommended
that the agencies clarify in the preamble to the final rule that
``significant nexus'' is a legal term, not a scientific one.
C. Significant Nexus Conclusions
As noted earlier, the agencies interpret the scope of ``waters of
the United States'' protected under the CWA based on the information
and conclusions in the Science Report, other relevant scientific
literature, the Technical Support Document that provides additional
legal and scientific discussion for issues raised in this rule, the
relevant Supreme Court decisions, the agencies' technical expertise and
experience, and the objectives and requirements of the CWA. In light of
this information, the agencies made scientifically and technically
informed judgments about the nexus between the relevant waters and the
significance of that nexus and conclude that ``tributaries'' and
``adjacent waters,'' each as defined by the rule, have a significant
nexus such that they are ``waters of the United States'' and no
additional analysis is required. The agencies also determined that
additional waters may, on a case-specific basis, have a significant
nexus to traditional navigable waters, interstate waters, and the
territorial seas, either alone or in combination with similarly
situated waters. The agencies' interpretation of the scope of ``waters
of the United States'' is informed by the Science Report and the review
and comments of the SAB. The rule reflects the judgment of the agencies
in balancing the science, the agencies' expertise, and the regulatory
goals of providing clarity to the public while protecting the
environment and public health, consistent with the law.
Since the Rapanos decision, the agencies have gained extensive
experience making significant nexus determinations, and that experience
and expertise has informed the judgment of the agencies as reflected in
the provisions of the rule. The agencies, most often the Corps, have
made more than 400,000 CWA jurisdictional determinations since 2008. Of
those, more than 120,000 are case-specific significant nexus
determinations. The agencies made determinations in every state in the
country, from the arid West to the tropics of Hawaii, from the
Appalachian Mountains in the East to the lush forests of the Northwest.
With field staff located in 38 Corps District offices and 10 EPA
regional offices, the agencies have almost a decade of nationwide
experience in making significant nexus determinations. These individual
jurisdictional determinations have been made for waters ranging from an
intermittent stream that provides flow to a drinking water source, to a
group of floodplain wetlands in North Dakota that provide important
protection from floodwaters to downstream communities alongside the Red
River, to headwater mountain streams that provide high quality water
that supplies baseflow and reduces the harmful concentrations of
pollutants in the main part of the river below. Through this
experience, the agencies developed wide-ranging technical expertise in
assessing the hydrologic flowpaths along which water and materials are
transported and transformed that determine the degree of chemical,
physical, or biological connectivity, as well as the variations in
climate, geology, and terrain within and among watersheds and over time
that affect the functions (such as the removal or transformation of
pollutants) performed by streams and wetlands for downstream
traditional navigable waters, interstate waters or the territorial
seas.
The agencies utilize many tools and many sources of information to
help make jurisdictional determinations, including U.S. Geological
Survey (USGS) and state and local topographic maps, aerial photography,
soil surveys, watershed studies, scientific literature and references,
and field work. For example, USGS and state and local stream maps and
datasets, aerial photography, gage data, watershed assessments,
monitoring data, and field observations are often used to help assess
the contributions of flow of tributary streams, including intermittent
and ephemeral streams, to downstream traditional navigable waters,
interstate waters or the territorial seas. Similarly, floodplain and
topographic maps of federal, state and local agencies, modeling tools,
and field observations can be used to assess how wetlands are trapping
floodwaters that might otherwise affect downstream waters. Further, the
agencies utilize the large body of scientific literature regarding the
functions of tributaries, including tributaries with ephemeral,
intermittent and perennial flow and of wetlands and open waters to
inform their evaluations of significant nexus. In addition, the
agencies have experience and expertise for decades prior to and since
the SWANCC and Rapanos decisions with making jurisdictional
determinations, and consider hydrology, ordinary high water mark,
biota, and other technical factors in implementing Clean Water Act
programs. This immersion in the science along with the practical
expertise developed through case-specific determinations across the
country and in diverse settings is reflected in the agencies'
conclusions with respect to waters that have a significant nexus, as
well as where the agencies have drawn boundaries demarking where
``waters of the United States'' end.
1. Scope of Significant Nexus Analysis
Under the significant nexus standard, waters possess the requisite
significant nexus if they ``either alone or in combination with
similarly situated [wet]lands in the region, significantly affect the
chemical, physical, and biological integrity of other covered waters
more readily understood as `navigable.' '' Rapanos at 780. Several
terms in this standard were not defined. In this rule the agencies
interpret these terms and the scope of ``waters of the United States''
based on the goals, objectives, and policies of the statute, the
scientific literature, the Supreme Court opinions, and the agencies'
technical expertise and experience. Therefore, for purposes of a
significant nexus analysis, the agencies have determined (1) which
waters are ``similarly situated,'' and thus should be analyzed in
combination, in (2) the ``region,'' for purposes of a significant nexus
analysis, and (3) the types of functions that should be analyzed to
determine if waters significantly affect the chemical, physical, or
biological integrity of traditional navigable waters, interstate
waters, or the territorial seas. These determinations underpin many of
the key elements of the rule and are reflected in the definition of
``significant nexus'' in the rule.
a. Similarly Situated Waters
As reflected in the rule's definition of ``significant nexus,'' the
agencies determined that it is reasonable to consider waters as
``similarly situated'' where they function alike and are sufficiently
close to function together in affecting the nearest traditional
[[Page 37066]]
navigable water, interstate water, or the territorial sea. Since the
focus of the significant nexus standard is on protecting and restoring
the chemical, physical, and biological integrity of the nation's
waters, the agencies interpret the phrase ``similarly situated'' in
terms of whether particular waters are providing common, or similar,
functions for downstream waters such that it is reasonable to consider
their effect together. Regarding covered tributaries and covered
adjacent waters, the agencies define each water type such that the
functions provided are similar and the waters are situated so as to
provide those functions together to affect downstream waters.
The science demonstrates that covered tributaries provide many
common vital functions important to the chemical, physical, and
biological integrity of downstream waters, regardless of the size of
the tributaries. The science also supports the conclusion that
sufficient volume, duration, and frequency of flow are required to
create a bed and banks and ordinary high water mark. The science also
supports the conclusion that tributaries function together to affect
downstream waters. The agencies conclude that covered tributaries with
a bed and banks and ordinary high water mark are similarly situated for
purposes of the agencies' significant nexus analysis.
For covered adjacent waters, the science demonstrates that these
waters provide many similar vital functions to downstream waters, and
the agencies defined ``adjacent waters'' with distance boundaries to
ensure that the waters are providing similar functions to downstream
waters and that the waters are located comparably in the region such
that the agencies' reasonably judged them to be similarly situated.
For waters for which a case-specific significant nexus
determination is required the agencies have determined that some waters
in specific regions are similarly situated; for other specified waters,
the determination of whether there are any other waters providing
similar functions in a similar situation in the region must be made as
part of a case-specific determination. See section IV.H.
Assessing the functions of identified waters in combination is
consistent not only with Justice Kennedy's significant nexus standard,
but with the science. Scientists routinely combine the effects of
groups of waters, aggregating the known effect of one water with those
of ecologically similar waters in a specific geographic area, or to a
certain scale. This is because the chemical, physical, and biological
integrity of downstream waters is directly related to the aggregate
contribution of upstream waters that flow into them, including any
tributaries and connected wetlands. As a result, the scientific
literature and the Science Report consistently document that the health
of larger downstream waters is directly related to the aggregate health
of waters located upstream, including waters such as wetlands that may
not be hydrologically connected but function together to ameliorate the
potential impacts of flooding and pollutant contamination from
affecting downstream waters. See Technical Support Document.
For example, excess nutrients discharged into small tributary
streams in the aggregate can cause algal blooms downstream that reduce
dissolved oxygen levels and increase turbidity in traditional navigable
waters, interstate waters, and the territorial seas. Water low in
dissolved oxygen cannot support aquatic life. This widely-recognized
phenomenon, known as hypoxia, has impacted commercial and recreational
fisheries in the northern Gulf of Mexico. In this instance, the
cumulative effects of nutrient export from the many small headwater
streams of the Mississippi River have resulted in large-scale
ecological and economically harmful impacts hundreds of miles
downstream. See Technical Support Document.
In review of the scientific and technical adequacy of the rule, the
SAB panel members ``generally agreed that aggregating `similarly
situated' waters is scientifically justified, given that the combined
effects of these waters on downstream waters are often only measurable
in aggregate.'' \10\ As stated in section III.B. above, one of the main
conclusions of the Science Report is that the incremental contributions
of individual streams and wetlands are cumulative across entire
watersheds, and their effects on downstream waters should be evaluated
within the context of other streams and wetlands in that watershed. For
example, the Science Report finds, ``[t]he amount of nutrients removed
by any one stream over multiple years or by all headwater streams in a
watershed in a given year can have substantial consequences for
downstream waters.'' Science Report at 1-11. Cumulative effects of
streams, wetlands, and open waters across a watershed must be
considered because ``[t]he downstream consequences (e.g., the amount
and quality of materials that eventually reach a river) are determined
by the aggregate effect of contributions and sequential alterations
that begin at the source waters and function along continuous flowpaths
to the watershed outlet.'' Id. at 1-19.
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\10\ September 2, 2014. Memorandum from Dr. Amanda Rodewald to
Dr. David Allen. Comments to the chartered SAB on the Adequacy of
the Scientific and Technical Basis of the EPA's Proposed Rule titled
``Definition of `Waters of the United States' under the Clean Water
Act.'' (``SAB 2014c.'')
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The agencies conclude that it is appropriate to assess the effects
of waters in combination based on the similarity of the functions they
provide to the downstream water and their location in the watershed.
This is consistent with the science and effectively meets the goals of
the CWA.
b. In the Region
Since Justice Kennedy did not define the ``region,'' the agencies
determined that the single point of entry watershed is a reasonable and
technically appropriate scale for identifying ``in the region'' for
purposes of the significant nexus standard. A single point of entry
watershed is the drainage basin within whose boundaries all
precipitation ultimately flows to the nearest single traditional
navigable water, interstate water, or the territorial sea. The agencies
determined that because the movement of water from watershed drainage
basins to coastal waters, river networks, and lakes shapes the
development and function of these systems in a way that is critical to
their long-term health, the watershed is a reasonable and technically
appropriate way to identify the scope of waters that together may have
an effect on the chemical, physical, or biological integrity of a
particular traditional navigable water, interstate water, or
territorial sea. The watershed includes all streams, wetlands, lakes,
and open waters within its boundaries. Using the watershed that flows
to the nearest single traditional navigable water, interstate water, or
territorial sea is consistent with court decisions that these waters
are the ultimate focus of CWA protections. Using the single point of
entry watershed ensures that any analysis of significant nexus is
appropriately connected to these touchstone waters.
Because the movement of water from watershed drainage basins to
coastal waters, river networks, and lakes shapes the development and
function of these systems in a way that is critical to their integrity,
using a watershed as the framework for conducting significant nexus
evaluations is scientifically supportable. Watersheds are generally
regarded as the most appropriate spatial unit for water resource
management. Anthropogenic actions and natural events can have
widespread effects within the watershed that collectively
[[Page 37067]]
impact the integrity and quality of the relevant traditional navigable
water, interstate water, or the territorial sea. The functions of the
contributing waters are inextricably linked and have a cumulative
effect on the integrity of the downstream traditional navigable water,
interstate water, or the territorial sea. For these reasons, it is more
appropriate to conduct a significant nexus analysis at the watershed
scale than to focus on a specific site, such as an individual stream
segment. See proposal Appendix A, Scientific Analysis, 79 FR 22246,
April 21, 2014, Science Report, and Technical Support Document.
Concluding that the watershed is the reasonable and appropriate
region for purposes of a significant nexus analysis is also consistent
with the agencies' longstanding practice and experience. To restore or
maintain the health of the downstream affected water, the agencies'
standard practice is to evaluate the condition of the waters that are
in the contributing watersheds and to develop a plan to address the
issues of concern. The Corps has used watershed framework approaches
for water sources, for navigation approaches for more than 100 years,
and in the regulatory program since its inception. Also, using a
watershed framework is consistent with more than two decades of
practice by EPA and many other governmental, academic, and additional
entities that recognize that a watershed approach is the most effective
framework to address water resource challenges. Finally, the watershed
that drains to the nearest (i.e., first downstream) traditional
navigable water, interstate water, or the territorial seas is likely to
be of a size commonly understood as a ``region.''
In light of the scientific literature, the longstanding approach of
the agencies' implementation of the CWA, and the statutory goals
underpinning Justice Kennedy's significant nexus framework, the
watershed draining to the nearest traditional navigable water,
interstate water, or the territorial sea, is the appropriate ``region''
for a significant nexus analysis. See the proposed rule preamble and
Technical Support Document.
c. Significantly Affect Chemical, Physical, or Biological Integrity
The agencies' definition of the term ``significant nexus'' in the
rule is consistent with language in Riverside Bayview, SWANCC, and
Rapanos, and with the goals, objectives, and policies of the CWA. The
definition reflects that not all waters have a requisite connection to
traditional navigable waters, interstate waters, or the territorial
seas sufficient to be determined jurisdictional. Justice Kennedy was
clear that to be covered, waters must significantly affect the
chemical, physical, or biological integrity of a downstream navigable
water and that the requisite nexus must be more than ``speculative or
insubstantial,'' Rapanos, at 780. The agencies define significant nexus
in precisely those terms. Under the rule a ``significant nexus'' is
established by a showing of a significant chemical, physical, or
biological effect. In characterizing the significant nexus standard,
Justice Kennedy stated: ``[t]he required nexus must be assessed in
terms of the statute's goals and purposes. Congress enacted the [CWA]
to `restore and maintain the chemical, physical, and biological
integrity of the Nation's waters'. . . .'' 547 U.S. at 779. It is clear
that Congress intended the CWA to ``restore and maintain'' all three
forms of ``integrity,'' Section 101(a), so if any one is compromised
then that is contrary to the statute's stated objective. It would
subvert the objective if the CWA only protected waters upon a showing
that they had effects on every attribute of the integrity of a
traditional navigable water, interstate water, or the territorial sea.
In the rule's definition of ``significant nexus,'' the agencies
identify the functions that waters provide that can significantly
affect the chemical, physical, or biological integrity of traditional
navigable waters, interstate waters and the territorial seas. In
identifying the functions to be considered the agencies were informed
by the goals of the statute and the available science. Among the means
to achieve the CWA's objective to restore and maintain the chemical,
physical, and biological integrity of the Nation's waters, Congress
established an interim national goal to achieve wherever possible
``water quality which provides for the protection and propagation of
fish, shellfish, and wildlife and provides for recreation in and on the
water.'' Section 101(a)(2). Functions to be considered for the purposes
of determining significant nexus are sediment trapping; nutrient
recycling; pollutant trapping, transformation, filtering, and
transport; retention and attenuation of floodwaters; runoff storage;
contribution of flow; export of organic matter; export of food
resources; and provision of life-cycle dependent aquatic habitat (such
as foraging, feeding, nesting, breeding, spawning, and use as a nursery
area) for species located in traditional navigable waters, interstate
waters, or the territorial seas. The effect of an upstream water can be
significant even when a water, alone or in combination, is providing a
subset, or even just one, of the functions listed.
Science demonstrates that these aquatic functions provided by
smaller streams, ponds, wetlands and other waters are important for
protecting the chemical, physical, and biological integrity of
downstream traditional navigable waters, interstate waters, and the
territorial seas. For example, States identify sediment and nutrients
as the primary contaminants in the nation's waters. Sediment storage
and export via streams to downstream waters is critical for maintaining
the river network, including the formation of channel features.
Although sediment is essential to river systems, excess sediment can
impair ecological integrity by filling interstitial spaces, reducing
channel capacity, blocking sunlight transmission through the water
column, and increasing contaminant and nutrient concentrations. Streams
and wetlands can prevent excess deposits of sediment downstream and
reduce pollutant concentrations in downstream waters. Thus the function
of trapping of excess sediment, along with export of sediment, have a
significant effect on the chemical, physical, and biological integrity
of downstream waters.
Nutrient recycling results in the uptake and transformation of
large quantities of nitrogen and other nutrients that otherwise would
be transported directly downstream, thereby decreasing nutrient loads
and associated impairments due to excess nutrients in downstream
waters. Streams, wetlands and open waters improve water quality through
the assimilation, transformation, or sequestration of pollutants,
including excess nutrients and chemical contaminants such as pesticides
and metals that can degrade downstream water integrity. Nutrient
transport exports nutrients downstream and can degrade water quality
and lead to stream impairments. Nutrients are necessary to support
aquatic life, but excess nutrients lead to excessive plant growth and
hypoxia, in which over-enrichment causes dissolved oxygen
concentrations to fall below the level necessary to sustain most
aquatic animal life in the downstream waters. Nutrient recycling,
retention, and export can significantly affect downstream chemical
integrity by impacting downstream water quality.
The contribution of flow downstream is an important role, as
upstream waters can be a cumulative source of the majority of the total
mean annual flow to bigger downstream rivers and waters, including via
the recharge of baseflow.
[[Page 37068]]
Streams, wetlands, and open waters contribute surface and subsurface
water downstream, and are the dominant sources of water in most rivers.
Contribution of flow can significantly affect the physical integrity of
downstream waters, helping to sustain the volume of water in larger
waters.
Small streams and wetlands are particularly effective at retaining
and attenuating floodwaters. By subsequently releasing
(desynchronizing) floodwaters and retaining large volumes of stormwater
that could otherwise negatively affect the condition or function of
downstream waters, streams and adjacent wetlands and open waters affect
the physical integrity of downstream traditional navigable waters,
interstate waters, or the territorial seas. This function can reduce
flood peaks downstream and can also maintain downstream river baseflows
by recharging alluvial aquifers.
Streams, wetlands, and open waters supply downstream waters with
dissolved and particulate organic matter (e.g., leaves, wood), which
support biological activity throughout the river network. In addition
to organic matter, streams, wetlands, and open waters can also export
other food resources downstream, such as aquatic insects that are the
food source for fish in downstream waters. The export of organic matter
and food resources downstream is important to maintaining the food webs
and thus the biological integrity of traditional navigable waters,
interstate waters, and the territorial seas.
Streams, wetlands, and open waters provide life-cycle dependent
aquatic habitat (such as foraging, feeding, nesting, breeding,
spawning, and use as a nursery area) for species located in traditional
navigable waters, interstate waters, or the territorial seas. Many
species require different habitats for different resources (e.g., food,
spawning habitat, overwintering habitat), and thus move throughout the
river network over their life-cycles. For example, headwater streams
can provide refuge habitat under adverse conditions, enabling fish to
persist and recolonize downstream areas once conditions have improved.
These upstream systems form integral components of downstream food
webs, providing nursery habitat for breeding fish and amphibians,
colonization opportunities for stream invertebrates, and maturation
habitat for stream insects, including for species that are critical to
downstream ecosystem function. The provision of life-cycle dependent
aquatic habitat for species located in downstream waters significantly
affects the biological integrity of those downstream waters.
Tributaries, adjacent wetlands, and open waters can perform
multiple functions, including functions that change depending upon the
season. For example, the same stream can contribute flow when
evapotranspiration is low and can retain water when evapotranspiration
is high. These functions, particularly when considered in aggregate
with the functions of similarly situated waters in the region, can
significantly affect the chemical, physical, or biological integrity of
a traditional navigable water, interstate water, or the territorial
seas. When considering the effect of an individual stream, wetland, or
open water, all contributions and functions that the water provides
should be evaluated cumulatively. For example, the same wetland retains
sediment, removes excess nutrients, mitigates flooding, and provides
habitat for amphibians that also live downstream; if any of these
functions is ignored, the overall effect of that wetland would be
underestimated. It is important to note, however, that a water or
wetland can provide just one function that may significantly affect the
chemical, physical or biological integrity of the downstream water.
2. Categories of Waters Determined to Have a Significant Nexus
In this rule, the agencies determine that: (1) Covered tributaries,
in combination with other covered tributaries located in a watershed
that drains to a traditional navigable water, interstate water, or the
territorial seas, significantly affect the chemical, physical, and
biological integrity of that water; and (2) covered adjacent waters, in
combination with other covered adjacent waters located in a watershed
that drains to a traditional navigable water, interstate water, or the
territorial seas, significantly affect the chemical, physical, and
biological integrity of that water.
a. Covered Tributaries
The agencies determine based on their scientific and technical
expertise that waters meeting the definition of ``tributary'' in a
single point of entry watershed are similarly situated and have a
significant nexus because they significantly affect the chemical,
physical, or biological integrity of traditional navigable waters,
interstate waters, and the territorial seas. As such, it is appropriate
to conclude covered tributaries as a category are ``waters of the
United States.'' See Technical Support Document. The agencies limited
the tributaries that are ``waters of the United States'' to those that
have both a bed and banks and another indicator of ordinary high water
mark. That limitation served as a reasonable basis to consider covered
tributaries similarly situated because those physical characteristics
indicated sufficient flow that the covered tributaries are performing
similar functions and located such that they are working together in
the region to provide those functions to the nearest traditional
navigable water, interstate water, or the territorial seas. Justice
Kennedy noted that the requirement of a perceptible ordinary high water
mark for tributaries, a measure that had been used by the Corps, ``may
well provide a reasonable measure of whether specific minor tributaries
bear a sufficient nexus with other regulated waters to constitute
`navigable waters' under the Act.'' 547 U.S. at 781, see also id. at
761. The science supports this.
The agencies analyzed the Science Report and other scientific
literature to determine whether tributaries to traditional navigable
waters, interstate waters, or the territorial seas have a significant
nexus to constitute ``waters of the United States'' under the Act such
that it is reasonable to assert CWA jurisdiction over all such
tributaries by rule. Covered tributaries have a significant impact on
the chemical, physical, or biological integrity of waters into which
they eventually flow--for CWA purposes, traditional navigable waters,
interstate waters, and the territorial seas. The great majority of
covered tributaries are headwater streams, and whether they are
perennial, intermittent, or ephemeral, they play an important role in
the transport of water, sediments, organic matter, nutrients, and
organisms to downstream waters. Covered tributaries serve to store
water, thereby reducing flooding; provide biogeochemical functions that
help maintain water quality; trap and transport sediments; transport,
store and modify pollutants; provide habitat for plants and animals;
and sustain the biological productivity of downstream rivers, lakes,
and estuaries. Such waters have these significant effects whether they
are natural, modified, or constructed.
Covered tributaries significantly affect the chemical integrity of
traditional navigable waters, interstate waters, and the territorial
seas. Covered tributaries influence the chemical composition of
downstream waters, through the transport and removal of chemical
elements and compounds, such as nutrients, ions, organic matter and
pollutants. Ecosystem processes in
[[Page 37069]]
covered tributaries transform, remove, and transport these substances
to downstream waters. In turn, these chemical compounds can influence
water quality, sediment deposition, nutrient availability, and biotic
functions in rivers. Because water flow transports chemical substances
downstream, chemical effects are closely related to hydrological
connectivity. Within covered tributaries, there are processes that
occur that transform and export nutrients and carbon to downstream
waters, serving important source functions that influence the chemical
integrity of downstream waters. Organic carbon, in both dissolved and
particulate forms, exported from covered tributaries is consumed by
downstream organisms. The organic carbon that is exported downstream
thus supports biological activity throughout the river network.
Covered tributaries act as both sinks and sources of chemical
substances, further affecting the chemical integrity of traditional
navigable waters, interstate waters, and the territorial seas. Covered
tributaries provide sink functions by trapping chemicals through
absorption to sediments in the stream substrate (e.g., phosphorous
adsorption to clay particles). They provide source functions by
transporting chemicals to downstream traditional navigable waters,
interstate waters, and the territorial seas as chemicals dissolved in
the waters or as chemicals attached to suspended sediments.
Covered tributaries significantly affect the physical integrity of
traditional navigable waters, interstate waters, and the territorial
seas. Physical connections between covered tributaries and traditional
navigable waters, interstate waters, and the territorial seas result
from the hydrologic transport from covered tributaries to downstream
waters of numerous materials, including water, sediment and organic
matter such as leaves and wood. This transport affects the physical
characteristics of downstream waters. Covered tributaries, even when
seasonally dry, are the dominant source of water in most rivers, rather
than direct precipitation or groundwater input to main stem river
segments. One of the primary functions of covered tributaries is
transporting sediment to downstream waters. Covered tributaries,
particularly headwaters, shape and maintain river channels by
accumulating and gradually or episodically releasing sediment and large
woody debris into river channels. These effects occur even when the
covered tributaries flow infrequently (such as ephemeral covered
tributaries), and even when the covered tributaries are great distances
from the traditional navigable water, interstate water, or the
territorial sea (such as some headwater covered tributaries).
Covered tributaries significantly affect the biological integrity
of traditional navigable waters, interstate waters, and the territorial
seas. Covered tributaries, including intermittent and ephemeral
streams, are critical in the life-cycles of many organisms capable of
moving throughout river networks. In fact, many organisms, such as
anadromous salmon, have complex life-cycles which involve migration
through the river network, from headwaters to downstream rivers and
oceans and back, over the course of their lives. In addition to
providing critical habitat for complex life-cycle completion, covered
tributaries provide refuge from predators and adverse physical
conditions in rivers, and are reservoirs of genetic- and species-level
diversity. Covered tributaries contribute materials to downstream food
networks and supporting populations for aquatic species, including
economically important species such as salmon. These effects occur even
when the covered tributaries flow infrequently (such as ephemeral
covered tributaries), and even when the covered tributaries are large
distances from the traditional navigable waters, interstate waters, and
the territorial seas (such as some headwater covered tributaries).
Similarly, modified and constructed tributaries perform the same
functions as natural tributaries, especially the conveyance of water
that carries nutrients, pollutants, and other constituents, both good
and bad, to traditional navigable waters, interstate waters, and the
territorial seas. Modified and constructed covered tributaries also
provide corridors for movement of organisms between headwaters and
traditional navigable waters, interstate waters, and the territorial
seas. The important effect--and thus the significant nexus--between a
covered tributary and a traditional navigable water, interstate water,
and the territorial sea is not broken where the covered tributary flows
through a culvert or other structure. The scientific literature
recognizes that features that convey water, whether they are natural,
modified, or constructed, provide substantial connectivity between
streams and downstream waters. For example, ditches that meet the
definition of tributary and are not excluded quickly move water
downstream to traditional navigable waters, interstate waters, and the
territorial seas due to their often straightened and channelized
nature, transporting downstream sediment, nutrients, and other
materials.
The CWA regulates and controls pollution at its source, in part
because most pollutants do not remain at the site of the discharge, but
instead flow and are washed downstream through the tributary system to
endanger drinking water supplies, fisheries, and recreation areas.
These fundamental facts about the movement of pollutants and the
interconnected nature of the tributary system demonstrate why covered
tributaries of traditional navigable waters, interstate waters, and the
territorial seas, alone or in combination with other covered
tributaries in a watershed, have a significant nexus with those
downstream waters. Thus, in the rule the agencies assert CWA
jurisdiction over all covered tributaries as defined. Those covered
tributaries are ``waters of the United States'' without the need for
further analysis.
b. Covered Adjacent Waters
Based on the agencies' review of the scientific literature and the
law, the agencies determine that covered adjacent waters, as defined,
have a significant nexus and are ``waters of the United States.'' The
scientific literature, including the Science Report, consistently
supports the conclusion that covered adjacent waters provide similar
functions and work together to maintain the chemical, physical, and
biological integrity of the downstream traditional navigable waters,
interstate waters, and the territorial seas because of their
hydrological and ecological connections to, and interactions with,
those waters. Science demonstrates that this functional connectivity is
particularly evident where covered adjacent waters are located within
the floodplain of the traditional navigable water, interstate water,
the territorial seas, covered tributary, or impoundment to which they
are adjacent or are otherwise sufficiently proximate to waters with no
floodplain, such as lakes and ponds. Location within the floodplain and
proximity ensure that the aquatic functions performed by covered
adjacent waters are effectively and consistently provided to downstream
waters. See Technical Support Document.
The agencies conclude that all waters meeting the definition of
``adjacent'' in the rule are similarly situated for purposes of
analyzing whether they have a significant nexus to a traditional
navigable water, interstate water, or the territorial sea. Based on a
review of the scientific literature, the agencies conclude that these
bordering, contiguous, or neighboring waters
[[Page 37070]]
provide similar functions and function together to significantly affect
the chemical, physical, or biological integrity of traditional
navigable waters, interstate waters, or the territorial seas. Further,
because the definition of ``adjacent'' considers both the functional
relationships and the proximity of the waters (i.e., those that are
located near traditional navigable waters, interstate waters, the
territorial seas, impoundments, and covered tributaries), interpreting
the term ``similarly situated'' to include all covered adjacent waters,
as defined in the rule, is informed by the science and is a reasonable
interpretation of the scope of the statute. The geographic proximity of
an ``adjacent'' water relative to the traditional navigable waters,
interstate waters, the territorial seas, impoundments, and covered
tributaries is indicative of the relationship to it, with many of its
defining characteristics resulting from the movement of materials and
energy between the categories of waters. The scientific literature
supports that waters, including wetlands, ponds, lakes, oxbow lakes,
and similar waters, that are ``adjacent,'' as defined in the rule, to
traditional navigable waters, interstate waters, the territorial seas,
impoundments, and covered tributaries, are integral parts of stream
networks because of their ecological functions and how they interact
with each other, and with downstream traditional navigable waters,
interstate waters, or the territorial seas.
Covered adjacent waters function together to maintain the chemical,
physical, or biological health of traditional navigable waters,
interstate waters, and the territorial seas to which they are directly
adjacent or to which they are connected by the tributary system. This
functional interaction can result from hydrologic connections or
because covered adjacent waters can act as water storage areas holding
damaging floodwaters or filtering harmful pollutants. These chemical,
physical, and biological connections affect the integrity of downstream
traditional navigable waters, interstate waters, and the territorial
seas through the temporary storage and deposition of channel-forming
sediment and woody debris, temporary storage of local groundwater
sources of baseflow for downstream waters and their tributaries, and
transformation and transport of organic matter. Covered adjacent waters
improve water quality through the assimilation, transformation, or
sequestration of pollutants, including excess nitrogen and phosphorus,
and chemical contaminants such as pesticides and metals that can
degrade downstream water integrity. In addition to providing effective
buffers to protect downstream waters from pollution, covered adjacent
waters form integral components of downstream food webs, providing
nursery habitat for breeding fish and amphibians, colonization
opportunities for stream invertebrates, and maturation habitat for
stream insects. Covered adjacent waters serve an important role in the
integrity of traditional navigable waters, interstate waters, and the
territorial seas by subsequently releasing (desynchronizing)
floodwaters and retaining large volumes of stormwater, sediment,
nutrients, and contaminants that could otherwise negatively impact the
condition or function of traditional navigable waters, interstate
waters, and the territorial seas.
Floodplain areas connect aquatic environments through both surface
and shallow subsurface hydrologic flowpaths. Waters in these areas are
therefore uniquely situated in watersheds to receive and process water
that passes over densely vegetated areas and through subsurface zones
before reaching streams and rivers. When contaminants reach a
floodplain water, they can be sequestered in sediments, assimilated
into wetland plants and animals, transformed into less harmful and/or
mobile forms or compounds, or lost to the atmosphere. Wetlands located
in floodplains store large amounts of sediment and organic matter from
upstream and upland areas. In addition, the primary function of many
floodplain wetlands in the Western United States is sediment exchange,
which can transform materials and compounds temporarily on floodplains.
Wetlands and other similar waters in floodplain areas act as
buffers that are among the most effective tools for mitigating nonpoint
source pollution. The literature shows that collectively, wetlands and
other similar waters improve water quality through assimilation,
transformation, or sequestration of nutrients, sediment, and other
pollutants--such as pesticides and metals--that can affect downstream
water quality. These pollutants enter floodplain wetlands from dry and
wet atmospheric deposition, runoff from upland agricultural and urban
areas, spray drift, subsurface water flows, outfalls, pipes, and
ditches.
Floodplain waters, including wetlands, can reduce flood peaks by
storing and desynchronizing floodwaters. They can also maintain river
baseflows by recharging alluvial aquifers. Many studies have documented
the ability of floodplain wetlands to reduce flood pulses by storing
excess water from streams and rivers. One review of wetland studies
reported that floodplain wetlands reduced or delayed floods in 23 of 28
studies. For example, peak discharges between upstream and downstream
gaging stations on the Cache River in Arkansas were reduced 10-20
percent primarily due to floodplain water storage.
Ecosystem function within a river system is driven by interactions
between the physical environment and the diverse biological communities
living within the river system. Wetlands in floodplains become
important seed sources for the river network, especially if
catastrophic flooding scours vegetation and seed banks in other parts
of the channel. Movements of organisms that connect aquatic habitats
and their populations, even across different watersheds, are important
for the survival of individuals, populations, and species, and for the
functioning of the river ecosystem. For example, lateral expansion and
contraction of the river in its floodplain results in an exchange of
matter and organisms, including fish populations that are adapted to
use floodplain habitat for feeding and spawning during high water. The
organisms that live within the hyporheic zone for these mid- and large-
sized river systems have a demonstrated connection outward to several
miles within the floodplain. General field practice observations
further indicate that covered adjacent waters with a close proximity
have a significant nexus with the downstream waters.
Waters adjacent to impoundments and covered tributaries are
integrally linked to the chemical, physical, and biological functions
of the waters to which they are adjacent and, through those waters, are
integrally linked to the chemical, physical, and biological functions
of the downstream traditional navigable waters, interstate waters, or
the territorial seas. Thus, where waters are adjacent to impoundments
or covered tributaries, they also have a significant nexus to the
downstream traditional navigable waters, interstate waters, or the
territorial seas. The important functions that covered adjacent waters
perform that impact downstream traditional navigable waters, interstate
waters, and the territorial seas and their integrated behavior with the
tributary system demonstrate why all waters adjacent to traditional
navigable waters, interstate waters, or the territorial seas as well as
impoundments and covered tributaries, alone or in combination with
other
[[Page 37071]]
covered adjacent wetlands in a watershed have a significant nexus with
those downstream waters.
Based on the science and their technical expertise and experience,
the agencies determine it is appropriate to protect all covered
adjacent waters because those waters are functioning as an integrated
system with the downstream traditional navigable waters, interstate
waters, or the territorial seas and significantly affect such
downstream waters. Consequently, these waters are ``adjacent'' and
therefore ``waters of the United States'' under the CWA. Covered
adjacent waters are ``waters of the United States'' without the need
for further analysis.
3. Case-Specific Significant Nexus Determinations
a. Two Exclusive Circumstances for Case-Specific Significant Nexus
Determinations
The rule identifies two exclusive circumstances under which a
significant nexus determination is made on a case-specific basis to
determine whether the water is a ``water of the United States.'' First,
there are five subcategories of waters--Prairie potholes, Carolina and
Delmarva bays, pocosins, western vernal pools in California, and Texas
coastal prairie wetlands--that the agencies conclude must be analyzed
``in combination'' as ``similarly situated '' waters when making a
case-specific significant nexus analysis. Second, there are waters for
which the agencies have made no conclusions with respect to which
waters are ``similarly situated'' but for which a case-specific
significant nexus analyses may be undertaken. The rule establishes that
case-specific determinations may be made for waters located within the
100-year floodplain of a traditional navigable water, interstate water,
or the territorial seas, and for waters located within 4,000 feet from
the high tide line or the ordinary high water mark of traditional
navigable waters, interstate waters, the territorial seas,
impoundments, or tributaries.
b. Summary of Rationale for ``Similarly Situated'' Determinations
Based on the agencies' expertise and experience and available
literature and data, the agencies have determined that waters in the
five subcategories of waters identified in paragraph (a)(7) are
similarly situated and must be combined with other waters in the same
subcategory located in the same watershed that drains to the nearest
traditional navigable water, interstate water, or the territorial seas.
See Technical Support Document. The scientific literature shows that
these subcategories of waters are frequently located together in a
complex or are otherwise closely co-located and perform similar
functions. The agencies specifically sought comment in the proposal on
options to address these five subcategories of waters, including
whether waters in these subcategories should be found ``similarly
situated'' by rule.
Based on the body of scientific literature regarding the
subcategories of waters specified in paragraph (a)(7) and their
functions, the agencies determined that waters of the specified
subcategories are similarly situated because they perform similar
functions and they are located sufficiently close to each other to
function together in affecting downstream waters and therefore
reasonably be evaluated in combination with regard to their effects on
the integrity of traditional navigable waters, interstate waters, or
the territorial seas. The specified subcategories of waters perform
similar functions as waters of the same subcategory in the same single
point of entry watershed and collectively function together to affect a
traditional navigable water, interstate water, or the territorial seas.
Among the functions and relationships in the landscape the agencies
considered to conclude that the subcategories are each similarly
situated are the physical capacity of the waters to provide flood and
sediment retention. In determining that the waters in each of the five
subcategories are ``similarly situated,'' the agencies concluded that
these subcategories of waters are co-located to each other or similar
to the tributary system such that they have cumulative and additive
effects on pollutant removal through parallel, serial, or sequential
processing, such as the role of pocosins in maintaining water quality
in estuaries. The subcategories of waters are sufficiently near each
other or the tributary system to function as an integrated habitat that
can support the life-cycle of a species or more broadly provide habitat
to a large number of a single species.
The SAB expressed support for the agencies' option in the preamble
of the proposed rule to identify certain subcategories of waters as
similarly situated and highlighted these same five subcategories. It
stated, ``[t]here is also adequate scientific evidence to support a
determination that certain subcategories and types of `other waters' in
particular regions of the United States (e.g., Carolina and Delmarva
Bays, Texas coastal prairie wetlands, prairie potholes, pocosins,
western vernal pools) are similarly situated (i.e., they have a similar
influence on the physical, chemical and biological integrity of
downstream waters and are similarly situated on the landscape) and thus
could be considered waters of the United States. Furthermore, as the
science continues to develop, other sets of wetlands may be identified
as `similarly situated.' '' SAB 2014b at 3.
The agencies concluded that the specific subcategories of waters
listed in paragraph (a)(7) are similarly situated for purposes of a
case-specific significant nexus based on the following:
(i) Prairie potholes are a complex of glacially formed wetlands,
usually occurring in depressions that lack permanent natural outlets
that are found in the central United States and Canada. In the United
States, they are found from central Iowa through western Minnesota,
Montana, eastern South Dakota, and North Dakota. Prairie potholes
demonstrate a wide range of hydrologic permanence; some hold permanent
standing water and others are wet only in years with high
precipitation. This in turn influences the diversity and structure of
their biological communities.
Prairie potholes generally accumulate and retain water effectively
due to the low permeability of their underlying soil, which can
modulate flow characteristics of nearby streams and rivers. One of the
most noted hydrologic functions of Prairie potholes is water storage.
Because most of the water outflow in Prairie potholes is via
evapotranspiration, Prairie potholes can become water sinks, preventing
flow to downstream waters. Prairie potholes also can accumulate
chemicals in overland flow, thereby reducing chemical loading to other
bodies of water. When Prairie potholes are artificially connected to
streams and lakes through drainage, they become sources of water and
chemicals to downstream waters. Prairie potholes also support a
community of highly mobile organisms, from plants to invertebrates that
move among Prairie potholes and that can biologically connect the
entire complex to the river network.
Prairie potholes can be highly connected to other Prairie potholes
via shallow subsurface connections and via surface hydrologic
connections during the wet season. They can also be connected to the
stream network via surface and shallow subsurface connections. Intense
precipitation events or high cumulative precipitation over one or more
seasons can result in temporary hydrologic connectivity between Prairie
potholes and from
[[Page 37072]]
Prairie potholes to the tributary system via ``fill-and-spill'' events.
Their density across the landscape varies from region to region as
the result of several factors, including patterns of glacial movement,
topography, and climate. In some parts of the region, prairie pothole
density is very high. Though their density varies across the landscape,
Prairie potholes often act as a complex. They have similar functions
that can collectively impact downstream waters.
Prairie potholes have been determined to be similarly situated
based on the characteristics of Prairie potholes, including their
density on the landscape, their interaction and formation as a complex
of wetlands and open waters, their connections to each other and the
tributary network, and their similar functions. In addition, their
chemical, physical, and biological connections to downstream waters and
the strength of their effects on the chemical, physical, or biological
integrity of a traditional navigable water, interstate water, or the
territorial seas support this determination that Prairie potholes are
similarly situated by rule.
(ii) Carolina and Delmarva bays are ponded depressional wetlands
that occur along the Atlantic coastal plain from northern Florida to
New Jersey. Though Carolina and Delmarva bays are from the same
category of wetland and perform similar functions, they are located in
different parts of the Atlantic coastal plain and thus have unique
names. Carolina bays are most abundant in North Carolina and South
Carolina, while Carolina bays found in the Delmarva Peninsula are
commonly referred to as Delmarva bays or Delmarva potholes.
Most bays receive water through precipitation, lose water through
evapotranspiration, and lack natural surface outlets. Both mineral-
based and peat-based bays have shown connections to shallow
groundwater. Bays typically are in proximity to each other or to
streams, providing for hydrologic connections to each other and to
downstream waters in large rain events via overland flow or shallow
subsurface connections. Some Delmarva bays have surface water
connections to the Chesapeake Bay. In addition, human channeling and
ditching of the bays are widespread and create surface connections to
other waters, including the tributary system and estuaries. These
ditches commonly connect the surface water of bays to other bays that
are lower on the landscape, and ultimately, to streams.
The hydrology in bays allow for denitrification (chemical and
biological processes that remove nitrogen from water), which can reduce
the amount of nitrate in both groundwater and downstream surface
waters. Because bays are frequently connected chemically to downstream
waters through ditches, they can be sources of sediment and nutrients
to downstream waters. Where they are not connected via confined surface
connections, bays can act as sediment and nutrient sinks.
Fish are reported in bays that are known to dry out, indirectly
demonstrating surficial connections. Amphibians and reptiles use bays
extensively for breeding and for rearing young. These animals can
disperse many feet on the landscape and can colonize, or serve as a
food source to, downstream waters. Similarly, bays foster abundant
insects that have the potential to become part of the downstream food
chain. Humans have ditched and channelized a high percentage of bays,
creating new surface connections to downstream waters and allowing
transfer of nutrients, sediment, and other pollutants, such as
methylmercury.
Carolina and Delmarva bays can occur in high density on the
landscape and can act as a wetlands complex. Bays have similar
functions to other bays and cumulatively these functions can impact
downstream waters.
The agencies conclude that Carolina and Delmarva bays are similarly
situated based on their close proximity to each other and the tributary
network, their hydrologic connections to each other and the tributary
network, their density on the landscape, and their similar functions.
(iii) The word pocosin comes from the Algonquin Native American
word for ``swamp on a hill,'' and these evergreen shrub and tree-
dominated wetlands are found from Virginia to northern Florida, but
mainly in North Carolina. Typically, there is no standing water present
in these peat-accumulating wetlands, but a shallow water table leaves
the soil saturated for much of the year. They range in size from less
than an acre to several thousand acres. The slow movement of water
through the dense organic matter in pocosins removes excess nutrients
deposited by rainwater. The same organic matter also acidifies the
water. This water is slowly released to downstream waters and
estuaries, where it helps to maintain the proper salinity, nutrients,
and acidity.
Because pocosins are the topographic high areas on the regional
landscape, they serve as the source of water for downstream waters.
Pocosins often have seasonal connections to drainageways leading to
estuaries or are adjoining other wetlands draining into perennial
streams or estuaries. Other pocosins have been ditched and are directly
connected to streams.
The agencies conclude that pocosins are similarly situated based on
their close proximity to each other and the tributary network, their
hydrologic connections to each other and the tributary network, their
density on the landscape, and their similar functions.
(iv) Western vernal pools are shallow, seasonal wetlands that
accumulate water during colder, wetter months and gradually dry up
during warmer, drier months. Western vernal pools are seasonal wetlands
from the Pacific Northwest to northern Baja California, Mexico
associated with topographic depressions, soils with poor drainage,
mild, wet winters and hot, dry summers. The agencies have determined
that California vernal pools are ``similarly situated.''
Because their hydrology and ecology are so tightly coupled with the
local and regional geological processes that formed them, western
vernal pools in California typically occur within ``vernal pool
landscapes,'' or complexes of pools in which swales connect pools to
each other and to seasonal streams. Some common findings about the
hydrologic connectivity of western vernal pools include evidence for
temporary or permanent outlets, frequent filling and spilling of higher
pools into lower elevation swales and stream channels, and conditions
supporting subsurface flows through pools without perched aquifers to
nearby streams.
Non-glaciated vernal pools in western states are reservoirs of
biodiversity and can be connected genetically to other locations and
aquatic habitats through wind- and animal-mediated dispersal. Animals
and other organisms can move between western vernal pool complexes and
streams. Insects and zooplankton can be flushed from vernal pools into
streams and other waters during periods of overflow, carried by animal
vectors (including humans), or dispersed by wind.
The agencies conclude that western vernal pools in California are
similarly situated based on their close proximity to each other and the
tributary network, their interaction and arrangement as a complex of
wetlands, their hydrologic connections to each other and the tributary
network, their density on the landscape, and their similar functions.
(v) Along the Gulf of Mexico from western Louisiana to south Texas,
freshwater wetlands occur as a mosaic
[[Page 37073]]
of depressions, ridges, intermound flats, and mima mounds. These
coastal prairie wetlands were formed thousands of years ago by ancient
rivers and bayous and once occupied almost a third of the landscape
around Galveston Bay, Texas. The term Texas coastal prairie wetlands is
not used uniformly in the scientific literature but encompasses Texas
prairie pothole (freshwater depressional wetlands) and marsh wetlands
that are described in some studies that occur on the Lissie and
Beaumont Geological Formations, and the Ingleside Sand.
Texas coastal prairie wetlands are locally abundant and in close
proximity to other coastal prairie wetlands and function together
cumulatively. Collectively as a complex, Texas coastal prairie wetlands
can be geographically and hydrologically connected to each other via
swales and connected to downstream waters, contributing flow to those
downstream waters. Cumulatively, these wetlands can control nutrient
release levels and rates to downstream waters, as they capture, store,
transform, and pulse releases of nutrients to those waters.
The agencies conclude that Texas coastal prairie wetlands are
similarly situated based on their close proximity to each other and the
tributary network, their hydrologic connections to each other and the
tributary network, their interaction and formation as a complex of
wetlands, their density on the landscape, and their similar functions.
IV. Definition of ``Waters of the United States''
A. Summary of the Rule
The rule revises the existing definition of ``waters of the United
States'' consistent with the CWA, science, the agencies' technical
expertise and experience, and Supreme Court decisions. The final rule
establishes categories of waters that are jurisdictional and other
categories of waters that are excluded, as well as categories of waters
and wetlands that require a case-specific significant nexus evaluation
to determine if they are ``waters of the United States'' and covered by
the CWA. The rule also provides definitions for key terms used in the
regulation. The final rule retains much of the structure of the
agencies' longstanding definition of ``waters of the United States,''
and many of the existing provisions of that definition where revisions
are not required in light of Supreme Court decisions or other bases for
revision. All existing exclusions from the definition of ``waters of
the United States'' are retained, and several exclusions reflecting
longstanding agencies' practice are added to the regulation for the
first time.
The agencies define ``waters of the United States'' in paragraph
(a) of the rule for all sections of the CWA to include the traditional
navigable waters (a)(1), interstate waters (a)(2), the territorial seas
(a)(3), impoundments of jurisdictional waters (a)(4), covered
tributaries (a)(5), and covered adjacent waters (a)(6). Waters in these
categories are jurisdictional ``waters of the United States'' by rule--
no additional analysis is required. This eliminates the need to make a
case-specific significant nexus determination for covered tributaries
or covered adjacent waters because the agencies determined that these
waters have a significant nexus to waters identified in (a)(1) through
(a)(3) of the rule and thus are ``waters of the United States.'' The
agencies emphasize that the finding of jurisdiction for these covered
tributaries and covered adjacent waters was not based on the mere
connection of a water body to downstream waters, but rather a
determination that the nexus, alone or in combination with other of
these covered tributaries or covered adjacent waters in the watershed,
is significant.
The agencies exclude specified waters from the definition of
``waters of the United States'' in paragraph (b) of the rule. The rule
makes no substantive change to the existing exclusion for waste
treatment systems designed consistent with the requirements of the CWA
and makes no change to the existing exclusion for prior converted
cropland. The rule excludes for the first time certain waters and
features over which the agencies have generally not asserted CWA
jurisdiction, as well as groundwater, which the agencies have never
interpreted to be a ``water of the United States'' under the CWA.
Codifying these longstanding practices supports the agencies' goals of
providing greater clarity, certainty, and predictability for the
regulated public and regulators, and makes rule implementation clear
and practical.
This final rule provides clear exclusions for certain types of
ditches. The final rule also expressly excludes stormwater control
features created in dry land and certain wastewater recycling
structures created in dry land. Waters and features that are excluded
under paragraph (b) of the rule cannot be determined to be
jurisdictional under any of the categories in the rule under paragraph
(a).
In addition to waters that are categorically ``waters of the United
States'' or categorically excluded under paragraphs (a) and (b), the
rule identifies certain waters that can be ``waters of the United
States'' only where a case-specific determination has found a
significant nexus between the water and traditional navigable waters,
interstate waters, or the territorial seas. First, paragraph (a)(7) of
the rule specifies five types of waters (Prairie potholes, Delmarva and
Carolina bays, pocosins, western vernal pools in California, and Texas
coastal prairie wetlands) that the agencies have determined to be
``similarly situated,'' and thus are to be considered in combination in
a significant nexus analysis. Second, paragraph (a)(8) specifies that
waters located within the 100-year floodplain of a traditional
navigable water, interstate water, or the territorial seas, and waters
located within 4,000 feet from the high tide line or the ordinary high
water mark of traditional navigable waters, interstate waters, the
territorial seas, impoundments, or covered tributaries may be found to
have a significant nexus on a case-specific basis, but the agencies
have not made a determination that the waters are ``similarly
situated.'' As a result, a significant nexus analysis for these waters
will include a case-specific assessment of whether there are any
similarly situated waters, as well as whether the water, alone or in
combination with any waters determined to be similarly situated, has a
significant nexus to a traditional navigable water, interstate water,
or territorial sea. The rule outlines at (c)(5)(i)-(ix) functions
relevant to these case-specific significant nexus analyses.
Paragraph (c) of the rule provides definitions for key terms used
in the regulation. Some of these are unchanged from the current
regulations, including the definitions for ``wetlands'' at (c)(4),
``ordinary high water mark'' at (c)(6) and ``high tide line'' at
(c)(7), although the latter two are existing, unchanged Corps'
definitions added to EPA's regulations for the first time. 33 CFR
328.3(d)-(e). The rule also defines for the first time ``tributary''
and ``tributaries'' at (c)(3), ``neighboring'' (an aspect of adjacency)
at (c)(2), and ``significant nexus'' at (c)(5).
This rule is effective on August 28, 2015. Under existing Corps'
regulations and guidance, approved jurisdictional determinations
generally are valid for five years. The agencies will not reopen
existing approved jurisdictional determinations unless requested to do
so by the applicant or, consistent with existing Corps' guidance,
unless new information warrants revision of the determination before
the expiration period. Similarly, consistent with existing regulations
and guidance, approved jurisdictional determinations
[[Page 37074]]
associated with issued permits and authorizations are valid until the
expiration date of the permit or authorization.
As a general matter, the agencies' actions are governed by the rule
in effect at the time the agency issues a jurisdictional determination
or permit authorization, not by the date of a permit application,
request for authorization, or request for a jurisdictional
determination. However, any jurisdictional determinations issued prior
to the effective date of the rule and jurisdictional determinations
associated with permit applications deemed by the Corps to have been
complete on the date this rule is published in the Federal Register,
including complete pre-construction notifications, will be made
consistent with the existing rule, unless the applicant requests that
its approved jurisdictional determination or permit authorization be
decided after the effective date of the new rule. Reliance on
preliminary jurisdictional determinations is also not affected by the
issuance of this rule. All other jurisdictional determinations and
requests for authorization requiring an approved jurisdictional
determination issued on or after the effective date of this rule will
be made consistent with this rule.
It is important to emphasize that the agencies do not anticipate
being able to complete new jurisdictional determinations submitted
after this rule is published before it becomes effective. As a result,
requesters seeking jurisdictional determinations after the rule is
published should expect the determination will be made consistent with
this rule. The agencies recognize there are a number of requests for
permit applications and requests for jurisdictional determinations
pending at any time. The agencies expect only a small portion of those
pending actions will require additional information from or work by the
requester. As described in the Economic Analysis, the vast majority of
requests address streams and adjacent wetlands, and the agencies do not
expect new information or work will be needed to complete those
requests. If any additional information is needed to assess these
requests, the agencies will work proactively with permit applicants to
reduce potential short-term disruptions in the permit process that may
be associated with the rule.
B. Traditional Navigable Waters
The existing regulations include within the definition of ``waters
of the United States'' all waters that are currently used, or were used
in the past, or may be susceptible to use in interstate or foreign
commerce, including all waters which are subject to the ebb and flow of
the tide. See, e.g., 33 CFR 328.3(a)(1); 40 CFR 230.3(s)(1); 40 CFR
122.2 (``waters of the U.S.''). This paragraph of the regulation
encompasses those waters that are often referred to as ``traditional
navigable waters.'' The rule does not make any changes to this
paragraph of the regulation.
For purposes of CWA jurisdiction, waters will be considered
traditional navigable waters, and jurisdictional under (a)(1) of the
rule, if they:
Are subject to section 9 or 10 of the Rivers and Harbors
Appropriations Act of 1899;
Have been determined by a Federal court to be navigable-
in-fact under Federal law;
Are waters currently being used for commercial navigation,
including commercial waterborne recreation (for example, boat rentals,
guided fishing trips, or water ski tournaments);
Have historically been used for commercial navigation,
including commercial waterborne recreation; or
Are susceptible to being used in the future for commercial
navigation, including commercial waterborne recreation.
See Technical Support Document; ``U.S. Army Corps of Engineers
Jurisdictional Determination Form Instructional Guidebook Appendix D,
`Traditional Navigable Waters,''' available at: https://www.usace.army.mil/Portals/2/docs/civilworks/regulatory/cwa_guide/app_d_traditional_navigable_waters.pdf.
The agencies received several comments on the scope of traditional
navigable waters. Some commenters observed that ``traditional navigable
waters'' as a jurisdictional category is not based in science. Several
commenters thought that the final rule should specify considerations to
be taken into account when determining if a water is susceptible to
being used in future commercial navigation. The agencies have not
revised the regulation to address susceptibility, but observe that case
law has provided a number of considerations and examples that are
described further in the Technical Support Document and are reflected
in longstanding agencies' practice.
C. Interstate Waters
The existing regulations define ``waters of the United States'' to
include interstate waters, including interstate wetlands. The rule does
not change that provision of the regulations. Therefore, interstate
waters are ``waters of the United States'' even if they are not
navigable for purposes of Federal regulation under (a)(1) and do not
connect to such waters. Moreover, the rule protects impoundments of
interstate waters, tributaries to interstate waters, waters adjacent to
interstate waters, and waters adjacent to covered tributaries of
interstate waters because they have a significant nexus to interstate
waters. Protection of these waters is thus critical to protecting
interstate waters.
The language of the CWA indicates that Congress intended the term
``navigable waters'' to include interstate waters without imposing a
requirement that they be traditional navigable waters themselves or be
connected to traditional navigable waters. The precursor statutes to
the CWA subjected interstate waters and their tributaries to Federal
jurisdiction. The text of the CWA, specifically CWA section 303, which
establishes ongoing requirements for interstate waters, in conjunction
with the definition of navigable waters, provides clear indication of
Congress' intent to protect interstate waters that were previously
subject to Federal regulation. Other provisions of the statute provide
additional textual evidence of the scope of the primary jurisdictional
term of the CWA.
The agencies also have a longstanding regulatory interpretation
that interstate waters fall within the scope of CWA jurisdiction. The
agencies' interpretation was promulgated contemporaneously with the
passage of the CWA and is consistent with the statutory and legislative
history of the CWA. Furthermore, the Supreme Court has never addressed
the CWA's coverage of interstate waters, and it is not reasonable to
read its decisions in SWANCC and Rapanos to question the jurisdictional
status of interstate waters or to impose additional jurisdictional
requirements on interstate waters. The assertion of jurisdiction over
interstate waters is based on the statute and under predecessor
statutes where ``interstate waters'' were defined as all rivers, lakes,
and other waters that flow across, or form a part of, state boundaries.
Pub. L. 80-845, sec. 10, 62 Stat. 1155, at 1161 (1948). The agencies
will continue to implement the provision consistent with the intent of
Congress. For additional discussion of the agencies' interpretation of
the CWA with respect to interstate waters, see Appendix B of the
proposed rule and the Technical Support Document.
It is reasonable to assert jurisdiction over tributaries, adjacent
waters, and waters that have a significant nexus to interstate waters
consistent with the framework set forth in Justice Kennedy's
[[Page 37075]]
opinion in Rapanos for establishing jurisdiction over waters with a
significant nexus to traditional navigable waters. Waters and wetlands
with a significant nexus to traditional navigable waters and interstate
waters have important beneficial effects on those waters, and by
recognizing that polluting or destroying waters with a significant
nexus can harm downstream jurisdictional waters. Traditional navigable
waters and interstate waters cannot be protected without also
protecting the waters that have a significant nexus to those waters as
identified in the rule. The rule thus defines ``waters of the United
States'' to include tributaries to interstate waters, waters adjacent
to interstate waters, waters adjacent to tributaries of interstate
waters, and other waters that have a significant nexus to interstate
waters.
The agencies received a number of comments on interstate waters.
Some commenters asserted that interstate waters required a significant
nexus to a traditional navigable water in order to be jurisdictional
after Rapanos. The agencies disagree for the reasons described above,
in Appendix B to the proposed rule, and in the Technical Support
Document.
D. Territorial Seas
The CWA and its existing regulations include ``the territorial
seas'' as a ``water of the United States.'' The rule makes no changes
to that provision of the regulation other than to change the ordering
to earlier in the regulation. The CWA defines ``navigable waters'' to
include ``the territorial seas'' at section 502(7). The CWA goes on to
define the ``territorial seas'' in section 502(8) as ``the belt of the
seas measured from the line of ordinary low water along that portion of
the coast which is in direct contact with the open sea and the line
marking the seaward limit of inland waters, and extending seaward a
distance of three miles.'' The territorial seas establish the seaward
limit of ``waters of the United States.'' The territorial seas are
clearly covered by the CWA (they are also traditional navigable
waters), and it is reasonable to protect their covered tributaries and
covered adjacent waters.
Although some comments addressed the definition of ``territorial
seas'' provided in the CWA suggesting that the distance thresholds be
revised to reflect other resource statutes, the agencies do not have
authority to revise statutory language.
E. Impoundments
The existing regulations provide that impoundments of ``waters of
the United States'' remain ``waters of the United States,'' and the
rule does not make any changes to the existing regulatory language.
Impoundments are jurisdictional because an impoundment of a ``water
of the United States'' remains a ``water of the United States,'' and
because scientific literature demonstrates that impoundments continue
to significantly affect the chemical, physical, or biological integrity
of downstream traditional navigable waters, interstate waters, and the
territorial seas. See Technical Support Document. The Supreme Court has
confirmed that damming or impounding a ``water of the United States''
does not make the water non-jurisdictional. See S. D. Warren Co. v.
Maine Bd. of Envtl. Prot., 547 U.S. 370, 379 n.5 (2006) (``[N]or can we
agree that one can denationalize national waters by exerting private
control over them.''). Similarly, when presented with a tributary to
the Snake River which flows only about two months per year because of
an irrigation diversion structure installed upstream, the Ninth Circuit
noted ``it is doubtful that a mere man-made diversion would have turned
what was part of the waters of the United States into something else
and, thus, eliminated it from national concern.'' U.S. v. Moses, 496
F.3d 984, 988 (9th Cir. 2007), cert. denied, 554 U.S. 918 (2008). As a
matter of policy and law, impoundments do not de-federalize a water,
even where there is no longer flow below the impoundment. The agencies
have analyzed stream networks, above and below impoundments, for
connection to downstream traditional navigable waters, interstate
waters, or the territorial seas. Scientific literature, as well as the
agencies' scientific and technical expertise and experience confirm
that impoundments have chemical, physical, and biological effects on
downstream waters. See Technical Support Document.
The agencies also note that an impoundment of a water that is not a
``water of the United States'' can become jurisdictional if, for
example, the impounded waters become navigable-in-fact and covered
under paragraph (a)(1) of the rule.
By their nature, impoundments of jurisdictional waters would also
often meet the definition of ``adjacent waters,'' as they are typically
bordering or contiguous. Impoundments of ``waters of the United
States'' are per se jurisdictional under paragraph (a)(4) of the rule
without the need to determine if they are also adjacent under paragraph
(a)(6). However, as described in section IV.G below, ``adjacent
waters,'' as defined, have a significant nexus to traditional navigable
waters, interstate waters, or the territorial seas, which bolsters the
agencies' determination that impoundments of ``waters of the United
States'' remain ``waters of the United States.''
Impoundments also may be one of the waters through which
tributaries indirectly contribute flow to a traditional navigable
water, interstate water, or territorial sea. As a matter of law and
science, an impoundment does not cut off a connection between upstream
tributaries and a downstream traditional navigable water, interstate
water, or territorial sea, so covered tributaries above the impoundment
are still considered a tributary to downstream traditional navigable
waters, interstate waters, or the territorial seas even where the flow
of water might be impeded due to the impoundment. See paragraph (a)(5).
The agencies received comments on impoundments, which generally
explored the impacts of impoundments on connectivity to downstream
waters. For the reasons described above and in the Technical Support
Document, the agencies concluded that impoundments of ``waters of the
United States'' remain ``waters of the United States.''
F. Tributaries
The existing definition of ``waters of the United States''
regulates all tributaries without qualification. The final rule
protects only waters that have a significant effect on the integrity of
traditional navigable waters, interstate waters, or the territorial
seas. The rule establishes a definition of ``tributary,'' and provides
that a water meeting the definition of tributary, unless it is excluded
under paragraph (b), is a ``water of the United States'' without the
need for a separate case-specific significant nexus evaluation. As
explained in Section III above, covered tributaries and the functions
they provide, alone or in combination with other tributaries in the
watershed, significantly affect the chemical, physical, and biological
integrity of traditional navigable waters, interstate waters, or the
territorial seas. See also Technical Support Document. This section
describes the provisions of the rule addressing tributaries and changes
made to the provisions in the proposed rule based on public comments.
[[Page 37076]]
1. What are the provisions in the rule?
The rule defines ``tributary'' by emphasizing the physical
characteristics created by sufficient volume, frequency and duration of
flow, and that the water contributes flow, either directly or through
another water, to a traditional navigable water, interstate water, or
the territorial seas. This definition is based on the best available
science, intent of the CWA, and case law, and is consistent with
current practice. As mentioned above in Section III, the Science Report
concludes that ``[t]he scientific literature unequivocally demonstrates
that streams, individually or cumulatively, exert a strong influence on
the integrity of downstream waters.'' Science Report at ES-2.
First, to meet the rule's definition of ``tributary,'' a water must
flow directly or through another water or waters to a traditional
navigable water, interstate water, or the territorial seas. Waters
through which a tributary may contribute flow indirectly include, for
example, impoundments, wetlands, lakes, and other tributaries. A
tributary may contribute flow through any number of downstream waters,
including non-jurisdictional features, such as a ditch excluded under
paragraph (b) of the rule, and jurisdictional waters that are not
tributaries, such as an adjacent wetland--but it must be part of a
tributary system that eventually flows to a traditional navigable
water, an interstate water, or the territorial seas. This limitation on
what constitutes a tributary for purposes of this rule is fundamental.
If a water is not part of the tributary system of a traditional
navigable water, interstate water, or the territorial seas, it does not
meet the definition of ``tributary'' and is not jurisdictional under
this provision of the rule. For example, an intermittent stream that
exists wholly within one state, is not itself a traditional navigable
water, and whose flows eventually ends without connecting to a
traditional navigable water, interstate water, or the territorial seas
is not a ``water of the United States'' as a ``tributary'' for purposes
of this rule. To determine whether a water meets this aspect of the
definition, the connection can be traced using direct observation, U.S.
Geological Survey (USGS) data, stream datasets such as the National
Hydrography Dataset, aerial photography or other reliable remote
sensing information, or other appropriate information.
Under the rule, flow in the tributary may be perennial,
intermittent, or ephemeral. The agencies received comments suggesting
that the final rule provide definitions for the terms ephemeral flow,
intermittent flow, and perennial flow. The agencies considered the
request and determined that there was no need to include a definition
since they are commonly used scientific terms. Longstanding agencies'
practice considers perennial streams as those with flowing water year-
round during a typical year, with groundwater or contributions of flow
from higher in the stream or river network as primary sources of water
for stream flow. Intermittent streams are those that have both
precipitation and groundwater providing part of the stream's flow, and
flow continuously only during certain times of the year (e.g., during
certain seasons such as the rainy season). Ephemeral streams have
flowing water only in response to precipitation events in a typical
year, and are always above the water table. Precipitation can include
rainfall as well as snowmelt. Science shows that tributaries regardless
of flow duration are very effective at transporting pollutants
downstream, such as excess nutrients and sediment, which impact the
integrity and character of traditional navigable waters, interstate
waters, and the territorial seas. See Technical Support Document.
Second, the rule requires two physical indicators of flow: There
must be a bed and banks and an indicator of ordinary high water mark.
This definition of ``tributary'' includes only those waters the
agencies have concluded are the type of waters that the CWA was
intended to protect and which either individually or in combination
with other covered tributaries in the watershed have a significant
nexus to a traditional navigable water, interstate water, or the
territorial seas. Thus, the agencies are not defining ``waters of the
United States'' to include all streams that might be considered
``tributaries'' in the general scientific literature. To provide
additional clarity and for ease of use for the public, the agencies are
including the Corps' existing definition of ordinary high water mark in
EPA's regulations as well. Under that existing Corps regulation,
ordinary high water mark indicators include characteristics such as
shelving, scour, changes in soil characteristics, and destruction of
terrestrial vegetation, among others.
A bed and banks and other indicators of ordinary high water mark
are physical indicators of water flow and are only created by
sufficient and regular intervals of flow. These physical indicators can
be created by perennial, intermittent, and ephemeral flows. See
Technical Support Document. For purposes of the rule, ``bed and banks''
means the substrate and sides of a channel between which flow is
confined. The banks constitute a break in slope between the edge of the
bed and the surrounding terrain, and may vary from steep to gradual.
Existing Corps regulations define ordinary high water mark as the line
on the shore established by the fluctuations of water and indicated by
physical characteristics such as a clear, natural line impressed on the
banks, shelving, changes in the character of soil, destruction of
terrestrial vegetation, the presence of litter and debris, or other
appropriate means that consider the characteristics of the surrounding
areas. 33 CFR 328.3(e). That definition is not changed by the rule and
is added to EPA's regulations.
Current Corps regulations and guidance identify bed and banks as
indicators of the ordinary high water mark. The definition of
``tributary'' in this rule requires the presence of a bed and banks and
an additional indicator of ordinary high water mark such as staining,
debris deposits, or other indicator identified in the rule or agency
guidance. In many tributaries, the bed is that part of the channel
below the ordinary high water mark, and the banks often extend above
the ordinary high water mark. For other tributaries, such as those that
are incised, changes in vegetation, changes in sediment
characteristics, staining, or other ordinary high water mark indicators
may be found within the banks. In concrete-lined channels, the concrete
acts as the bed and banks and can have other ordinary high water mark
indicators such as staining and debris deposits. Indicators of an
ordinary high water mark may vary from region to region across the
country. See Technical Support Document.
Other evidence, besides direct field observation, may establish the
presence of bed and banks and another indicator of ordinary high water
mark. The agencies currently use many tools in identifying tributaries
and will continue to rely on their experience and expertise in
identifying the presence of a bed and banks and ordinary high water
mark. For example, several reliable, well-established remote sensing
sources of information or mapping can assist to establish the presence
of water that contributes flow to a traditional navigable water,
interstate water, or the territorial seas and provide evidence
regarding the presence of a bed and banks and another indicator of
ordinary high water mark. Among the types of remote sensing or mapping
information that can assist in establishing the presence of water are
USGS topographic
[[Page 37077]]
data, the USGS National Hydrography Dataset (NHD), Natural Resources
Conservation Service (NRCS) Soil Surveys, and State or local stream
maps, as well as the analysis of aerial photographs, and light
detection and ranging (also known as LIDAR) data, and desktop tools
that provide for the hydrologic estimation of a discharge sufficient to
create an ordinary high water mark, such as a regional regression
analysis or hydrologic modeling. These sources of information can
sometimes be used independently to infer the presence of a bed and
banks and another indicator of ordinary high water mark, or where they
correlate, can be used to reasonably conclude the presence of a bed and
banks and ordinary high water mark.
Both the USGS topographic data and the NHD data assist to delineate
tributaries to traditional navigable waters, interstate waters, or the
territorial seas. Where one or both of these sources have indicated a
``blue line stream,'' there is an indication that the tributary could
exhibit a bed and banks and another indicator of ordinary high water
mark. Where this information is combined with stream order,\11\ more
certainty can result. For example, a water that is a second-order
stream will be more likely to exhibit a bed and banks and another
indicator of ordinary high water mark as compared to a first-order
stream. This information will vary in validity in different parts of
the country, so care will be taken to evaluate additional information
prior to reasonably concluding a bed and banks or other indicators of
ordinary high water mark are associated with the stream. This will be
particularly true for first-order streams and for many streams in the
arid portions of the country. Supporting information that can be used
to conclude the presence of a bed and banks and another indicator of
ordinary high water mark would be the presence of USGS stream data on
the NRCS county Soil Survey or local stream maps which are mapped
independently of the USGS, aerial photography interpretation, or
digital terrain depictions created from LIDAR. See Technical Support
Document.
---------------------------------------------------------------------------
\11\ Stream order is a method for stream classification based on
relative position within a river network, when streams lacking
upstream tributaries (i.e., headwater streams) are first-order
streams and the junction of two streams of the same order results in
an increase in stream order (i.e., two first-order streams join to
form a second-order stream, and so on). When streams of different
orders join, the order of the larger stream is retained. See Science
Report and Technical Support Document.
---------------------------------------------------------------------------
Tributaries are observable in aerial photography by their
topographic expression, characteristic linear and curvilinear patterns,
dark photographic tones, and the presence and pattern of riparian
vegetation. The characteristic linear and curvilinear patterns and dark
photographic tones observed on aerial photography can be caused by
shadow cast from the banks of an incised stream or from water in the
stream channel itself. In some cases stream channel morphology is
visible, providing evidence of scour, materials sorting, and
deposition, all characteristics of an ordinary high water mark. Visible
persistent water (e.g., multiple dates of aerial photography showing
visible water) provides strong evidence of the sufficient frequency and
duration of surface flow to create a bed and banks and other indicators
of ordinary high water mark. Visible indicators of running water such
as rapids, riffles, and pools all indicate the presence of a bed and
banks and other indicators of ordinary high water mark. Other physical
characteristics of an ordinary high water mark that may be visible on
aerial photography include the destruction of terrestrial vegetation
and the absence of vegetation in a channel. These indicators gleaned
from aerial photography interpretation can be correlated with the
presence of USGS streams data in reasonably concluding that a bed and
banks and another indicator of ordinary high water mark are present.
See Technical Support Document.
Additional desktop tools can assist in the identification of bed
and banks and other indicators of ordinary high water mark. For
instance, field staff use other methods for estimating ordinary high
water mark, including, but not limited to, lake and stream gage data,
flood predictions, historic records of water flow, and statistical
evidence. Some desktop tools, such as a regional regression analysis
and the Hydrologic Modeling System (HEC-HMS), provide for the
hydrologic estimation of stream discharge sufficient to create an
ordinary high water mark in tributaries under regional conditions. Such
desktop tools are particularly useful for identifying presence of bed
and banks and another indicator of ordinary high water mark when
supported by additional remote sensing tools that indicate the presence
of such physical features.
LIDAR is a powerful tool to analyze the characteristics of the land
surface, including tributary identification and characterization. LIDAR
data are becoming more and more widespread for engineering and land use
planning purposes. Where LIDAR data have been processed to create a
bare earth model, detailed depictions of the land surface are
available. Bare earth models reveal subtle elevation changes and can
clearly show a tributary's bed and banks and channel morphology. In
many cases LIDAR can help delineate tributaries that would exhibit a
bed and banks and another indicator of an ordinary high water mark in
greater detail than aerial photography interpretation alone can.
Visible linear and curvilinear incisions on a bare earth model are
strong evidence that a tributary with a bed and banks and another
indicator of an ordinary high water mark is present. LIDAR-indicated
tributaries can be correlated with aerial photography interpretation
and USGS stream data, to reasonably conclude the presence of a bed and
banks and another indicator of an ordinary high water mark in the
absence of a field visit. See Technical Support Document. The agencies
have been using such remote sensing and desktop tools to delineate
tributaries for many years where data from the field are unavailable or
a field visit is not possible.
In addition, such desktop tools are critical in circumstances where
physical characteristics of bed and banks and another indicator of
ordinary high water mark are absent in the field, often due to
unpermitted alteration of streams. In such cases where physical
characteristics of bed and banks and another indicator of ordinary high
water mark no longer exist, they may be determined by using other
appropriate means that consider the characteristics of the surrounding
areas. Such reliable methods that can indicate prior existence of bed
and banks and other indicators of ordinary high water mark include, but
are not limited to, lake and stream gage data, elevation data, spillway
height, historic water flow records, flood predictions, statistical
evidence, the use of reference conditions, or through the remote
sensing and desktop tools described above.
The upper limit of the tributary is the point where a bed and banks
and another indicator of ordinary high water mark cease to be
identifiable. The ordinary high water mark establishes the lateral
limits of a water, and its absence generally determines when a
tributary's channel or bed and banks has ended, representing the upper
limit of the tributary. However, a natural or constructed break in bed
and banks or other indicator of ordinary high water mark does not
constitute the upper limit of a tributary where bed and banks or other
indicator ordinary high water mark can be found farther upstream. Note
that waters, including wetlands, which are adjacent to a tributary at
the
[[Page 37078]]
upper limit of the channel are jurisdictional as ``adjacent waters.''
The definition of ``tributary'' includes tributaries that flow
directly or indirectly through impoundments that are jurisdictional
under paragraph (a)(4) of the rule. Tributaries to impoundments of
``waters of the United States'' are jurisdictional for the same reasons
the impoundments themselves are jurisdictional. As discussed in section
IV. E., under case law, an impoundment of a ``water of the United
States'' remains a ``water of the United States,'' and scientific
literature demonstrates that impoundments continue to significantly
affect the chemical, physical, or biological integrity of downstream
waters traditional navigable waters, interstate waters, and the
territorial seas. Therefore, tributaries to such impoundments continue
to have a significant nexus, alone or in combination with other covered
tributaries in the watershed, to the downstream traditional navigable
water, interstate water, or the territorial seas.
Waters that meet the rule definition of tributary remain
tributaries even if there is a manmade or natural break at some point
along the connection to the traditional navigable water, interstate
water, or the territorial seas. In many tributaries, there are often
natural or constructed breaks in the presence of a bed and banks or
ordinary high water mark while hydrologic connectivity remains. For
example, in some regions of the country where there is a very low
gradient, the banks of a tributary may be very low or may even
disappear at times. Many tributaries lose their ordinary high water
mark when adjacent wetlands are contiguous with the stream channel. The
definition of ``tributary'' addresses these circumstances and states
that waters that meet the definition of tributary remain tributaries
even if such breaks occur, so long as bed and banks and an ordinary
high water mark are present upstream of the break. Under the rule, when
a covered tributary flows through a wetland into another tributary
(sometimes called a ``run-of-stream'' wetland), the covered tributary
remains jurisdictional even though it lost its ordinary high water mark
through the wetland. By looking to the presence of a bed and banks and
an ordinary high water mark upstream, the rule ensures that a mere
break in the ordinary high water mark does not render tributaries with
a significant nexus to downstream waters not jurisdictional. Other
breaks that do not sever jurisdiction include constructed breaks such
as bridges, culverts, pipes, dams, or waste treatment systems, or
natural breaks such as debris piles, boulder fields, or a stream that
flows underground so long as a bed and banks and an ordinary high water
mark can be identified upstream of the break. Site specific conditions
will continue to determine the distance up valley that needs to be
evaluated to see if the break in bed and banks and ordinary high water
mark is temporary or the start of the stream system.
The rule also clarifies that a water meets the definition of
tributary if the water contributes flow through an excluded feature
such as a ditch with ephemeral flow. While the water above and below
the excluded feature is jurisdictional if it meets the definition of
tributary, the excluded feature does not become jurisdictional. A water
also continues to meet the definition of tributary if at some point the
water contributes flow through a jurisdictional water that is not a
tributary, such as an adjacent wetland or impoundment.
The agencies' longstanding interpretation of the CWA has included
tributaries that are natural, modified, or constructed waters. While
this rule at paragraph (b) excludes specific types of constructed
waters from jurisdiction, it continues to interpret constructed
tributaries as jurisdictional unless expressly excluded in paragraph
(b). Natural, modified, and constructed tributaries provide many of the
same functions, especially as conduits for the movement of water and
pollutants to other tributaries or directly to traditional navigable
waters, interstate waters, or the territorial seas. The discharge of a
pollutant into a tributary generally has the same effect downstream
whether the tributary waterway is natural, modified, or constructed.
See discussion in section III.C. above and the Technical Support
Document. Given the extensive human modification of watercourses and
hydrologic systems throughout the country, it is often difficult to
distinguish between natural watercourses and watercourses that are
wholly or partly modified or constructed. For example, tributaries that
have been channelized in concrete or otherwise have been modified may
still meet the definition of tributaries under the rule so long as they
have bed and banks and an ordinary high water mark, contribute flow to
a traditional navigable water, interstate water, or the territorial
seas, and are not excluded under paragraph (b). The important
consideration for a modified or constructed water is whether it meets
the definition of ``tributary'' and is not excluded under paragraph
(b).
Ditches are one important example of constructed features that in
many instances can meet the definition of tributary. Ditches are
jurisdictional under the rule only if they both meet the definition of
``tributary'' and are not excluded under paragraph (b)(3) in the rule.
Not all ditches meet the definition of a tributary, and others--as
discussed in Section I--are expressly excluded from jurisdiction.
Ditches protected by the rule must meet the definition of
tributary, having a bed and banks and ordinary high water mark, and
contributing flow directly or indirectly through another water to a
traditional navigable water, interstate water, or the territorial seas.
Jurisdictional ditches include ditches such as the following:
Ditches with perennial flow,
Ditches with intermittent flow that are a relocated
tributary, or are excavated in a tributary, or drain wetlands,
Ditches, regardless of flow, that are excavated in or
relocate a tributary.
The definition of tributary includes natural, undisturbed waters
and those that have been man-altered or constructed, but which science
shows function as a tributary. In addition, alteration or modification
of natural streams and rivers for purposes such as flood control,
erosion control, and other reasons does not convert the tributary to a
ditch. A stream or river that has been channelized or straightened
because its natural sinuosity has been altered, cutting off the
meanders, is not a ditch. A stream that has banks stabilized through
use of concrete or rip-rap (e.g., rocks or stones) is not a ditch. The
Los Angeles River, for example, is a ``water of the United States''
(and, indeed, a traditional navigable water) and remains a ``water of
the United States'' and is not excluded under paragraph (b)(3) even
where it has been ditched, channelized, or concreted.
A ditch that relocates a stream is not an excluded ditch under
paragraph (b)(3), and a stream is relocated either when at least a
portion of its original channel has been physically moved, or when the
majority of its flow has been redirected. A ditch that is a relocated
stream is distinguishable from a ditch that withdraws water from a
stream without changing the stream's aquatic character. The latter type
of ditch is excluded from jurisdiction where it meets the listed
characteristics of excluded ditches under paragraph (b)(3). Agency
staff can determine historical presence of tributaries using a variety
of resources, such as historical maps, historic aerial photographs,
local surface water management plans, street
[[Page 37079]]
maintenance data, wetlands and conservation programs and plans, as well
as functional assessments and monitoring efforts. A ditch with
intermittent flow that drains a wetland and otherwise meets the
definition of ``tributary'' is a ``tributary'' and is not excluded
under paragraph (b)(3). See IV.I. below.
Evidence, such as current or historic photographs, prior
delineations, or USGS, state and local topographic maps, may be used to
determine whether a ditch is an excluded ditch. Site characteristics
may also be present to inform the determination of whether the water
body is a ditch, such as shape, sinuosity, flow indications, etc., as
ditches are often created in a linear fashion with little sinuosity and
may or may not connect to another ``water of the United States.''
2. What changes did the Agencies make from the proposed rule based on
public comments?
The rule's definition of ``tributary'' retains many elements from
the proposed rule, but reflects public comments in several important
ways. In particular, the rule emphasizes flow. The rule defines
``tributary'' by emphasizing physical characteristics created by water
flow and requiring that the water contributes flow, either directly or
through another water, to a traditional navigable water, interstate
water, or the territorial seas. The rule also is clearer regarding the
jurisdictional status of certain ditches, and clarifies that wetlands
and waters such as ponds and lakes that contribute flow to a
traditional navigable water, interstate water, or the territorial seas
but typically lack a bed and banks and ordinary high water mark are
considered ``adjacent'' but not a ``tributary.''
A number of commenters suggested that the agencies should exclude
ephemeral streams from the definition of tributary, expressing concern
that ephemeral waters that flow very rarely would be considered a
jurisdictional tributary. The rule definition of ``tributary'' requires
that flow must be of sufficient volume, frequency, and duration to
create the physical characteristics of bed and banks and an ordinary
high water mark. If a water lacks sufficient flow to create such
characteristics, it is not considered a ``tributary'' under this rule.
While some commenters expressed concern that a feature that flowed very
rarely could meet the proposed definition of ``tributary,'' it is the
agencies' judgment that such a feature is not a tributary under the
rule because it would not form the physical indicators required under
the definitions of ``ordinary high water mark'' and ``tributary.''
The rule includes ephemeral streams that meet the definition of
tributary as ``waters of the United States'' because the agencies
determined that such streams provide important functions for downstream
waters, and in combination with other covered tributaries in a
watershed significantly affect the chemical, physical, and biological
integrity of traditional navigable waters, interstate waters, and the
territorial seas. As noted by the SAB, and consistent with the
scientific literature, tributaries as a group exert strong influence on
the chemical, physical, and biological integrity of downstream waters,
even though the degree of connectivity is a function of variation in
the frequency, duration, magnitude, predictability, and consequences of
chemical, physical, and biological processes. See, e.g., SAB 2014b.
These significant effects on traditional navigable waters, interstate
waters, and the territorial seas occur even when the tributary is
small, intermittent, or ephemeral.
In addition, the Science Report concludes that, ``[a]lthough less
abundant, the available evidence for connectivity and downstream
effects of ephemeral streams was strong and compelling, particularly in
context with the large body of evidence supporting the physical
connectivity and cumulative effects of channelized flows that form and
maintain stream networks.'' Science Report at 6-13. For example,
ephemeral headwater streams shape river channels in traditional
navigable or interstate waters by accumulating and gradually or
episodically releasing stored materials such as sediment and large
woody debris. These materials help structure traditional navigable and
interstate river channels by slowing the flow of water through channels
and providing substrate and habitat for aquatic organisms.
Moreover, the agencies have historically considered ephemeral
tributaries to be ``waters of the United States.'' For example, for
many years EPA has reviewed and approved state water quality standards
for ephemeral waters under CWA section 303(c), several Corps'
Nationwide Permits under CWA section 404 address discharges of dredged
or fill material into ephemeral waters, and the agencies' definition of
``waters of the United States'' prior to this rule included all
tributaries without reference to flow regime.
Numerous commenters asked that the final rule define ``bed and
banks,'' which are physical characteristics called for under the
definition of tributary. Such commenters emphasized the importance of a
definition of ``bed and banks,'' and some suggested definitional
language. To increase clarity, the preamble in IV.F.1. above includes a
definition of bed and banks adapted largely from longstanding agencies'
practice as well as comments. Several commenters suggested that the
rule should add a definition of ``ordinary high water mark.'' In
response and to increase clarity, the rule adds the Corps' existing
regulatory ordinary high water mark definition to EPA's regulations.
Corps technical manuals are available to help identify ordinary high
water mark, referenced above. Several commenters suggested that the
agencies not require a tributary to have both bed and banks and
ordinary high water mark, because bed and banks are themselves an
indicator of ordinary high water mark, and because ordinary high water
mark alone is an appropriate criterion for many streams in the arid
west where the characteristic of bed and banks is less common. The
agencies based their significant nexus determination for the covered
tributaries in part on the amount of flow indicated where a tributary
has both a bed banks and another indicator of ordinary high water mark,
so the rule continues to require both physical indicators with the
preamble at IV.F.1. above clarifying the means to conclude that those
indicators exist.
Several commenters suggested that the rule exclude all constructed
waters from the definition of ``waters of the United States.'' While
the rule does exclude several types of constructed waters from
jurisdiction, it continues to consider constructed tributaries as
jurisdictional unless expressly excluded in paragraph (b) for the
reasons described in section IV.I. and the Technical Support Document.
Many comments recommended that wetlands, ponds, and lakes that
contribute flow to a traditional navigable water, interstate water, or
the territorial seas but lack a bed and banks and ordinary high water
mark not be considered as tributaries, because of the importance of
those physical characteristics to the definition. Wetlands typically
lack bed and banks and ordinary high water mark, while lakes and ponds
typically have an ordinary high water mark and a bed but may lack
banks. The proposed rule expressly sought comment on whether such
waters should be considered as tributaries or as ``adjacent waters,''
recognizing that it might add an element of uncertainty to the
definition of
[[Page 37080]]
``tributary'' to include waters that lacked the physical features
called for in the definition. In addition, the SAB commented that
tributaries are not typically defined to include lentic systems (still
waters), and suggested that the agencies reconsider including ponds,
lakes, and wetlands as covered adjacent waters instead of tributaries.
SAB 2014b at 2. In response, the rule does not consider these waters to
be tributaries, but defines covered adjacent waters to include
wetlands, lakes, and ponds that connect segments of tributaries or are
at the head of the tributary system. See section G for further
discussion.
G. Adjacent Waters
Section III above explains the basis for the agencies' conclusion
that covered adjacent waters have a significant nexus with
traditionally navigable waters, interstate waters, or the territorial
seas. The adjacency provision is based on the best available science,
intent of the CWA, and case law, and is consistent with the experience
of the agencies in making case-specific significant nexus
determinations. As discussed above in Section III, the SAB concludes,
``[t]he available science supports [the agencies'] proposal to include
adjacent waters and wetlands as waters of the United States.'' SAB
2014b at 2. This section describes the provisions of the rule governing
adjacent waters, changes made to the adjacent waters provision based on
comments on the proposed rule, and, finally, how science and the law
support the agencies' conclusions in the final rule.
1. What are the provisions of the rule?
Under the rule, ``adjacent'' means bordering, contiguous, or
neighboring, including waters separated from other ``waters of the
United States'' by constructed dikes or barriers, natural river berms,
beach dunes, and the like. Waters adjacent to a traditional navigable
water, interstate water, territorial sea, impoundment, or tributary,
are ``waters of the United States.'' For purposes of adjacency, an
adjacent water includes wetlands within or abutting its ordinary high
water mark. Adjacency is not limited to waters located laterally to a
traditional navigable water, interstate water, the territorial seas, an
impoundment, or a tributary. Therefore, waters that connect segments of
a traditional navigable water, interstate water, the territorial seas,
an impoundment, or a tributary or are located at the head of a
traditional navigable water, interstate water, the territorial seas, an
impoundment, or a tributary may be determined to be bordering,
contiguous, or neighboring, and thus adjacent. ``Adjacent waters''
include wetlands, ponds, lakes, oxbows, impoundments, and similar water
features. ``Adjacent waters'' do not include any water excluded under
paragraph (b) of the rule. Note also that a water that does not meet
the definition of ``adjacent waters'' may be determined to be a ``water
of the United States'' on a case-specific basis under paragraph (a)(8)
of the rule.
Within the definition of ``adjacent,'' the terms bordering and
contiguous are well understood, and for continuity and clarity the
agencies continue to interpret and implement those terms consistent
with the current policy and practice. Waters separated by a berm or
other similar feature remain ``adjacent'' under the definition.
Some waters included under the definition of ``tributary'' in the
proposed rule, after consideration of public comment, are ``adjacent''
in the final rule. Specifically, waters that connect segments of, or
are at the head of, a traditional navigable water, interstate water,
the territorial seas, an impoundment, or a tributary are adjacent to
that water. For example, a pond that is the source water to a tributary
and borders the tributary at its uppermost reach is jurisdictional as
an adjacent water. Further, the rule states that an adjacent water
includes wetlands within or abutting its ordinary high water mark. This
language is designed to ensure that if there is a fringe wetland
abutting that pond that is the source water to a tributary, that
wetland is considered part of the pond under the rule and such pond as
a whole, including any abutting wetlands, is jurisdictional as an
adjacent water.
For purposes of adjacency, including all three provisions of the
definition of ``neighboring,'' the entire water is adjacent if any part
of the water is bordering, contiguous or neighboring. Therefore, the
entire wetland is ``adjacent'' if any part of it is within the distance
thresholds established in the definition of ``neighboring.'' For
example, if a tributary has a 1,000 foot wide 100-year floodplain, then
a water that is located within 1,000 feet of the ordinary high water
mark of a covered tributary and extends to 2,000 feet is jurisdictional
in its entirety as ``neighboring.'' In addition, for purposes of
determining whether a water is ``adjacent'' artificial features (such
as roads) do not divide a water; rather, the water is treated as one
entire water.
The definition of ``adjacent'' in the rule does not include those
waters in which established, normal farming, silviculture, and ranching
activities occur. Wetlands and farm ponds in which normal farming
activities occur, as those terms are used in section 404(f) of the
Clean Water Act and its implementing regulations, are not
jurisdictional under the Act as an ``adjacent'' water. Waters in which
normal farming, ranching, and silviculture activities occur instead
will continue to be subject to case-specific review, as they are today.
These waters may be determined to have a significant nexus on a case-
specific basis under paragraph (a)(7) or (a)(8). Recognizing the vital
role of farmers in providing the nation with food, fiber, and fuel, the
Clean Water Act in Section 404(f) exempts many normal farming
activities such as seeding, harvesting, cultivating, planting, soil and
water conservation practices, and other activities from the Section 404
permitting requirement. ``Normal'' farming, ranching, and silviculture
is clarified in the agencies' implementing regulations to mean
established and ongoing activities to distinguish from activities
needed to convert an area to farming, silviculture, or ranching and
activities that convert a water to a non-water. 40 CFR 232.3(c)(1). The
rule reflects this framework by clarifying the waters in which the
activities Congress exempted under Section 404(f) occur are not
jurisdictional as ``adjacent.'' It is important to recognize that
``tributaries,'' including those ditches that meet the tributary
definition, are not ``adjacent'' waters and are jurisdictional by rule.
This provision interprets the intent of Congress and reflects the
intent of the agencies to minimize potential regulatory burdens on the
nation's agriculture community, and recognizes the work of farmers to
protect and conserve natural resources and water quality on
agricultural lands. While waters in which normal farming, silviculture,
or ranching practices occur may be determined to significantly affect
the chemical, physical, or biological integrity of downstream navigable
waters, the agencies believe that such determination should be made
based on a case-specific basis instead of by rule. The agencies also
recognize that waters in which normal farming, silviculture, or
ranching practices occur are often associated with modifications and
alterations including drainage, changes to vegetation, and other
disturbances the agencies believe should be specifically considered in
making a significant nexus determination.
The rule establishes a definition of ``neighboring'' for purposes
of determining adjacency. In the rule, the
[[Page 37081]]
agencies identify three circumstances under which waters would be
``neighboring'' and therefore ``waters of the United States.''
First, the term ``neighboring'' includes all waters located in
whole or in part within 100 feet of the ordinary high water mark of a
traditional navigable water, interstate water, the territorial seas, an
impoundment, or a covered tributary.
Second, the term ``neighboring'' includes all waters within the
100-year floodplain of a traditional navigable water, interstate water,
the territorial seas, an impoundment, or a covered tributary that is
located in whole or in part within 1,500 feet of the ordinary high
water mark of that jurisdictional water. In this rule, the agencies
interpret ``100-year floodplain'' to mean ``the area that will be
inundated by the flood event having a one percent chance of being
equaled or exceeded in any given year.'' This is consistent with the
Federal Emergency Management Agency's (FEMA) definition of ``100-year
flood.'' If the 100-year floodplain is greater than 1,500 feet from the
ordinary high water mark, only those waters that are located in whole
or in part within 1,500 feet of the ordinary high water mark are
``neighboring.'' In addition, if the 100-year floodplain is less than
1,500 feet from the ordinary high water mark, only those waters located
in whole or in part within the floodplain are ``neighboring'' under
this provision.
Third, the rule defines ``neighboring'' to include all waters
located in whole or in part within 1,500 feet of the high tide line of
a traditional navigable water or the territorial seas, and all waters
located within 1,500 feet of the ordinary high water mark of the Great
Lakes. This provision defines waters that begin within 1,500 feet of a
tidally-influence traditional navigable water or the territorial seas
and waters within 1,500 feet of the ordinary high water mark of the
Great Lakes as ``waters of the United States.'' To provide clarity for
this aspect of the definition, the agencies incorporated the Corps'
existing definition of high tide line into EPA's regulations at
paragraph (c)(7) in the rule.
As noted above, the rule provides that with respect to the
boundaries for covered adjacent waters the entire water is
jurisdictional as long as the water is at least partially located
within the distance threshold, and the agencies interpret the rule to
apply to any single water or wetland that may straddle a distance
threshold. Low-centered polygonal tundra and patterned ground bogs
(also called strangmoor, string bogs, or patterned ground fens) are
considered a single water for purposes of the rule because their small,
intermingled wetland and non-wetland components are physically and
functionally integrated. These areas often have complex micro-
topography with repeated small changes in elevation occurring over
short distances. Science demonstrates that these wetlands function as a
single wetland matrix having clearly hydrophytic vegetation, hydric
soils, and wetland hydrology. As a result, the agencies will continue
to evaluate these wetlands as a single water under the rule. Where any
portion of these wetland types is bordering, contiguous or neighboring,
the entire wetland is a ``water of the United States.'' Similarly, for
purposes of a case-specific determination under paragraph (a)(8),
wetlands of these types constitute a single water when making a
significant nexus determination. Other wetlands may also have
intermingled wetland and non-wetland components that are so physically
and functionally integrated they can be considered a single water for
purposes of the rule. Groups of wetlands that are simply part of a
complex of wetlands would not be considered a single water for purposes
of the rule.
The final rule also makes some ministerial changes to the
definition of ``adjacent.'' The existing regulation defined
``adjacent'' to mean ``bordering, contiguous, or neighboring,'' and had
a second sentence that clarified that wetlands separated by berms and
the like remain adjacent wetlands. The final rule combines those
sentences without changing the scope of adjacency.
When determining the jurisdictional boundaries under the CWA for
``adjacent waters,'' the agencies will rely on published FEMA Flood
Zone Maps to identify the location and extent of the 100-year
floodplain. https://msc.fema.gov/portal. These maps are publicly
available and provide a readily accessible and transparent tool for the
public and agencies to use in locating the 100-year floodplain. It is
important to recognize, however, that much of the United States has not
been mapped by FEMA and, in some cases, a particular map may be out of
date and may not accurately represent existing circumstances on the
ground. The agencies will determine if a particular map is no longer
accurate based on factors, such as streams or rivers moving out of
their channels with associated changes in the location of the
floodplain. In the absence of applicable FEMA maps, or in circumstances
where an existing FEMA map is deemed by the agencies to be out of date,
the agencies will rely on other available tools to identify the 100-
year floodplain, including other Federal, State, or local floodplain
maps, Natural Resources Conservation Service (NRCS) Soil Surveys
(Flooding Frequency Classes), tidal gage data, and site-specific
modeling (e.g., Hydrologic Engineering Centers River System Analysis
System or HEC-RAS). https://websoilsurvey.sc.egov.usda.gov/App/HomePage.htm and HEC-RAS and https://www.hec.usace.army.mil/software/hec-ras/. Additional supporting information can include historical
evidence, such as photographs, prior delineations, topographic maps,
and existing site characteristics. Because identifying the 100-year
floodplain is an important aspect of establishing jurisdiction under
the rule and the reliable and appropriate tools for identifying the
100-year floodplain may vary, the agencies will coordinate with other
federal and state agencies to develop additional information for EPA
and Corps field staff to further improve tools for identifying the 100-
year floodplain in a consistent, predictable, and scientifically valid
manner.
When determining the outer distance threshold for an ``adjacent
water'' the line is drawn perpendicular to the ordinary high water mark
or high tide line of the traditional navigable water, interstate water,
the territorial seas, impoundment, or covered tributary and extended
landward from that point. If there are breaks in the ordinary high
water mark, the line should be extrapolated from the point where the
ordinary high water mark is observed on the downstream side to the
point where the ordinary high water mark is lost on the upstream side.
Therefore, waters may meet the definition of neighboring even where,
for example, a tributary temporarily flows underground.
The agencies emphasize that they fully support efforts by States
and tribes to protect under their own laws any additional waters,
including locally special waters that may not be within the Federal
protections of the CWA as the agencies have interpreted its scope in
this rule. In promulgating the adjacent water boundaries, the agencies
have balanced protection and clarity, scientific uncertainties and
regulatory experience, and established boundaries that are, in their
judgment, reasonable and consistent with the statute and its goals and
objectives.
If waters identified in this section are determined to be adjacent,
no case-specific significant nexus evaluation is required.
[[Page 37082]]
2. What changes did the agencies make from the proposed rule based on
public comments?
In the proposal, the agencies sought comment on a number of ways to
address and clarify jurisdiction over ``adjacent waters,'' including
establishing a floodplain interval and providing clarity on reasonable
proximity as an important aspect of adjacency. In light of the
comments, the science, the agencies' experience, and the Supreme
Court's consistent recognition of the agencies' discretion to interpret
the bounds of CWA jurisdiction, the agencies have made some revisions
in the final rule designed to more clearly establish boundaries on the
scope of ``adjacent waters.''
Under the proposal and the final rule, ``adjacent waters'' are
jurisdictional based on the conclusion that they have a significant
nexus to traditional navigable waters, interstate waters, or the
territorial seas, and there is no need for additional analysis. Some
commenters wanted a case-specific analysis for all ``adjacent waters''
as they believed that the waters would not individually have a
significant nexus to an adjacent ``water of the United States,'' while
others noted that their functional relationship to the downstream
traditional navigable waters, interstate waters, or the territorial
seas warranted the conclusion that they were all jurisdictional. Based
on a review of the science, the agencies' expertise and experience, and
the law, the agencies determined that ``adjacent waters,'' as defined,
alone or in combination with other covered ``adjacent waters'' in a
watershed have a significant nexus to a traditional navigable water,
interstate water or the territorial seas and therefore are ``waters of
the United States'' without the need for any additional analysis.
However, the rule also provides for case-specific analysis of some
waters that do not meet the definition of ``neighboring'' established
by the rule. See section IV.H.
The proposal included wetlands, ponds, lakes, and impoundments that
contribute flow, directly or indirectly, to the downstream traditional
navigable waters, interstate waters, or the territorial seas in the
definition of ``tributary.'' Some commenters expressed concern that
since such waters generally do not have both an ordinary high water
mark and a bed and banks, the definition of tributary was contradictory
and confusing. The agencies sought comment on whether to treat these
waters as ``adjacent waters'' instead of tributaries, since they not
only contribute flow, but they also border or are contiguous to the
waters to which they contribute flow. The SAB in particular commented
that the agencies ``may want to consider whether flow-through lentic
systems should be included as ``adjacent waters'' and wetlands, rather
than as tributaries.'' SAB 2014b at 2. In light of the comments and to
provide additional clarity, the agencies revised the definitions of
``adjacent'' and ``tributary'' to include these waters as ``adjacent.''
Under the existing rule, there is no definition for the term
``neighboring,'' and the public commented that not having a definition
created a lack of clarity and inconsistent field practices across the
nation. In the proposal, ``neighboring'' was defined to include waters
located within the riparian area or floodplain of a traditional
navigable water, interstate water, territorial sea, impoundment, or
tributary; waters with a shallow subsurface hydrologic connection to a
jurisdictional water; and waters with a confined surface hydrologic
connection to a jurisdictional water. Although the definitions were
scientifically-based for the terms ``riparian area'' and ``floodplain''
to define the lateral reach of the term ``neighboring,'' some
commenters indicated that the proposed definitions to clarify
neighboring were not clear. Those commenters requested that a specific
floodplain interval or other limitation should be established to more
clearly identify the outer limit of neighboring. Some commenters stated
that the proposed definition of ``neighboring'' was unclear, while
other commenters found the definition helped clarify CWA jurisdiction
and were supportive of including a broad definition, based on
ecological interconnectedness.
Some commenters stated that the proposed definitions of ``riparian
area'' and ``floodplain'' were vague or ambiguous, broad or effectively
limitless, beyond the agencies' authority or difficult or impossible to
implement in the field. Other commenters were supportive of using the
riparian area as a basis for adjacency. Some commenters asked why the
agencies were proposing a new definition of ``floodplain'' that was
inconsistent with the definition used by other Federal agencies like
NRCS or FEMA. Some commenters suggested that if the agencies use
floodplains as a means to define ``neighboring,'' it should be limited
to the area inundated by the 2-year, 5-year, 10-year, or 20-year flood,
while other commenters supported the use of the 100-year floodplain as
a component of ``neighboring.'' Some commenters supported including all
wetlands and other waters in the 100-year floodplain as categorically
jurisdictional. Other commenters requested that floodplain size be
based on tributary size, while others suggested that it should be based
on soil and geologic features, and some suggested the use of the FEMA
flood zone maps. Some commenters stated that ``reasonable proximity''
was neither defined nor clarified adjacency, noting that adjacency
should not apply to waters separated from a ``water of the United
States'' by great distances.
In response to comments and to provide greater clarity and
consistency, in the rule the agencies establish a definition of
neighboring which provides additional specificity requested by some
commenters, including establishing a floodplain interval and providing
specific boundaries from traditional navigable waters, interstate
waters, the territorial seas, impoundments, and tributaries. In the
proposal, the agencies requested comment on whether the rule should
provide greater specificity with regard to how the agencies will
determine if a water is located in the floodplain of a jurisdictional
water. 79 FR 22209. As recommended by the public and based on science,
the agencies' boundaries for ``neighboring'' are based largely on use
of the 100-year floodplain. The agencies concluded that the use of the
riparian area was unnecessarily complicated and that as a general
matter, waters in the riparian area will also be in the 100-year
floodplain. Further, should the riparian area on occasion extend beyond
the 100-year floodplain, the agencies have the ability to perform a
case-specific significant nexus analysis on a water out to 4,000 feet
from the ordinary high water mark or high tide line of a traditional
navigable water, interstate water, the territorial sea, impoundment, or
tributary. The agencies have drawn these lines based on their technical
expertise and experience in order to provide a rule that is practical
to understand and implement and protects those waters that
significantly affect the chemical, physical, or biological integrity of
traditional navigable waters, interstate waters, or the territorial
seas. Because science indicates that connectivity is on a gradient, the
agencies have also identified limited circumstances in which waters
that do not meet the definition of ``neighboring'' may be determined on
a case-specific basis to have a significant nexus. See section IV.I.
First, the rule establishes as ``neighboring'' waters that occur
within 100 feet from traditional navigable
[[Page 37083]]
waters, interstate waters, the territorial seas, impoundments, and
tributaries.
Second, the rule utilizes a specific floodplain and also
establishes maximum distances for purposes of ``neighboring.'' Studies
have found that waters within the floodplain are dynamically connected
and frequently interact with the downstream traditional navigable
water, interstate water, territorial sea, impoundment, or tributary.
Some commenters indicated that a specific floodplain or other
designation should be set to define the outer boundary of
``neighboring.'' Further, some commenters requested that the 100-year
floodplain designation be used to define the outer boundary of
adjacency because the public understands this concept. Several
commenters recommended that FEMA or NRCS maps be used to support the
analysis as these maps are easily accessible to the public. Because
FEMA maps exist for many areas of the country and the NRCS Soil Survey
maps do as well, the agencies decided that defining ``neighboring''
based in part on a particular floodplain or recurrence interval was a
reasonable means of ensuring the consistency and certainty that is
important to the public and for implementation of the CWA. In drawing
lines, the agencies chose the 100-year floodplain in part because FEMA
and NRCS together have generally mapped large portions of the United
States, and these maps are publicly available, well-known and well-
understood.
Because the 100-year floodplain can be very wide in some areas of
the country, particularly near large rivers, the agencies chose to
provide increased clarity and certainty while ensuring that waters that
provide important functions significantly affecting the chemical,
physical, and biological integrity of the downstream traditional
navigable waters, interstate waters, or the territorial seas are
protected by establishing a 1,500 foot maximum distance for neighboring
waters in the rule. Waters within the 100-year floodplain to a maximum
of 1,500 feet of the ordinary high water mark are adjacent without
regard to the presence of berms or other barriers. However, because the
science demonstrates that floodplain waters provide important functions
for downstream waters, the agencies have established a provision under
paragraph (a)(8) for case-specific significant nexus evaluations of
waters located in the 100-year floodplain of a traditional navigable
water, interstate water, or the territorial seas beyond 1,500 feet.
The rule also establishes a separate bright line for including as
jurisdictional those waters that occur within 1,500 feet of tidally-
influenced traditional navigable waters or the territorial seas.
The proposal defined ``neighboring'' to include waters with a
surface connection to jurisdictional waters and some commenters
recommended eliminating surface hydrologic connectivity as a basis for
adjacency. The definition of neighboring does not include a provision
defining ``neighboring'' based on a surface hydrologic connection.
However, waters with confined surface hydrologic connections are
considered adjacent where they are bordering, contiguous, or
neighboring a traditional navigable water, interstate water, the
territorial seas, impoundment, or covered tributary. For example, a
water with a confined surface hydrologic connection to a traditional
navigable water that is 1,200 feet from the high tide line of that
water would meet the definition of neighboring and be considered an
adjacent water. In circumstances where a water does not meet the
definition of neighboring but is located within the 100-year floodplain
of a traditional navigable water, interstate water, or the territorial
seas, or within 4,000 feet of a jurisdictional water, a confined
surface hydrologic connection may be an important factor in evaluating
a case-specific significant nexus under paragraph (a)(8). See section
H. below.
The proposal defined ``neighboring'' to include waters connected
with a shallow subsurface connection, and some commenters recommended
eliminating subsurface hydrologic connectivity as a basis for
adjacency. For example, some commenters asserted that, because the CWA
does not apply to groundwater, the agencies do not have the authority
to assert jurisdiction over waters connected to other ``waters of the
United States'' via a shallow subsurface hydrologic connection. Some
commenters were concerned that the distinction between ``groundwater''
and a ``shallow subsurface connection'' was unclear and questioned
whether using a shallow subsurface connection as a basis for adjacency
is contradictory to excluding groundwater--including groundwater
drained through subsurface drainage systems--as a ``water of the United
States.'' Some commenters supported use of shallow subsurface
connectivity for adjacency, since the significant nexus test would be
employed to make the determination of jurisdiction. Several commenters
suggested that the rule should protect groundwater and shallow
subsurface flow, due to its connectivity to other ``waters of the
United States'' and particularly since altering it could affect the
downstream waters. A few commenters simply requested clarifications
regarding issues such as how to determine whether a subsurface
connection exists; the meaning of ``shallow;'' distinguishing between
``shallow'' and ``deep;'' whether there were any boundaries on
adjacency via hydrologic connectivity; and determining whether the
connection was ``sufficient'' to establish adjacency. In order to
provide more certainty to the public, the rule does not include a
provision defining neighboring based on shallow subsurface flow, though
such flow may be an important factor in evaluating a water on a case-
specific basis under paragraph (a)(8), as appropriate.
Some commenters expressed concern that the agencies' proposed
definition of ``neighboring,'' ``riparian area,'' and ``floodplain''
would mean that all land within the floodplain or riparian area would
become regulated. In fact, only waters, not land, in the floodplain or
riparian area would have been considered adjacent under the proposed
rule. Similarly, under the final rule, only waters, not land, are
adjacent. In response, the agencies have eliminated the definitions of
floodplain and riparian area and have provided a definition of
neighboring which is clear that only waters in specified circumstances
may be ``waters of the United States.''
The agencies also eliminated a parenthetical from the existing
``adjacent wetlands'' regulatory provision. The phrase ``other than
waters that are themselves wetlands'' was intended to preclude
asserting CWA jurisdiction over wetlands that were simply adjacent to a
non-jurisdictional wetland. Such waters do not meet the definition of
``adjacent'' under the rule since waters must be adjacent to a
traditional navigable water, interstate water, the territorial seas,
impoundment, or covered tributary, so the phrase is unnecessary and
confusing. With this change, the agencies are protecting all waters
that meet the definition of ``adjacent'' as ``waters of the United
States,'' and eliminating confusion caused by the parenthetical. For
example, where the 100-year floodplain is greater than 1,500 feet, all
wetlands within 1,500 feet of the tributary's ordinary high water mark
are jurisdictional because they are ``neighboring'' to the tributary,
regardless of the wetlands' position relative to each other.
Some commenters stated that the proposed rule was an expansion of
jurisdiction because it would change the
[[Page 37084]]
provision from ``adjacent wetlands'' to ``adjacent waters.'' The
agencies acknowledge that under the existing regulation, the adjacency
provision applied only to wetlands adjacent to ``waters of the United
States.'' However, also under the existing regulation, ``other waters''
(such as intrastate rivers, lakes and wetlands that are not otherwise
jurisdictional under other sections of the rule) could be determined to
be jurisdictional if the use, degradation or destruction of the water
could affect interstate or foreign commerce. This provision of the
existing regulation reflected the agencies' interpretation at the time
of the jurisdiction of the CWA to extend to the maximum extent
permissible under the Commerce Clause of the Constitution. Therefore,
while the language of the specific adjacency provision in the final
rule may have changed from wetlands to waters, that does not represent
an expansion of jurisdiction as a whole in comparison to the existing
regulation, since adjacent non-wetland waters would have been subject
to jurisdiction under the ``other waters'' provision. The final rule
does not protect all waters that were protected under the ``other
waters'' provision of the existing regulation, and therefore the
inclusion of adjacent ponds, for example, in the ``adjacent waters''
provision of the final rule does not reflect an overall expansion of
jurisdiction when compared to the existing regulation.
3. How do science and law support the rule?
Based on a review of the scientific literature and the agencies'
expertise and experience the agencies determined that the categories of
waters discussed below are integrally linked to the chemical, physical,
or biological functions of waters to which they are adjacent and
downstream to the traditional navigable waters, interstate waters or
the territorial seas. Therefore, the agencies determined that the
waters defined as adjacent have a significant nexus with traditional
navigable waters, interstate waters or the territorial seas and are
thus ``waters of the United States.'' Additional information, including
citations, can be found in section III of the preamble, the Science
Report, and the Technical Support Document for the rule.
a. Waters that are Bordering or Contiguous
As discussed in section III above, wetlands, ponds, lakes, oxbows,
impoundments, and similar water features that are bordering or
contiguous perform a myriad of critical chemical and biological
functions associated with the downstream traditional navigable waters,
interstate waters, or the territorial seas. Such waters are integrally
linked with the jurisdictional waters to which they are adjacent.
Because of their close physical proximity to nearby jurisdictional
waters, bordering or contiguous waters readily exchange their waters
through the saturated soils surrounding the traditional navigable
water, interstate water, the territorial seas, impoundment, or covered
tributary or through surface exchange. This commingling of waters
allows bordering or contiguous waters to both provide chemically
transformed waters to streams and to absorb excess stream flow, which
in turn can significantly affect downstream traditional navigable
waters, interstate waters, or the territorial seas. The close proximity
also allows for the direct exchange of biological materials, including
organic matter that serves as part of the food web of downstream
traditional navigable waters, interstate waters, or the territorial
seas. Waters that are bordering or contiguous are often located on the
floodplain or within the riparian area of the waters to which they are
adjacent. Bordering or contiguous waters include those that directly
abut a traditional navigable water, interstate water, the territorial
seas, impoundment, or covered tributary. The Science Report and the
Technical Support Document demonstrate that such waters are physically,
chemically, and biologically integrated with downstream traditional
navigable waters, interstate waters, or the territorial seas and
significantly affect their integrity.
b. Waters Separated From Other ``Waters of the United States'' by
Constructed Dikes or Barriers, Natural River Berms, Beach Dunes and the
Like
Adjacent waters separated from a traditional navigable water,
interstate water, the territorial seas, impoundment, or covered
tributary by constructed dikes or barriers, natural river berms, beach
dunes, and the like continue to have a significant effect on downstream
traditional navigable waters, interstate waters, or the territorial
seas, either alone or in combination with other ``adjacent waters.''
Such waters continue to have a hydrologic connection to downstream
waters. This is because constructed dikes or barriers, natural river
berms, beach dunes, and the like typically do not block all water flow.
This hydrologic connection can occur via seepage, or the flow of water
through the soil pores, or via over-topping, where water from the
nearby traditional navigable water, interstate water, the territorial
seas, impoundment, or covered tributary periodically overtops the berm
or other similar feature. Berm-like landforms known as natural levees
occur naturally and do not isolate adjacent wetlands from the streams
that form them. Natural levees and the wetlands and waters behind them
are part of the floodplain. Natural levees are discontinuous, which
allows for a hydrologic connection to the stream or river via openings
in the levees and thus the periodic mixing of river water and
backwater. Man-made levees and similar structures also do not isolate
``adjacent waters.'' Waters, including wetlands, separated from a
jurisdictional water by a natural or man-made berm serve many of the
same functions as other ``adjacent waters.'' Furthermore, even in cases
where a hydrologic connection may not exist, there are other important
considerations, such as chemical and biological functions, that result
in a significant nexus between the adjacent wetlands or waters and the
nearby ``waters of the United States,'' and traditional navigable
waters, interstate waters, or the territorial seas. On this point,
Justice Kennedy stated: ``In many cases, moreover, filling in wetlands
separated from another water by a berm can mean that floodwater,
impurities, or runoff that would have been stored or contained in the
wetlands will instead flow out to major waterways. With these concerns
in mind, the Corps' definition of adjacency is a reasonable one, for it
may be the absence of an interchange of waters prior to the dredge and
fill activity that makes protection of the wetlands critical to the
statutory scheme.'' Rapanos at 775. For instance, covered adjacent
waters behind berms can still serve important water quality functions,
serving to filter pollutants and sediment before they reach downstream
waters. Wetlands and open waters behind berms, where the system is
extensive, can help reduce the impacts of storm surges caused by
hurricanes. Such ``adjacent waters,'' including wetlands, separated
from waters by berms and the like maintain ecological connection with
those waters. It is not the existence of the dike, levee, and the like
that makes these waters jurisdictional. Adjacent waters separated from
the tributary network by constructed dikes or barriers, natural river
berms, beach dunes, and the like continue to have a hydrologic
connection to downstream waters.
[[Page 37085]]
Waters behind berms and the like can significantly affect the chemical,
physical, and biologic integrity of traditional navigable waters,
interstate waters, or the territorial seas.
c. Waters Within 100 Feet
All wetlands, ponds, lakes, oxbows, impoundments, and similar water
features that are located in whole or in part within 100 feet of the
ordinary high water mark of a jurisdictional water perform a myriad of
critical chemical, physical, and biological functions associated with
the downstream traditional navigable water, interstate water or the
territorial seas and therefore the agencies have determined that they
are ``neighboring'' and thus ``waters of the United States.'' Waters
within 100 feet of a jurisdictional water are often located within the
riparian area and are often connected via surface and shallow
subsurface hydrology to the water to which they are adjacent. While the
SAB was clear that distance is not the only factor that influences
connections and their effects downstream, due to their close proximity
to jurisdictional waters, waters within 100 feet are often located
within a landscape position that allows for them to receive and process
surface and shallow subsurface flows before they reach streams and
rivers. These waters individually and collectively affect the integrity
of downstream waters by acting primarily as sinks that retain
floodwaters, sediments, nutrients, and contaminants that could
otherwise negatively impact the condition or function of downstream
waters. Wetlands and open waters within close proximity of
jurisdictional waters improve water quality through assimilation,
transformation, or sequestration of nutrients, sediment, and other
pollutants that can affect the integrity of downstream traditional
navigable waters, interstate waters, or the territorial seas. These
waters, including wetlands, also provide important habitat for aquatic-
associated species to forage, breed, and rest.
In order to provide greater clarity and consistency and based on a
review of the science and the agencies' expertise and experience, the
agencies identified a 100 foot threshold for neighboring waters to a
traditional navigable water, interstate water, territorial sea,
tributary, or impoundment. Further, the agencies determined that there
is a significant nexus with the downstream traditional navigable
waters, interstate waters, or the territorial seas, and these
``adjacent waters'' are ``waters of the United States.'' With respect
to provision of water quality benefits downstream, non-floodplain
waters within close proximity of the stream network often are able to
have more water quality benefits than those located at a distance from
the stream. Many studies indicate that the primary water quality and
habitat benefits will generally occur within a several hundred foot
zone of a water. In addition, the scientific literature indicates that
to be effective, contaminant removal needs to occur at a reasonable
distance prior to entry into the downstream traditional navigable
waters, interstate waters, or the territorial seas. Some studies also
indicate that fish, amphibians (e.g., frogs, toads), reptiles (e.g.,
turtles), and small mammals (e.g., otters, beavers, etc.) will use at
least a 100 foot zone for foraging, breeding, nesting, and other life
cycle needs.
Based on a review of the scientific literature and the agencies'
expertise and experience, there is clear evidence that the identified
waters within 100 feet of the ordinary high water mark of a
jurisdictional water, even when located outside the floodplain, perform
critical processes and functions discussed in section III above. All
waters within 100 feet of a jurisdictional water significantly affect
the chemical, physical, or biological integrity of the waters to which
they are adjacent, and those waters in turn significantly affect the
chemical, physical, or biological integrity of the downstream
traditional navigable waters, interstate waters, or the territorial
seas. The agencies established a 100 foot threshold from the water's
lateral limit in the definition of neighboring because, based on the
agencies' expertise and experience implementing the CWA and in light of
the science, the agencies concluded this was a reasonable and practical
boundary within which to conclude the waters clearly significantly
affected the integrity of traditional navigable waters, interstate
waters, or the territorial seas, and these ``adjacent waters'' are
``waters of the United States.''
d. Floodplain Waters Within 1,500 Feet
As discussed in section III above, wetlands and open waters that
are neighboring perform a myriad of critical chemical and biological
functions associated with the downstream traditional navigable waters,
interstate waters, or the territorial seas. The scientific literature
supports that wetlands and open waters in floodplains are chemically,
physically, and biologically connected to downstream traditional
navigable waters, interstate waters, or the territorial seas and
significantly affect the integrity of such waters. The Science Report
concludes that wetlands and open waters located in ``floodplains are
physically, chemically and biologically integrated with rivers via
functions that improve downstream water quality, including the
temporary storage and deposition of channel-forming sediment and woody
debris, temporary storage of local ground water that supports baseflow
in rivers, and transformation and transport of stored organic matter.''
Science Report at ES-2 to ES-3. Such waters act as the most effective
buffer to protect downstream waters from nonpoint source pollution
(such as nitrogen and phosphorus), provide habitat for breeding fish
and aquatic insects that also live in streams, and retain floodwaters,
sediment, nutrients, and contaminants that could otherwise negatively
impact the condition or function of downstream waters.
For waters in the 100-year floodplain within 1,500 feet of the
ordinary high water mark of a traditional navigable water, interstate
water, the territorial seas, impoundment, or covered tributary, the
agencies determine there is a significant nexus with the downstream
traditional navigable waters, interstate waters, or the territorial
seas and these waters are critical to protect the downstream waters.
Based on a review of the scientific literature, the agencies' technical
expertise and experience, and the implementation value of drawing clear
lines, the rule establishes a boundary for floodplain waters to meet
the definition of ``neighboring'' and be ``waters of the United
States'' by rule. This boundary was established in order to protect
vitally important waters within a watershed while at the same time
providing a practical and implementable rule. The agencies are not
determining that waters in the floodplain farther than 1,500 feet from
the ordinary high water mark never have a significant nexus. Rather,
the agencies are using their technical expertise to promulgate a
practical rule that draws reasonable boundaries in order to protect the
waters that most clearly have a significant nexus while minimizing
uncertainty about the scope of ``waters of the United States.'' Because
waters beyond these boundaries may have a significant nexus, the rule
also establishes areas in which a case-specific significant nexus
determination must be made. See section IV.H.
e. Waters Within 1,500 Feet of Tidally-Influenced Traditional Navigable
Waters or the Territorial Seas or the Great Lakes
Many tidally-influenced waters do not have floodplains, so the
agencies
[[Page 37086]]
include a separate provision within the definition of ``neighboring''
to protect the ``adjacent'' waters that have a significant nexus to
tidally-influenced traditional navigable waters or the territorial seas
or the Great Lakes. Under Riverside Bayview and Justice Kennedy's
opinion in Rapanos, waters adjacent to traditional navigable waters,
including the territorial seas, are ``waters of the United States.''
Because the connection to a tidally-influenced traditional navigable
water, the territorial seas, or the Great Lakes is so close, the rule
defines ``neighboring'' to include waters within 1,500 feet of the high
tide line or the ordinary high water mark of the Great Lakes. Wetlands,
ponds, lakes, oxbows, impoundments, and similar water features within
1,500 feet of these waters are physically connected to such waters by
surface and shallow subsurface flow. As demonstrated in section III
above, these waters perform a myriad of critical chemical and
biological functions associated with these nearby waters to which they
are adjacent.
These waters in combination significantly affect the integrity of
the connected tidally influenced traditional navigable water or the
territorial seas or the Great Lakes by acting primarily as sinks that
retain floodwaters, sediments, nutrients, and contaminants that could
otherwise negatively impact the condition or function of those waters.
Like floodplain waters, the scientific literature supports that
wetlands and other similar waters within close proximity improve water
quality through assimilation, transformation, or sequestration of
nutrients, sediment, and other pollutants that can affect downstream
water quality. These waters also provide important habitat for aquatic-
associated species to forage, breed, and rest in.
For example, wetlands dominated by grass-like vegetation that occur
in depressional areas between sand dunes or beach ridges along the
territorial seas and the Great Lakes shoreline are dependent upon these
waters for their water source. The waters, including wetlands,
generally form when water levels of the territorial seas fall or the
Great Lakes drop, creating swales that support a diverse mix of wetland
vegetation and many endangered and threatened species. Many studies
demonstrate that these waters have been shown to act in concert with
the rising and lowering of the tide, and that the critical functions
provided by these waters are similar and play an important role in
maintaining the chemical, physical, or biological integrity of the
nearby traditional navigable waters, interstate waters, or the
territorial seas because of the hydrological and ecological connections
to and interactions with those waters.
Science demonstrates that distance is a factor in the connectivity
and the strength of connectivity of wetlands and open waters to
downstream waters. Thus, waters that are more distant generally have
less opportunity to be connected to downstream waters. Wetlands and
open waters closer to the stream network generally will have greater
hydrologic and biological connectivity than waters located farther from
the same network. For instance, waters that are more closely proximate
have a greater opportunity to contribute flow. Via their hydrologic
connectivity, they also have chemical connectivity to and effects on
these downstream waters and are more likely to impact water quality due
to their close distance. Waters more closely located to these waters
are also more likely to be biologically connected to such waters more
frequently and by more species, including amphibians and other aquatic
animals. Because tidally-influenced traditional navigable waters, the
territorial seas, and the Great Lakes are generally much larger in size
than other jurisdictional waters, the agencies believe that a 1,500
foot threshold is a reasonable distance to capture most wetlands and
open waters that are so closely linked to these waters that they can
properly be considered adjacent as neighboring waters.
Based on a review of the scientific literature and the agencies'
expertise and experience, there is clear evidence waters within 1,500
feet of these waters, even when located outside the floodplain, perform
critical processes and functions discussed in section III above. The
agencies established a 1,500 foot threshold from the water's lateral
limit, which would be either the high tide line or the ordinary high
water mark, in the definition of neighboring because, based on the
agencies' expertise and experience implementing the CWA and in light of
the science, the agencies concluded this was a reasonable and practical
boundary within which to conclude the waters most clearly significantly
affected the integrity of the traditional navigable water or the
territorial seas, and these covered adjacent waters are ``waters of the
United States.'' Waters located within the 100-year floodplain of a
traditional navigable water, interstate water, or the territorial seas,
and waters located more than 1,500 feet and less than 4,000 feet from
the ordinary high water mark of a traditional navigable water,
interstate water, the territorial seas, an impoundment, or a tributary,
may still be determined to have a significant nexus on a case-specific
basis under paragraph (a)(8) of the rule and therefore be a ``water of
the United States.'' See section IV.H.
H. Case-Specific ``Waters of the United States''
The rule establishes two exclusive circumstances under which case-
specific determinations will be made for whether a water has a
``significant nexus'' and is therefore a ``water of the United
States.'' The proposed rule included a broad provision that allowed for
a case-specific determination of significant nexus for any water that
was not categorically jurisdictional or excluded. Many commenters
expressed concern that such a broad opportunity for case-specific
``waters of the United States'' determinations would lead to too much
uncertainty about the jurisdictional status of waters in broad areas
throughout the country. The agencies have greatly reduced the extent of
waters subject to this individual review by carefully incorporating the
scientific literature and by utilizing agency expertise and experience
to draw boundaries. The rule provides for case-specific determinations
under more narrowly targeted circumstances based on the agencies'
assessment of the importance of certain specified waters to the
chemical, physical, and biological integrity of traditional navigable
waters, interstate waters, and the territorial seas.
First, the rule identifies at paragraph (a)(7) five subcategories
of waters (Prairie potholes, Carolina and Delmarva bays, pocosins,
western vernal pools in California, and Texas coastal prairie wetlands)
that the agencies have determined are ``similarly situated'' for
purposes of a significant nexus determination. Second, the rule
identifies at paragraph (a)(8) specific circumstances under which
waters will be subject to a case-specific significant nexus
determination but for which the agencies have not made a ``similarly
situated'' determination: Waters within the 100-year floodplain of a
traditional navigable water, interstate water, or the territorial seas,
and waters within 4,000 feet of the high tide line or the ordinary high
water mark of a traditional navigable water, interstate water, the
territorial seas, impoundments, or tributaries, as defined. If any
water meets the definition of ``adjacent'' waters it is jurisdictional
under paragraph (a)(6) and no case-specific significant nexus is
required. Waters that do not fall within the six categorically
jurisdictional waters identified in paragraph (a)(1) through
[[Page 37087]]
(a)(6) of the rule or within these two case-specific provisions are not
``waters of the United States.''
This section first discusses the five subcategories of waters that
the agencies determine are ``similarly situated'' for purposes of a
significant nexus determination; second, the 100-year floodplain and
4,000 foot boundaries under which waters will be subject to a case-
specific significant nexus determination but for which the agencies
have not made a ``similarly situated'' determination; third, the
definition of ``significant nexus'' and how the case-specific
significant nexus determinations will be made under these two
provisions; and, finally, the revisions made to the rule with respect
to case-specific determinations and major comments.
1. Waters Determined To Be ``Similarly Situated'' by Rule for Which a
Case-Specific Significant Nexus Determinations Is Required
In the rule, paragraph (a)(7) specifies the subcategories of waters
(Prairie potholes, Carolina and Delmarva bays, pocosins, western vernal
pools in California, and Texas coastal prairie wetlands) that, if they
are not otherwise jurisdictional under paragraphs (a)(1) through
(a)(6), the agencies determine to be ``similarly situated'' by rule. In
the proposal the agencies sought comment on a number of options to
address remaining waters that did not fit within the jurisdictional
categories, including whether to conclude that other waters were
``similarly situated'' in certain areas of the country or whether to
conclude that specified subcategories of waters were jurisdictional. 79
FR 22215, 22216. The agencies concluded that waters within the five
subcategories were ``similarly situated'' in the areas of the country
in which they are located. The rationale for this determination is
discussed above in Section III. Under paragraph (a)(7), Prairie
potholes, Carolina and Delmarva bays, pocosins, western vernal pools in
California, and Texas coastal prairie wetlands are jurisdictional when
they have a significant nexus to a traditional navigable water,
interstate water, or the territorial seas. Waters subject to normal
farming, silviculture, and ranching activities that are within these
subcategories will be assessed consistent with this provision of the
rule. Waters in these subcategories are not jurisdictional as a class
under the rule. However, because the agencies determined that these
subcategories of waters are ``similarly situated,'' the waters within
the specified subcategories that are not otherwise jurisdictional under
paragraph (a)(6) of the rule must be assessed in combination with all
waters of the same subcategory in the region identified by the
watershed that drains to the nearest point of entry of a traditional
navigable water, interstate water, or the territorial seas (hereinafter
referred to as the point of entry watershed).
When performing a case-specific significant nexus evaluation for a
water in the paragraph (a)(7) subcategories, the rule establishes which
waters must be considered in combination. The similarly situated waters
identified in the subparagraphs will be combined with other waters in
the same subparagraph located in a single point of entry watershed. For
example, under paragraph (a)(7) only western vernal pools can be
analyzed with other western vernal pools in the same point of entry
watershed. Waters identified in the subparagraphs that are otherwise
jurisdictional under the rule cannot be considered in combination with
paragraph (a)(7) waters for purposes of a case-specific significant
nexus determination under paragraph (a)(7). Individual waters of the
specified subcategories may be jurisdictional under other paragraphs of
this rule (e.g., a Prairie pothole that sits on a state border is an
interstate water under paragraph (a)(2) or a western vernal pool that
meets the definition of adjacent under paragraph (a)(6)). Where those
individual waters are jurisdictional under paragraph (a)(1) through
(a)(6) by rule, no case-specific significant nexus analysis is
required. The rule also states that waters in paragraph (a)(7) shall
not be combined with waters jurisdictional under paragraph (a)(6).
Essentially, while Prairie potholes are an identified subcategory under
paragraph (a)(7), that identification does not affect a Prairie pothole
that borders a covered tributary and is jurisdictional as an adjacent
water under paragraph (a)(6). Additionally, a Prairie pothole that is
jurisdictional under paragraph (a)(6) cannot be combined with Prairie
potholes that require a case-specific jurisdictional analysis under
paragraph (a)(7) since ``adjacent waters'' have already been determined
to have a significant nexus by rule. Finally, waters within the
specified subcategories in paragraph (a)(7) are assessed under
paragraph (a)(7) not under paragraph (a)(8); waters within the
specified subcategories that are within the 100-year flood plain of a
traditional navigable water, interstate water, or the territorial seas
or within the 4,000 foot boundary established for case-specific
determinations under paragraph (a)(8) remain ``similarly situated''
waters under paragraph (a)(7). These similarly situated waters are
evaluated in combination for their effect on the chemical, physical, or
biological integrity of traditional navigable waters, interstate
waters, or the territorial seas. Additional details about the case-
specific significant nexus analysis are found in section 4 below.
2. Waters Within the 100-Year Floodplain of a Traditional Navigable
Water, Interstate Water, or the Territorial Seas and Waters Within
4,000 Foot Boundary for Which a Case-Specific Significant Nexus
Determination Is Required
Paragraph (a)(8) in the rule specifies that a water that does not
otherwise meet the definition of adjacency is evaluated on a case-
specific basis for significant nexus under this paragraph where it is
located within the 100-year floodplain of a traditional navigable
water, interstate water, or the territorial seas or within 4,000 feet
of the high tide line or ordinary high water mark of a traditional
navigable water, interstate water, the territorial seas, impoundment,
or covered tributary. Although these waters are not considered
similarly situated by rule, waters under this paragraph can be
determined on a case-specific basis to be similarly situated. This is a
change from the proposal which would have allowed for a similarly
situated analysis and significant nexus determination for any water,
anywhere in the region. Under the rule, the waters specified in
paragraph (a)(7) and waters that meet the requirements in paragraph
(a)(8) are the only waters for which a case-specific significant nexus
determination may be made.
Under paragraph (a)(8), only waters that are within the 100-year
floodplain of a traditional navigable water, interstate water, or the
territorial seas or within the 4,000 foot boundary can be evaluated on
a case-specific basis for significant nexus to a traditional navigable
water, interstate water, or the territorial seas. If a portion of the
water is located within the 100-year floodplain of a traditional
navigable water, interstate water, or the territorial seas or 4,000
feet of the ordinary high water mark or high tide line of a traditional
navigable water, interstate water, the territorial seas, impoundment,
or covered tributary, the entire water will be considered to be within
the boundaries for paragraph (a)(8) and will undergo a case-specific
significant nexus determination. Under this provision, if the 100-year
floodplain of a traditional navigable water,
[[Page 37088]]
interstate water, or the territorial seas extends beyond 4,000 feet of
the ordinary high water mark, a water, that is not otherwise
jurisdictional under the rule, within that floodplain will be evaluated
under the 100-year floodplain boundary of paragraph (a)(8). A water
within the boundaries must be evaluated on a case-specific basis for
not only a significant nexus but also for a determination of whether
there are any waters with which the waters is similarly situated.
Waters identified in paragraph (a)(8) may not be combined with waters
identified in paragraph (a)(6) for purposes of the significant nexus
analysis, but may be combined with similarly situated waters located in
the same point of entry watershed. If waters identified in paragraph
(a)(8) also meet the definition of adjacency under paragraph (a)(6),
they are jurisdictional as ``adjacent waters'' and do not need a case-
specific significant nexus analysis. Under paragraph (a)(8), for
example, the agencies would evaluate on a case-specific basis whether a
low-centered polygonal tundra and patterned ground bog in an area with
a small floodplain and located beyond the 1,500 foot boundary but
within the 100-year floodplain of a traditional navigable water,
interstate water, or the territorial seas or within the 4,000 foot
boundary, or a wetland in which normal farming, ranching, or
silviculture activities occur, as those terms are used in section
404(f) of the Clean Water Act and its implementing regulations, has a
significant nexus as defined in the rule.
Waters identified in the subcategories in paragraph (a)(7) are
evaluated under paragraph (a)(7) only; the provisions of paragraph
(a)(8), including the boundaries in paragraph (a)(8), do not apply to
paragraph (a)(7) waters. The significant nexus analysis for waters
under paragraph (a)(8) will then consider the waters individually or,
if it is determined that there are similarly situated waters, as a
group of waters within a point of entry watershed for their effect on
the chemical, physical, or biological integrity of traditional
navigable waters, interstate waters, or the territorial seas.
Some commenters asked how wetlands underlain by permafrost would be
treated under this rule. Waters subject to case-specific review under
paragraph (a)(8) will include areas determined to meet the technical
definition of ``wetlands'' because they have the required hydrology,
vegetation, and soils. The presence of permafrost is not itself
determinative of whether a particular area satisfies the three
parameter requirement needed to be wetlands under the rule. This is
true under existing regulations and remains unchanged in this rule.
Because the definition of wetland does not change under the rule, the
agencies do not anticipate the rule will alter the current scope of CWA
jurisdiction over wetlands underlain by permafrost.
a. Summary of Rationale for Case-Specific Significant Nexus Analysis
Within 100-Year Floodplain of a Traditional Navigable Water, Interstate
Water, or the Territorial Seas
As discussed in Section III, above, the scientific literature
supports that wetlands and open waters in floodplains are physically,
chemically, and biologically connected to downstream traditional
navigable waters, interstate waters, or the territorial seas and
significantly affect the integrity of such waters. The Science Report
concludes that wetlands and open waters located in ``floodplains are
physically, chemically and biologically integrated with rivers via
functions that improve downstream water quality, including the
temporary storage and deposition of channel-forming sediment and woody
debris, temporary storage of local ground water that supports baseflow
in rivers, and transformation and transport of stored organic matter.''
Science Report at ES-2 to ES-3. As described in the Science Report and
the Technical Support Document, such waters act as the most effective
buffer to protect downstream waters from nonpoint source pollution
(such as nitrogen and phosphorus), provide habitat for breeding fish
and aquatic insects that also live in streams, and retain floodwaters,
sediment, nutrients, and contaminants that could otherwise negatively
impact the condition or function of downstream waters. As discussed
above, in defining waters as adjacent, and therefore categorically
jurisdictional, the agencies established a 1,500 foot boundary for
waters located within the 100-year floodplain of a traditional
navigable water, interstate water, the territorial seas, impoundment,
or covered tributary in order to protect vitally important waters while
at the same time providing a practical and implementable rule. In light
of the science on the functions provided by floodplain waters and
wetlands, waters and wetlands within the 100-year floodplain of
traditional navigable waters, interstate waters, or the territorial
seas are likely to provide those functions for traditional navigable
waters, interstate waters, or the territorial seas. However, because
the 100-year floodplain of a traditional navigable water can, in some
case be quite large, the agencies concluded it was reasonable to
subject waters and wetlands in the 100-year floodplain that are beyond
1,500 feet of the ordinary high water mark, and therefore do not meet
the definition of ``neighboring,'' to a case-specific significant nexus
analysis rather than concluding that such waters are categorically
jurisdictional. This inclusion of a case-specific analysis for such
floodplain waters is supported by the SAB. The SAB concluded that
``distance should not be the sole indicator used to evaluate the
connection of `other waters' to jurisdictional waters.'' SAB 2014b at
3. In allowing the case-specific evaluation of waters within the 100-
year floodplain of a traditional navigable water, interstate water, or
the territorial seas that do not meet the definition of adjacency, the
agencies are allowing for the functional relationship of those
floodplain waters to be considered regardless of distance. The SAB also
supported the Science Report's conclusion that ``the scientific
literature strongly supports the conclusions that streams and
`bidirectional' floodplain wetlands are physically, chemically, and/or
biologically connected to downstream navigable waters; however, these
connections should be considered in terms of a connectivity gradient.''
SAB 2014a at 1. In addition, the SAB noted, ``the literature review
does substantiate the conclusion that floodplains and waters and
wetlands in floodplain settings support the physical, chemical, and
biological integrity of downstream waters.'' Id. at 3.
The agencies do not anticipate that there will be numerous
circumstances in which this provision will be utilized because
relatively few traditional navigable waters will have floodplains
larger than 4,000 feet (the other threshold in paragraph (a)(8) for
waters regardless of floodplain). Further, the agencies recognize that
extensive areas of the nation's floodplains have been affected by
levees and dikes which reduce the scope of flooding. In these
circumstances, the scope of the 100-year floodplain is also reduced and
is reflected in FEMA mapping used by the agencies. In circumstances
where there is little or no alteration of the floodplain and it remains
relatively broad, the agencies will explicitly consider distance
between the water being evaluated and traditional navigable water,
interstate water, or the territorial seas when making a case-specific
significant nexus determination. Based on the science concerning the
important functions provided by floodplain waters and wetlands, the
agencies established this provision to ensure that truly
[[Page 37089]]
important waters may still be protected on a case-specific basis. By
using the 100-year floodplain and limiting the provision to traditional
navigable waters, interstate waters, or the territorial seas, the
agencies are reasonably balancing the protection of waters that may
have a significant nexus with the goal of providing additional
certainty.
b. Summary of Rationale for Case-Specific Significant Nexus Analysis
Within 4,000 Foot Boundary
The agencies establish a provision in the rule for case-specific
significant nexus determinations because the agencies concluded that
some waters located beyond the distance limitations established for
``adjacent waters'' can have significant chemical, physical, and
biological connections to and effects on traditional navigable waters,
interstate waters, or the territorial seas. The agencies reasonably
identified the 4,000 foot boundary for these case-specific significant
nexus determinations by balancing consideration of the science and the
agencies' expertise and experience in making significant nexus
determinations with the goal of providing clarity to the public while
protecting the environment and public health. The agencies' experience
has shown that the vast majority of waters where a significant nexus
has been found, and which are therefore important to protect to achieve
the goals of the Act, are located within the 4,000 foot boundary.
Moreover, because of the unique status under the CWA of traditional
navigable waters, interstate waters, and the territorial seas, the 100-
year floodplain boundary for these waters provides another means of
identifying on a case-specific basis those waters that significantly
affect traditional navigable waters, interstate waters or the
territorial seas. The agencies' balancing of these considerations is
consistent with the statute and the Supreme Court opinions. The
agencies decided that it is important to promulgate a rule that not
only protects the most vital of our Nation's waters, but one that is
practical and provides sufficient boundaries so that the public
reasonably understands where CWA jurisdiction ends.
The agencies' decision to establish a provision that authorizes
case-specific significant nexus analysis for waters within 4,000 feet
is based on a number of factors. These waters may be located within the
floodplain of a traditional navigable water, interstate water, the
territorial seas, impoundment, or covered tributary. Section IV.G. and
the Technical Support Document discuss the importance of floodplain
waters on the chemical, physical, and biological integrity of
downstream traditional navigable waters, interstate waters, or the
territorial seas. For purposes of clarity and to provide regulatory
certainty, the agencies decided to use distance boundaries within the
100-year floodplain to define adjacency for floodplain waters. Under
the rule, the only floodplain waters that are specifically identified
as being jurisdictional as ``adjacent'' are those located in whole or
in part within the 100-year floodplain and not more than 1,500 feet of
the ordinary high water mark of jurisdictional waters.
Similarly, due to the many functions that waters located within
4,000 feet of the high tide line of a traditional navigable water or
the territorial seas provide and their often close connections to the
surrounding traditional navigable waters, science supports the
agencies' determination that such waters are rightfully evaluated on a
case-specific basis for significant nexus to a traditional navigable
water or the territorial seas. Waters within 4,000 feet of the ordinary
high water mark of a traditional navigable water, interstate water, the
territorial seas, impoundment, or covered tributary may fall within the
riparian areas of such waters. As discussed in section IV.G., in
response to comments regarding the uncertainty of the term ``riparian
area,'' the agencies removed the term from the definition of
``neighboring.'' However, the agencies continue to recognize that
science is clear that wetlands and open waters in riparian areas
individually and cumulatively can have a significant effect on the
chemical, physical, or biological integrity of downstream waters. Thus,
the rule allows for a case-specific determination of significant nexus
for waters located within 4,000 feet of the high tide line or the
ordinary high water mark of a traditional navigable water, interstate
water, the territorial seas, impoundment, or covered tributary.
The agencies have always recognized that adjacency is bounded by
proximity, and the rule adds additional clarity to adjacency by
bounding what can be considered neighboring. The science is clear that
a water's proximity to downstream waters influences its impact on those
waters. The Science Report states, ``[s]patial proximity is one
important determinant of the magnitude, frequency and duration of
connections between wetlands and streams that will ultimately influence
the fluxes of water, materials and biota between wetlands and
downstream waters.'' Science Report at ES-11. Generally, waters that
are closer to a jurisdictional water are more likely to be connected to
that water than waters that are farther away. A case-specific analysis
for waters located within 4,000 feet of the high tide line or the
ordinary high water mark of a traditional navigable water, interstate
water, the territorial seas, impoundment, or covered tributary allows
such waters to be considered jurisdictional only where they meet the
significant nexus requirements. Even where not within a 100-year
floodplain, waters within 4,000 feet of the high tide line or the
ordinary high water mark of a traditional navigable water, interstate
water, the territorial seas, impoundment, or covered tributary can have
significant chemical, physical, and biological connections with
traditional navigable waters, interstate waters, or the territorial
seas.
As noted previously, in response to comments concerned that there
were no bounds in the proposed rule on how far a surface hydrologic
connection could be for purposes of adjacency, the agencies did not
include surface hydrologic connections as its own factor for
determining adjacency in the final rule. Such connections, however, are
relevant in a case-specific significant nexus determination under
paragraph (a)(8). For example, waters located within 4,000 feet of the
high tide line or the ordinary high water mark of a traditional
navigable water, interstate water, the territorial seas, impoundment,
or covered tributary that contribute confined surface flow to a
downstream water can have important hydrologic connections to and
effects on that downstream water such as the attenuation and cycling of
nutrients that would otherwise effect downstream water quality.
The agencies' decision to establish the case-specific provision at
paragraph (a)(8), including the boundaries, was also informed by the
knowledge that waters located within 4,000 feet of the high tide line
or the ordinary high water mark of a traditional navigable water,
interstate water, the territorial seas, impoundment, or covered
tributary can have a confined surface or shallow subsurface connection
to such a water. In order to provide the clarity and certainty that
many commenters requested regarding ``adjacent waters,'' the rule does
not define ``neighboring'' to include all waters with confined surface
or shallow subsurface connections.
However, the agencies recognize that the science demonstrates that
waters with a confined surface or shallow subsurface connection to
jurisdictional
[[Page 37090]]
waters can have important effects on downstream waters. For purposes of
a case-specific significant nexus analysis under the rule, a shallow
subsurface hydrologic connection is lateral water flow over a
restricting layer in the top soil horizons, or a shallow water table
which fluctuates within the soil profile, sometimes rising to or near
the ground surface. In addition, water can move within confined man-
made subsurface conveyance systems such as drain tiles and storm
sewers, and in karst topography. Confined subsurface systems can move
water, and potential contaminants, directly to surface waters and
rapidly without the opportunity for nutrient or sediment reduction
along the pathway.
Shallow subsurface connections move quickly through the soil and
impact surface water directly within hours or days rather than the
years it may take long pathways to reach surface waters. See Technical
Support Document. Tools to assess shallow subsurface flow include
reviewing the soils information from the NRCS Soil Survey, which is
available for nearly every county in the United States. When assessing
whether a water within the 4,000 foot boundary performs any of the
functions identified in the rule's definition of significant nexus, the
significant nexus determination can consider whether shallow subsurface
connections contribute to the type and strength of functions provided
by a water or similarly situated waters. However, neither shallow
subsurface connections nor any type of groundwater, shallow or deep,
are themselves ``waters of the United States.''
The proposed rule did not set a distance threshold for case-
specific waters to be evaluated for a significant nexus. Some
commenters argued that there should be a limitation on areas subject to
case-specific analysis while others contended that the agencies lack
discretion to set regulatory limits that would exclude from
jurisdiction any water meeting the significant nexus test. The agencies
disagree that the agencies lack the authority to establish reasonable
boundaries to determine what areas are subject to case-specific
significant nexus analysis. Nothing in the CWA or case law mandates
that the agencies require every water feature in the nation be subject
to analysis for significant nexus. The Supreme Court has made clear
that the agencies have the authority and responsibility to determine
the limits of CWA jurisdiction, and establishing boundaries based on
agency judgment, expertise and experience in administering the statute
is at the core of the agencies authority and discretion.
After weighing the scientific information about these waters'
connectivity and importance to protecting downstream waters, the
agencies' considerable experience making jurisdictional determinations,
the objective of enhancing regulatory clarity and consistent with the
statute and the caselaw, the agencies decided to set a boundary of
4,000 feet for case-specific significant nexus analysis for waters that
do not otherwise meet the requirements of paragraphs (a)(1) through
(a)(7). Tying this provision for case-specific significant nexus
analysis to distance informed by the science, and the agencies'
experience and expertise, as spatial proximity is a key contributor to
connectivity among waters. Science Report at ES-11. Distance is by no
means the sole factor, and aquatic functions will play a prominent role
in determining whether specific waters covered under this aspect of
paragraph (a)(8) have a significant nexus. In light of the role spatial
proximity plays in connectivity and the objective of enhancing
regulatory clarity, predictability and consistency, the agencies
conclude that establishing a boundary for this aspect of waters subject
to case-specific significant nexus analysis based on distance is
reasonable.
While, for purposes of this national rule, distance is a reasonable
and appropriate measure for identifying where this case-specific
significant nexus analysis will be conducted, the science does not
point to any particular bright line delineating waters that have a
significant nexus from those that do not. The Science Report concluded
that connectivity of streams and wetlands to downstream waters occurs
along a gradient. The evidence unequivocally demonstrates that the
stream channels and floodplain wetlands or open waters that together
form river networks are clearly connected to downstream waters in ways
that profoundly influence downstream water integrity. The connectivity
and effects of non-floodplain wetlands and open waters are more
variable and thus more difficult to address solely from evidence
available in peer-reviewed studies. Science Report at ES-5. Because of
this variability, with respect to waters that are not covered by
paragraphs (a)(1) through (a)(7) of the rule, the science does not
provide a precise point along the continuum at which waters provide
only speculative or insubstantial functions to downstream waters.
Like connectivity itself, there is also a continuum of outcomes
associated with picking a distance threshold. A smaller threshold
increases the likelihood that waters that could have a significant
nexus will not be analyzed and therefore not subject to the Act; a
larger threshold reduces that possibility, but also means that agency
and the public's resources are expended conducting significant nexus
analyses on waters that have a lower likelihood of meriting the Act's
protection.
Recognizing that there is no optimal line, in selecting both the
100-year floodplain for and the 4,000 foot boundaries the agencies
looked principally to the extensive experience the Corps has gained in
making significant nexus determinations since the Rapanos decision. As
noted in Section III above, since the Rapanos decision, the agencies
have developed extensive experience making significant nexus
determinations, and that experience and expertise informed the judgment
of the agencies in establishing both the 100-year floodplain boundary
and the 4,000 foot boundary. The agencies have made determinations in
every state in the country, for a wide range of waters in a wide range
of conditions. The vast majority of the waters that the Corps has
determined have a significant nexus are located within 4,000 feet of a
jurisdictional tributary, traditional navigable or interstate water, or
the territorial seas. Therefore, the agencies conclude that the 100-
year floodplain and 4,000 foot boundaries in the rule will sufficiently
capture for analysis those waters that are important to protect to
achieve the goals of the Clean Water Act.
The agencies acknowledge that, as with any meaningful boundary,
some waters that could be found jurisdictional lie beyond the boundary
and will not be analyzed for significant nexus. The agencies minimize
that risk by also establishing a provision in paragraph (a)(8) for
case-specific significant nexus analysis of waters located within the
100-year floodplain of a traditional navigable water, interstate water,
or the territorial seas. While in the agencies' experience the vast
majority of wetlands with a significant nexus are located within the
4,000 foot boundary, it is the agencies' experience that there are a
few waters that have been determined to be jurisdictional that are
located beyond this boundary, typically due to a surface or shallow
subsurface hydrologic connections. Nonetheless, the agencies have
weighed these considerations and concluded that the value of enhancing
regulatory clarity, predictability and consistency through a distance
limit outweigh the likelihood that a distinct minority of waters that
might be shown
[[Page 37091]]
to meet the significant nexus test will not be subject to analysis. In
the agencies' experience, requiring an evaluation of significant nexus
for waters covered by paragraph (a)(8) should capture the vast majority
of waters having a significant nexus to the downstream waters. The
agencies therefore conclude that that adoption of the 4,000 foot
boundary is reasonable.
The rule's requirements for these waters, coupled with those for
``adjacent waters,'' create an integrated approach that tailors the
regulatory regime based on the science and the agencies' policy
objectives. Determining by rule that covered adjacent waters have a
significant nexus follows the science, achieves regulatory clarity and
predictability, and avoids expenditure of agency and public resources
on case-specific significant nexus analysis. Similarly, providing for
case-specific significant nexus analysis for waters that are not
adjacent but within the 4,000 foot distance limit, as well as those
within the 100-year floodplain of a traditional navigable water,
interstate water, or the territorial seas, is consistent with science
and agency experience, will ensure protection of the important waters
whose protection will advance the goals of the Clean Water Act, and
will greatly enhance regulatory clarity for agency staff, regulated
parties, and the public.
For these reasons, the agencies decided to allow case-specific
determinations of significant nexus for waters located within the 100-
year floodplain of a traditional navigable water, interstate water, or
the territorial seas and for waters located within 4,000 feet of the
high tide line or the ordinary high water mark of a traditional
navigable water, an interstate water, the territorial seas, an
impoundment, or a covered tributary. Under the rule, these waters are
jurisdictional only where they individually or cumulatively (if it is
determined that there are other similarly situated waters) have a
significant nexus to traditional navigable waters, interstate waters,
or the territorial seas. Additional scientific and policy rationale for
including such waters as waters that can be evaluated on a case-
specific basis can be find in the Technical Support Document.
The agencies emphasize that they fully support efforts by States
and tribes to protect under their own laws any additional waters,
including locally special waters that may not be within the
jurisdiction of the CWA as the agencies have interpreted its scope in
this rule. Indeed, the promulgation of the 100-year floodplain and 4000
foot boundaries for purposes of a case-specific analysis of significant
nexus does not foreclose states from acting consistent with their state
authorities to establish protection for waters that fall outside of the
protection of the CWA. In promulgating the 4,000 foot boundary, the
agencies have balanced protection and clarity, scientific uncertainties
and regulatory experience, and established a line that is, in their
judgment, reasonable and consistent with the statute and its goals and
objectives.
3. Case-Specific Significant Nexus Determinations
Only waters identified in paragraphs (a)(7) or (a)(8) of the rule
require a case-specific determination of significant nexus. This
section discusses the definition of significant nexus in the rule and
how the agencies will make case-specific significant nexus
determinations under the rule.
a. Definition of Significant Nexus
Paragraph (c)(5) of the rule defines the term ``significant nexus''
to mean a significant effect (more than speculative or insubstantial)
on the chemical, physical, or biological integrity of a traditional
navigable water, interstate water, or the territorial seas. Waters,
including wetlands, are evaluated either alone, or in combination with
other similarly situated waters in the region, based on the functions
the evaluated waters perform. Functions to be considered for the
purposes of determining significant nexus are sediment trapping,
nutrient recycling, pollutant trapping, transformation, filtering and
transport, retention and attenuation of floodwaters, runoff storage,
contribution of flow, export of organic matter, export of food
resources, and provision of life-cycle dependent aquatic habitat (such
as foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in traditional navigable waters, interstate
waters, or the territorial seas.
The agencies' definition of significant nexus is based upon the
language in SWANCC and Rapanos. The definition is also consistent with
current practice, where field staff evaluate the functions of the
waters in question and the effects of these functions on downstream
waters. In order to add clarity and transparency to the definition of
significant nexus, the agencies have listed in the definition the
functions that will be considered in a significant nexus analysis.
These functions are consistent with the agencies' scientific
understanding of the functioning of aquatic ecosystems. A water does
not need to perform all of the functions listed in paragraph (c)(5) in
order to have a significant nexus. Depending upon the particular water
and the functions it provides, if a water, either alone or in
combination with similarly situated waters, performs just one function,
and that function has a significant impact on the integrity of a
traditional navigable water, interstate water, or the territorial seas,
that water would have a significant nexus.
Case-specific determinations of significant nexus require paragraph
(a)(7) or (a)(8) waters to be evaluated either alone, or in combination
with other similarly situated waters in the region. In the rule, the
agencies interpret the phrase ``in the region'' to mean the watershed
that drains to the nearest traditional navigable water, interstate
water, or the territorial seas through a single point of entry. See
Section III. In circumstances where the single point of entry watershed
includes waters that are identified under paragraph (a)(7) and waters
that are subject to analysis under paragraph (a)(8), those waters will
be analyzed separately under the provisions of those paragraphs.
In a case-specific analysis of significant nexus, the agencies
determine whether the water they are evaluating, in combination with
other similarly situated waters in the region, has a significant effect
on the chemical, physical, or biological integrity of the nearest
traditional navigable water, interstate water, or the territorial seas.
As noted previously, the agencies evaluate the listed functions in
paragraph (c)(5) as part of that evaluation to determine if the water
has an impact that is more than speculative or insubstantial.
b. Conducting Case-Specific Significant Nexus Determinations Under
Paragraphs (a)(7) and (a)(8)
The significant nexus analysis for waters assessed under paragraphs
(a)(7) and (a)(8) is a three-step process: First, the region for the
significant nexus analysis must be identified--under the rule, it is
the watershed which drains to the nearest traditional navigable water,
interstate water or territorial sea; second, any similarly situated
waters must be identified--under the rule, that is waters that function
alike and are sufficiently close to function together in affecting
downstream waters; and third, the waters are evaluated individually or
in combination with any identified similarly situated waters in the
single point of entry watershed to determine if they significantly
impact the chemical, physical or biological integrity of the
traditional navigable water, interstate water or the territorial seas.
[[Page 37092]]
i. ``In the Region''--The Point of Entry Watershed
As discussed in Section III of the preamble and established in the
definition of ``significant nexus,'' the region for purposes of a
significant nexus analysis is the watershed that drains to the nearest
traditional navigable water, interstate water, or the territorial seas.
The first step of the analysis is to identify the point of entry
watershed that the water being evaluated under paragraphs (a)(7) or
(a)(8) drains to. This point of entry approach identifies the nearest
traditional navigable water, interstate water, or the territorial seas
that the water being evaluated and any similarly situated waters flow
to and delineates the watershed of that nearest traditional navigable
water, interstate water, or the territorial seas. The point of entry
watershed is the area drained by the nearest traditional navigable
water, interstate water, or the territorial seas and is typically
defined by the topographic divides between one traditional navigable
water, interstate water, or the territorial seas and another.
Available mapping tools, such as those that are based on the NHD,
topographic maps, and elevation data, can be used to demarcate
boundaries of the single point of entry watershed. As discussed in
Section III and in the Technical Support Document, the single point of
entry watershed represents the scientifically appropriate sized area
for conducting a case-specific significant nexus evaluation in most
cases.
In the arid West, the agencies recognize there may be situations
where the single point of entry watershed is very large, and it may be
reasonable to evaluate all similarly situated waters in a smaller
watershed. Under those circumstances, the agencies may demarcate
adjoining catchments surrounding the water to be evaluated that,
together, are generally no smaller than a typical 10-digit hydrologic
unit code (HUC-10) watershed in the same area. The area identified by
this combination of catchments would be the ``region'' used for
conducting a significant nexus evaluation under paragraphs (a)(7) or
(a)(8) under those situations. The basis for such an approach in very
large single point of entry watersheds in the arid West should be
documented in the jurisdictional determination.
ii. ``Similarly Situated''
Second, the agencies determine if the water or waters to be
evaluated are similarly situated. The waters identified in paragraph
(a)(7) are similarly situated by rule and shall be combined with other
waters of the same category located in the same watershed that drains
to the nearest traditional navigable water, interstate water, or the
territorial seas with no need for a case-specific similarly situated
finding. Under paragraph (a)(7), only waters of the same subparagraph
in the point of entry watershed can be considered as similarly
situated. For example, only pocosins may be evaluated with other
pocosins in the same point of entry watershed. Pocosins in different
point of entry watersheds cannot be combined, and pocosins cannot be
combined with Carolina bays under paragraph (a)(7), even where they
occur in the same point of entry watershed.
Unlike waters evaluated under paragraph (a)(7), the waters
specified at paragraph (a)(8) require a determination whether they are
similarly situated. Under this step, the agencies apply factors in the
determination of when waters evaluated under paragraph (a)(8) should be
considered either individually or in combination for purposes of a
significant nexus analysis. A determination of ``similarly situated''
requires an evaluation of whether a group of waters in the region that
meet the distance thresholds set out under paragraph (a)(8) can
reasonably be expected to function together in their effect on the
chemical, physical, or biological integrity of downstream traditional
navigable waters, interstate waters, or the territorial seas.
Similarly situated waters can be identified as sufficiently close
together for purposes of this paragraph of the regulation when they are
within a contiguous area of land with relatively homogeneous soils,
vegetation, and landform (e.g., plain, mountain, valley, etc.). In
general, it would be inappropriate, for example, to consider waters as
``similarly situated'' under paragraph (a)(8) if these waters are
located in different landforms, have different elevation profiles, or
have different soil and vegetation characteristics, unless the waters
perform similar functions and are located sufficiently close to a
``water of the United States'' to allow them to consistently and
collectively function together to affect a traditional navigable water,
interstate water, or the territorial seas. In determining whether
waters under paragraph (a)(8) are sufficiently close to each other the
agencies will also consider hydrologic connectivity to each other or a
jurisdictional water.
In determining whether groups of waters under paragraph (a)(8)
perform ``similar functions'' the agencies will consider functions such
as habitat, water storage, sediment retention, and pollution
sequestration. In addition, consideration of wetland/water type and
landscape location are relevant for determining if the waters are
similarly situated. For example, Texas coastal sand sheet wetlands that
form a complex of wetlands with other wetlands of the same type on the
landscape and are densely located may very well be similarly situated
and considered in combination with other Texas coastal sand sheet
wetlands in the same single point of entry watershed. However, under
paragraph (a)(8), waters do not need to be of the same type (as they do
in paragraph (a)(7)) to be considered similarly situated. As described
above, waters are similarly situated under paragraph (a)(8) where they
perform similar functions or are located sufficiently close to each
other, regardless of type. The agencies will consider the hydrologic,
geomorphic, and ecological characteristics and circumstances of the
waters under consideration. Examples include: Documentation of
chemical, physical, or biological interactions of the similarly
situated waters; aerial photography; USGS and state and local
topographical or terrain maps and information; NRCS soil survey maps
and data; other available geographic information systems (GIS) data;
National Wetlands Inventory maps where wetlands meet the CWA
definition; and state and local information. The evaluation will use
any available site information and pertinent field observations where
available, relevant scientific studies or data, or other relevant
jurisdictional determinations that have been completed in the region.
Only those waters that do not meet the requirements in paragraph
(a)(1) through (a)(6) are to be considered in case-specific significant
nexus determinations; subcategory waters that meet the provisions in
paragraph (a)(1) through (a)(6) are per se jurisdictional without the
need for a significant nexus determination. For example, waters that
are identified under paragraph (a)(6) are adjacent and are not subject
to a case-specific significant nexus evaluation under paragraph (a)(7)
or (a)(8). Waters evaluated under paragraph (a)(7) cannot be combined
with waters identified in paragraph paragraph (a)(6) or (a)(8), and
waters evaluated under paragraph (a)(8) cannot be combined with waters
identified in paragraph (a)(6) or (a)(7). For example, Prairie potholes
being evaluated under paragraph (a)(7) may not be combined with Prairie
potholes that are per se jurisdictional under paragraph (a)(6) that
meet the definition
[[Page 37093]]
of adjacent. When a water meets the specifications at both paragraphs
(a)(7) and (a)(8), it can only be evaluated under paragraph (a)(7).
That is, for example, if a wetland is a Western vernal pool and is also
within 4,000 feet of the ordinary high water mark of a covered
tributary, it can only be assessed for significant nexus under
paragraph (a)(7) in combination with other Western vernal pools in the
point of entry watershed. Unlike paragraph (a)(8), there is no distance
threshold for waters evaluated under paragraph (a)(7)--that is, waters
in the paragraph (a)(7) subcategories that are more than 4,000 feet
from the high tide line or the ordinary high water mark of a
traditional navigable water, interstate water, the territorial seas,
impoundment, or covered tributary or are beyond the 100-year floodplain
of an traditional navigable water, interstate water, or the territorial
seas are to be included in combination in a significant nexus analysis.
iii. Significant Nexus Analysis for Paragraph (a)(7) and (a)(8) Waters
Third, the agencies evaluate waters individually or in combination
with any identified similarly situated waters in the single point of
entry watershed to determine if they significantly impact the chemical,
physical, or biological integrity of the traditional navigable water,
interstate water, or the territorial seas. For purposes of determining
significant nexus under paragraph (a)(7), all waters of the specified
subcategory are to be considered in combination in the point of entry
watershed, as those waters are similarly situated. For purposes of
determining significant nexus under paragraph (a)(8), depending on the
results of step two, a water within the boundaries in paragraph (a)(8)
is evaluated either alone or in combination with other similarly
situated waters in the region. For example, in the case where the
agencies have determined that a particular water under paragraph (a)(8)
is not similarly situated, it is evaluated individually for significant
nexus; the water cannot be aggregated if it is not similarly situated
with other such waters.
The analysis will include an evaluation of the functions listed in
paragraph (c)(5) of the rule, which defines significant nexus. A water
has a significant nexus when any single function or combination of
functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest traditional
navigable water, interstate water, or the territorial seas. A water may
be determined to have a significant nexus based on performing any of
the following functions: sediment trapping, nutrient recycling,
pollutant trapping, transformation, filtering, and transport, retention
and attenuation of floodwaters, runoff storage, contribution of flow,
export of organic matter, export of food resources, or provision of
life cycle dependent aquatic habitat (such as foraging, feeding,
nesting, breeding, spawning, or use as a nursery area) for species
located in a traditional navigable water, interstate water, or the
territorial seas.
For purposes of paragraph (c)(5)(ix), a species is located in a
traditional navigable water, interstate water, or the territorial seas
if such a water is a typical type of habitat for at least part of the
life cycle of the species. For example, amphibians and many reptiles
can use a traditional navigable water, interstate water, or the
territorial seas for part of their life cycle needs.
When evaluating a water individually or in combination with other
similarly situated waters for the presence of a significant nexus to a
traditional navigable water, interstate water, or the territorial seas,
a variety of factors will influence the chemical, physical, or
biological connections the water has with the downstream traditional
navigable water, interstate water, or the territorial seas, including
distance from a jurisdictional water, the presence of surface or
shallow subsurface hydrologic connections, and density of waters of the
same type (if it has been concluded that such waters can be evaluated
in combination). The likelihood of a significant connection is greater
with increasing size and decreasing distance from the identified
traditional navigable water, interstate water, or the territorial seas,
as well as with increased density of the waters for such waters that
can be considered in combination as similarly situated waters. In
addition, the presence of a surface or shallow subsurface hydrologic
connection can influence the impact that a water has with downstream
waters.
In many cases, the presence of a hydrologic connection increases
the strength of the impact of the downstream traditional navigable
water, interstate water, or the territorial seas. However, a hydrologic
connection is not necessary to establish a significant nexus, because,
as Justice Kennedy stated, in some cases the lack of a hydrologic
connection would be a sign of the water's function in relationship to
the traditional navigable water, interstate water, or the territorial
seas. These functional relationships include retention of floodwaters
or pollutants that would otherwise flow downstream to the traditional
navigable water, interstate water, or the territorial seas. See 547
U.S. at 775 (citations omitted) (J. Kennedy) (``it may be the absence
of an interchange of waters prior to the dredge and fill activity that
makes protection of the wetlands critical to the statutory scheme'').
The Science Report concludes, ``[s]ome effects of non-floodplain
wetlands on downstream waters are due to their isolation, rather than
their connectivity. Wetland `sink' functions that trap materials and
prevent their export to downstream waters (e.g., sediment and entrained
pollutant removal, water storage) result because of the wetland's
ability to isolate material fluxes.'' Science Report at ES-4. For
example, a report that reviewed the results of multiple scientific
studies concluded that depressional wetlands lacking a surface outlet
functioned together to significantly reduce or attenuate flooding. See
Science Report and Technical Support Document. Even when they lack a
surface hydrologic connection to downstream traditional navigable
waters, interstate waters, or the territorial seas, Prairie potholes,
for instance, cumulatively can store large volumes of water, impacting
streamflow and reducing flooding downstream, and several studies have
quantified the large storage capacity of Prairie pothole complexes.
This water storage function is estimated to hold tens of millions of
cubic meters of water, including for example Prairie potholes located
in the watersheds of Devils Lake and the Red River of the North, which
have both had a long history of flooding. Where Prairie potholes lack a
surface hydrologic connection, this water storage capacity is
particularly effective in reducing downstream flooding and can have a
significant effect on downstream traditional navigable waters,
interstate waters, or the territorial seas. Thus, even when lacking a
surface hydrologic connection, a water can still have a significant
effect on the chemical or the biological integrity of downstream
traditional navigable waters, interstate waters, or the territorial
seas.
The rule recognizes that not all waters have the requisite
connection to traditional navigable waters, interstate waters, or the
territorial seas sufficient to be determined jurisdictional. Waters
with a significant nexus must significantly affect the chemical,
physical, or biological integrity of a downstream traditional navigable
water,
[[Page 37094]]
interstate water, or the territorial seas, and the requisite nexus must
be more than ``speculative or insubstantial.'' Rapanos at 780.
Evidence of chemical connectivity and the effect on waters can be
found by identifying the properties of the water in comparison to the
identified traditional navigable water, interstate water, or the
territorial seas; signs of retention, release, or transformation of
nutrients or pollutants; and the effect of landscape position on the
strength of the connection to the nearest ``water of the United
States,'' and through it to a traditional navigable water, interstate
water, or the territorial seas. In addition, relevant factors
influencing chemical connectivity include hydrologic connectivity (see
physical factors, below), surrounding land use and land cover, the
landscape setting, and deposition of chemical constituents (e.g.,
acidic deposition).
Evidence of physical connectivity and the effect on traditional
navigable waters, interstate waters, or the territorial seas can be
found by identifying evidence of physical connections, such as flood
water or sediment retention (flood prevention). Presence of indicators
of hydrologic connections between the other water and jurisdictional
water are also indicators of a physical connection. Factors influencing
physical connectivity include rain intensity, duration of rain events
or wet season, soil permeability, and distance of hydrologic connection
between the paragraph (a)(7) or (a)(8) water and the traditional
navigable water, interstate water, or the territorial seas, depth from
surface to water table, and any preferential flowpaths.
Evidence of biological connectivity and the effect on waters can be
found by identifying: Resident aquatic or semi-aquatic species present
in the case-specific water and the tributary system (e.g., amphibians,
aquatic and semi-aquatic reptiles, aquatic birds); whether those
species show life-cycle dependency on the identified aquatic resources
(foraging, feeding, nesting, breeding, spawning, use as a nursery area,
etc.); and whether there is reason to expect presence or dispersal
around the case-specific water, and if so whether such dispersal
extends to the tributary system or beyond or from the tributary system
to the case-specific water. Factors influencing biological connectivity
include species' life history traits, species' behavioral traits,
dispersal range, population size, timing of dispersal, distance between
the case-specific water and a traditional navigable water, interstate
water, or the territorial seas, the presence of habitat corridors or
barriers, and the number, area, and spatial distribution of habitats.
Non-aquatic species or species such as non-resident migratory birds do
not demonstrate a life cycle dependency on the identified aquatic
resources and are not evidence of biological connectivity for purposes
of this rule.
For practical administrative purposes, the rule does not require
evaluation of all similarly situated waters under paragraph (a)(7) or
(a)(8) when concluding that those waters have a significant nexus to a
traditional navigable water, interstate water, or territorial sea. When
a subset of similarly situated waters provides a sufficient science-
based justification to conclude presence of a significant nexus, for
efficiency purposes a significant nexus analysis need not unnecessarily
require time and resources to locate and analyze all similarly situated
waters in the entire point of entry watershed. For example, if a single
Carolina bay or a group of Carolina bays in a portion of the point of
entry watershed is determined to significantly affect the chemical,
physical, or biological integrity of a traditional navigable water,
interstate water, or the territorial seas, the analysis does not have
to document all of the similarly situated Carolina bays in the
watershed in order to conduct the significant nexus analysis. A
conclusion that significant nexus is lacking may not be based on
consideration of a subset of similarly situated waters because under
the significant nexus standard the inquiry is how the similarly
situated waters in combination affect the integrity of the downstream
water.
While the rule is clear that waters that are jurisdictional by rule
cannot be combined with waters subject to a case-specific significant
nexus analysis, the analysis may appropriately include the evaluation
of functions of paragraph (a)(8) waters that reach covered waters
through paragraph (a)(6) waters without consideration of the functions
contributed by those paragraph (a)(6) waters. The hydrologic
connections between paragraph (a)(8) waters and a covered tributary and
eventually to a traditional navigable water, interstate water, or the
territorial seas, can often occur through an adjacent water. This
hydrologic connection is an appropriate part of the case-specific
analysis as to whether the paragraph (a)(8) waters, alone or in
combination with any similarly situated paragraph (a)(8) waters in the
point of entry watershed, provide those functions downstream such that
they significantly affect the chemical, physical or biological
integrity of the traditional navigable water, interstate water, or the
territorial seas. For example, when evaluating a wetland that is 2,500
feet from the ordinary high water mark of an paragraph (a)(5) water and
that has surface or shallow subsurface connections to downstream
traditional navigable waters, interstate waters, or the territorial
seas via a wetland that is adjacent to an paragraph (a)(4) water, the
existence of those connections is not ignored. However, while a water's
connections to the traditional navigable water, interstate water, or
the territorial seas through paragraph (a)(5) through (a)(7) waters can
be considered in the significant nexus analysis in order to determine
whether the functions of the paragraph (a)(8) waters are provided
downstream, only the functions of the water, along with any similarly
situated waters, being evaluated under paragraph (a)(8) on downstream
water integrity can be included in the significant nexus analysis.
The administrative record for a jurisdictional determination for a
water under paragraph (a)(7) or (a)(8) will include available
information supporting the determination. In addition to location and
other descriptive information regarding the water at issue, the record
will include an explanation of the rationale for the jurisdictional
conclusion and a description of the information used. Relevant
information can come from many sources, and need not always be specific
to the water whose jurisdictional status is being evaluated. Studies of
the same type of water or similarly situated waters can help to inform
a significant nexus analysis as long as they are applicable to the
water being evaluated. In the case of paragraph (a)(8) waters, the
administrative record will include the rationale behind the similarly
situated analysis, including an explanation of the data or information
examined.
The agencies expect that where waters are determined to be
similarly situated in a single point of entry watershed, such similarly
situated waters will often be found jurisdictional through the case-
specific analysis of significant nexus. However, case-specific factors
such as distance to the traditional navigable water, interstate water,
or the territorial seas; density or number of similarly situated
waters; individual and cumulative size of the similarly situated
waters; soil permeability; climate; etc., may be considered in the
determination, and there could be cases where even considering these
waters in combination with similarly situated waters will not
[[Page 37095]]
be sufficient for waters to have a significant nexus.
Within a single point of entry watershed, over a period of time
there will likely be multiple jurisdictional determinations. For
paragraph (a)(7) waters, if a case-specific significant nexus
determination has been made in the point of entry watershed, all waters
in the subcategory in the point of entry watershed are jurisdictional.
For paragraph (a)(8) waters, the case-specific significant nexus
analyses must use information used in previous jurisdictional
determinations, and if a significant nexus has been established for one
water in the watershed, then other similarly situated waters in the
watershed would also be found to have a significant nexus. This is
because under Justice Kennedy's test, similarly situated waters in the
region should be evaluated together. A positive significant nexus
determination would then apply to all similarly situated waters within
the point of the watershed. A negative case-specific significant nexus
evaluation under paragraph (a)(7) or (a)(8) of all similarly situated
waters in the point of entry watershed applies to all similarly
situated waters in that watershed. However, as noted above, a
conclusion that significant nexus is lacking may not be based on
consideration of a subset of similarly situated waters, because under
the significant nexus standard the inquiry is how the similarly
situated waters in combination affect the integrity of the downstream
water. The documentation for each case should be complete enough to
support the specific jurisdictional determination, including an
explanation of which waters were considered together as similarly
situated and in the same region.
4. Summary of Revisions to Case-Specific Determinations of ``Waters of
the United States'' and Major Comments
a. Significant Nexus
Some commenters stated concerns over the potential for inconsistent
application of the significant nexus analysis in a jurisdictional
determination. To address this concern within the regulatory framework,
the agencies provide more detail regarding the definition of
significant nexus in the rule and list the specific functions that will
be considered in the analysis. This approach provides individual
regulators who conduct the analysis clear and consistent parameters
that they will consider during their review in making jurisdictional
determinations and provides transparency to the regulated public over
which factors will be considered.
Overall, there was support for the concept of the single point of
entry watershed as the interpretation of ``in the region.'' Several
commenters supported the approach that the single point of entry
watershed was an appropriate scale to use to measure effect on
traditional navigable waters, interstate waters, or the territorial
seas. Other commenters felt the single point of entry watershed was too
small to capture all the benefits that waters that do not meet the
definition of adjacency contribute. Some of the SAB panel members
thought that because surface and ground-watershed units may not align,
watersheds might be problematic for defining ``in the region.'' These
panel members suggested that a more scientifically justified approach
would include surface and subsurface waters in a watershed delineation.
The agencies have retained the single point of entry watershed from the
proposed rule as the appropriate unit of analysis for significant nexus
in the final rule as these watersheds are more easily understood and
easier to delineate than those that map subsurface waters as the SAB
suggested.
With respect to the agencies' approach to ``similarly situated
waters,'' commenters offered support for assessing waters in
combination based on their type and function, particularly waters such
as Prairie potholes. Conversely, several commenters found that the
ability to aggregate waters that do not meet the definition of
adjacency is over-reaching and causes uncertainty to the regulated
public. Some commenters also attributed uncertainty in which waters
were regulated to subjectivity in review by Federal regulator(s).
Similarly, some commenters were concerned that waters eligible for
protection were based on an individual analyst's interpretation and
wanted to know how the agencies would address consistency and potential
bias. In response, the rule lists in paragraph (a)(7) a limited number
of subcategories of waters where waters of the specified types have
been determined by rule to be similarly situated for a significant
nexus analysis. This will add consistency, predictability, and clarity,
as the rule explicitly states that such waters are similarly situated
for purposes of the significant nexus analysis. For waters identified
under paragraph (a)(8), the agencies have established two limitations:
Waters within the 100-year floodplain of a traditional navigable water,
interstate water, or the territorial seas, and waters within 4,000 foot
feet of a traditional navigable water, interstate water, the
territorial seas, impoundment, or covered tributary. The agencies also
have established within the definition of significant nexus at
paragraph (c)(5) criteria for determining whether waters are similarly
situated and should therefore be analyzed in combination. Waters
identified under paragraph (a)(8) are similarly situated when they
function alike and are sufficiently close to function together in
affecting downstream waters. The agencies have not determined that such
waters are categorically similarly situated, so the agencies will base
their case-specific determinations of whether a particular water has
any similarly situated waters on the available information and science.
The rule also clarifies that paragraph (a)(8) waters cannot be
considered similarly situated with ``adjacent waters,'' which are
jurisdictional by rule, and paragraph (a)(7) waters, which have been
determined to be similarly situated by rule. These parameters will
reduce inconsistency in reviews and add clarity.
Similarly, several commenters expressed concern that landowners
would not know which water bodies on their property are subject to CWA
jurisdiction due to aggregation, as waters on their property may be
considered similarly situated with waters located off-site. While the
rule does not eliminate the use of case-specific significant nexus
analyses, and the concern arises from Justice Kennedy's phrase
``similarly situated,'' the parameters placed on waters requiring a
case-specific determination and the clearer definition of significant
nexus address the concerns about uncertainty and inconsistencies in
reviews. In particular, waters that are not either one of the five
identified subcategories in paragraph (a)(7) or within the thresholds
in paragraph (a)(8) cannot be subject to a case-specific significant
nexus analysis under the rule. Generally, jurisdictional determinations
are conducted at the request of an applicant or landowner for specific
waters. While the agencies cannot arbitrarily depart from a
determination that waters are ``similarly situated,'' landowners may
provide new information to inform subsequent jurisdictional
determinations. In addition, owners with questions regarding
jurisdiction of waters on their property may always consult their local
Corps District or EPA Regional Office, which is not a change from
longstanding practice.
[[Page 37096]]
b. Case-Specific Determinations
The rule provides more regulatory certainty by narrowing the scope
of waters that can be assessed under a case-specific significant nexus
evaluation as compared to the proposal. These changes still allow the
scientific value of specific waters not covered in paragraph (a)(1)
through (a)(6) to be evaluated on a case-specific basis.
In the proposal, the agencies solicited comment regarding a variety
of approaches to the category of waters subject to a case-specific
significant nexus analysis. In addition, the agencies solicited comment
on additional scientific research and data that might further inform
decisions about these waters. In particular the agencies solicited
information about whether current scientific research and data
regarding particular types of waters are sufficient to support the
inclusion of subcategories of types of waters, either alone or in
combination with similarly situated waters, that can appropriately be
identified as always lacking or always having a significant nexus. One
of these alternate approaches in the preamble to the proposed rule was
to determine by rule that certain additional subcategories of waters
would be jurisdictional rather than addressed with a case-specific
basis for determining significant nexus.
Many commenters expressed support for the agencies' proposed
approach to case-specific waters, included additional references to
support these waters being protected by rule, and supported the
treatment of certain categories of waters as similarly situated (that
is, evaluating them in combination with similarly situated waters for
the purposes of the significant nexus analysis). Some suggested the
agencies establish jurisdiction over case-specific waters by rule and
provided detailed information in support of their position. Other
commenters suggested additional subcategories of waters be considered
as jurisdictional or as similarly situated by rule, such as playa
lakes, kettle lakes, and woodland vernal pools.
However, there was a concern raised by other commenters about what
was termed regulatory overreach and uncertainty created by the ``other
waters'' category in the proposal. Some commenters stated that the
``other waters'' category in the proposal would allow the agencies to
regulate virtually any water. To address this concern, the rule places
limits on which waters could be subject to a case-specific significant
nexus determination, in recognition that case-specific analysis of
significant nexus is resource-intensive and based on the body of
science that exists. As noted above, the agencies also establish by
rule subcategories of waters that are ``similarly situated'' for the
purposes of a significant nexus analysis because science supports that
the subcategory waters fall within a higher gradient of connectivity.
By not determining that any one of the waters available for case-
specific analysis is jurisdictional by rule, the agencies are
recognizing the gradient of connectivity that exists and will assert
jurisdiction only when that connection and the downstream effects are
significant and more than speculative and insubstantial.
Waters are covered under the rule only where they are identified as
jurisdictional in paragraphs (a)(1) through (a)(6), where they are not
excluded under paragraph (b), or where they are within the limited
number of subcategories listed in paragraphs (a)(7) and (a)(8) and have
a case-specific significant nexus to a traditional navigable water,
interstate water, or the territorial seas. These limits on jurisdiction
reflect the case law and are in response to comments requesting greater
regulatory certainty. Although some commenters suggested additional
subcategories of waters for consideration, such as playa lakes and
kettle lakes, the agencies at this time are not able to determine that
the available science supports that the suggested additional
subcategories of waters as a class have a significant nexus to
traditional navigable waters, interstate waters, or the territorial
seas. However, to be clear, under the rule, individual waters of the
suggested additional subcategories are jurisdictional where they meet
the requirements of paragraphs (a)(1) through (a)(6) or (a)(8) (e.g., a
playa lake that is an interstate water, a kettle lake that is an
adjacent water, or a woodland vernal pool that is less than 4,000 feet
from a jurisdictional tributary and is determined on a case-specific
basis to have a significant nexus to a traditional navigable water,
interstate water, or the territorial seas).
In consideration of the variety of views of the commenters, the
Science Report, the input from the SAB, and the developing state of the
science, the agencies reasonably decided not to establish jurisdiction
over all waters that do not meet the requirements of paragraph (a)(1)
through (a)(6) by rule. Instead, the agencies established case-specific
provisions for some specified waters at paragraph (a)(7) and waters
within the boundaries at paragraph (a)(8). This approach strikes a
balance between requests for clear boundaries and limited case-specific
reviews with scientific support.
I. Waters and Features That Are Not ``Waters of the United States''
In the rule, the agencies identify a variety of waters and features
that are not ``waters of the United States.'' Prior converted cropland
and waste treatment systems have been excluded from this definition
since 1992 and 1979, respectively, and they remain substantively and
operationally unchanged. Only ministerial changes to delete an outdated
cross reference are made to the exclusion for waste treatment systems.
The agencies add exclusions for all waters and features identified as
generally exempt in preamble language from Federal Register documents
by the Corps on November 13, 1986, and by EPA on June 6, 1988. This is
the first time these exclusions have been established by rule. In
addition, under prior preamble language, the agencies retained the
authority to determine that a particular feature generally considered
non-jurisdictional was in fact a ``water of the United States.'' The
agencies do not retain that authority for features excluded under the
rule. The agencies for the first time also establish by rule that
certain ditches are excluded from jurisdiction. The agencies add
exclusions for groundwater and erosional features, as well as
exclusions for some waters that were identified in public comments as
possibly being found jurisdictional under proposed rule language where
this was never the agencies' intent. These exclusions are reflective of
current agencies' practice, and their inclusion in the rule furthers
the agencies' goal of providing greater clarity over what waters are
and are not protected under the CWA. Importantly, under the rule all
waters and features identified in paragraph (b) as excluded will not be
``waters of the United States,'' even if they otherwise fall within one
of the categories in paragraphs (a)(4) through (a)(8). For example, a
ditch that is excluded under paragraph (b)(3)(i) or (b)(3)(ii) is not
jurisdictional even when the ditch connects directly or through another
water to a traditional navigable water, interstate water, or the
territorial seas. The proposed rule referenced paragraphs (a)(1)
through (a)(8), but the agencies did not intend to exclude any
traditional navigable waters, for example, and the revision clarifies
that. Finally, nothing in the rule is intended to change the way in
which the Corps applies individual or nationwide permits.
The exclusions reflect the agencies' long-standing practice and
technical judgment that certain waters and
[[Page 37097]]
features are not subject to the CWA. The exclusions are also guided by
Supreme Court cases. The significant nexus standard arises from the
case law and is used to interpret the terms of the CWA. Thus, a
significant nexus determination is not a purely scientific inquiry, but
rather is a determination by the agencies in light of the statutory
language, the statute's goals, objectives and policies, the case law,
the relevant science, and the agencies' technical expertise and
experience. The plurality opinion in Rapanos also noted that there were
certain features that were not primarily the focus of the CWA. See 547
U.S. at 734. In this section of the proposed rule, the agencies are
drawing lines and concluding that certain waters and features are not
subject to the jurisdiction of the Clean Water Act. The Supreme Court
has recognized that clarifying the lines of jurisdiction is a difficult
task: ``Our common experience tells us that this is often no easy task:
The transition from water to solid ground is not necessarily or even
typically an abrupt one. Rather, between open waters and dry land may
lie shallows, marshes, mudflats, swamps, bogs--in short, a huge array
of areas that are not wholly aquatic but nevertheless fall far short of
being dry land. Where on this continuum to find the limit of `waters'
is far from obvious.'' Riverside Bayview at 132-33. The exclusions are
an important aspect of the agencies' policy goal of providing clarity
and certainty. Just as the categorical assertions of jurisdiction over
covered tributaries and covered adjacent waters simplify the
jurisdiction issue, the categorical exclusions will likewise simplify
the process, and they reflect the agencies' determinations of the lines
of jurisdiction based on science, the case law and the agencies'
experience and expertise.
The existing exclusion for waste treatment systems moves to
paragraph (b)(1) with no substantive changes. One ministerial change is
the deletion of a cross-reference in the current language to an EPA
regulation that no longer exists. Because the agencies are not
addressing the substance of the exclusion, the agencies do not make
conforming changes to ensure that each of the existing definitions of
the ``waters of the United States'' for the various CWA programs have
the exact same language with respect to the waste treatment system
exclusion, with the exception of deleting the cross-reference.
Many commenters expressed concern about whether the agencies'
insertion of a comma following this ministerial change unintentionally
narrowed the exclusion such that all excluded waste treatment systems
must be designed to meet the requirements of the Clean Water Act. The
commenters indicated concerns that waste treatment systems built before
the Clean Water Act or primarily for purposes of other environmental
laws could not be exempt. The agencies do not intend to change how the
waste treatment exclusion is implemented and have deleted this proposed
comma. Continuing current practice, any waste treatment system built in
a ``water of the United States'' would need a section 404 permit to be
constructed and a section 402 permit for discharges from the waste
treatment system into ``waters of United States.''
A number of commenters suggested the agencies clarify how the waste
treatment system exclusion is currently implemented. Many comments
raised questions about stormwater systems and wastewater reuse and
whether such facilities qualified under the waste treatment system
exclusion as part of a complete waste treatment system. For clarity,
the agencies have identified related exclusions in paragraphs (b)(6)
and (b)(7). Many commenters also suggested making substantive changes
to the existing exclusion for waste treatment systems. Because the
agencies are not making any substantive changes to the waste treatment
system exclusion and these comments are outside the scope of the
proposed rule, the final rule does not reflect changes suggested in
public comments.
The existing exclusion for prior converted cropland moves to
paragraph (b)(2) of the rule and is unchanged. A number of commenters
suggested changes to the existing exclusion for prior converted
cropland. As with waste treatment systems, the preamble to the proposed
rule stated this rulemaking was not making changes to the exclusion for
prior converted cropland. As a result, comments requesting changes to
the prior converted cropland exclusion or seeking clarification of how
the exclusion is implemented in the field are outside the scope of this
rulemaking, and the rule does not reflect changes or respond to issues
raised in public comments. The agencies will continue to implement this
exclusion consistent with current policy and practice.
The agencies identify excluded ditches in paragraph (b)(3).
Jurisdictional ditches are discussed at more detail in section IV.F.
The rule excludes all ditches with ephemeral flow that are not
excavated in or relocate a tributary. The rule also excludes ditches
with intermittent flow that are not a relocated tributary, excavated in
a tributary, or drain wetlands, regardless of whether or not the
wetland is a jurisdictional water. Finally, ditches that do not connect
to a traditional navigable water, interstate water, or territorial sea
either directly or through another water are excluded, regardless of
whether the flow is ephemeral, intermittent, or perennial. These ditch
exclusions are clearer for the regulated public to identify and more
straightforward for agency staff to implement than the proposed rule or
current policies. The ditch exclusions do not affect the possible
status of a ditch as a point source.
Many comments addressed ditches, and many of these comments are
reflected in the approach to ditches articulated in the rule. The
majority of commenters requested that the agencies' ditch exclusion be
clarified or broadened. Many commenters were confused by the term
``uplands'' and did not feel the term had a common understanding. For
example, some commenters felt the term referred only to areas at higher
elevations in the landscape. Many expressed concerns that all ditches
would be jurisdictional under the proposed rule. Many groups especially
called for exclusions of roadside ditches.
The revised exclusions reflect the agencies' careful consideration
of these comments. First, the agencies have eliminated the term
``uplands'' in response to the questions the term created. Second, the
agencies have instead provided a clearer statement of the types of
ditches that are subject to exclusion--ditches that are not excavated
in or relocate a tributary and ditches that do not drain a wetland.
Eliminating the term ``uplands'' with this more straightforward
description should improve clarity. Finally, the agencies have more
clearly stated the flow regimes in ditches that are subject to the
exclusions; these flow regimes are described earlier and have been used
by the agencies consistently and are readily understood by field staff
and the public.
As noted, the agencies received many comments asking that roadside
ditches be addressed, and more specifically excluded, in the final
rule. Like the proposed rule, the final rule does not include an
explicit exclusion for roadside ditches, but the agencies believe the
exclusions included in the final rule will address the vast majority of
roadside and other transportation ditches. Moreover, since the agencies
have focused in the final rule on the physical characteristics of
excluded ditches, the exclusions will address all ditches that the
agencies have
[[Page 37098]]
concluded should not be subject to jurisdiction, including certain
ditches on agricultural lands and ditches associated with modes of
transportation, such as roadways, airports, and rail lines.
As discussed in Section IV.F.1., the definition of tributary
includes natural, undisturbed waters and those that have been man-
altered or constructed, but which science shows function as a
tributary. In addition, natural streams and rivers that are altered or
modified for purposes as flood control, erosion control, and other
reasons does not convert the tributary to a ditch. A stream or river
that has been channelized or straightened because its natural sinuosity
has been altered, cutting off the meanders, is not a ditch. A stream
that has banks stabilized through use of concrete or rip-rap (e.g.,
rocks or stones) is not a ditch. The Los Angeles River, for example, is
a ``water of the United States'' (and, indeed, a traditional navigable
water) and remains a ``water of the United States'' and is not a
excluded under paragraph (b)(3), even where it has been ditched,
channelized, or concreted.
The rule excludes ditches with ephemeral flow except where a ditch
is excavated in or relocates a covered tributary. Under the rule, that
portion of a ditch with ephemeral flow actually excavated in or
relocating the covered tributary would be considered jurisdictional.
The jurisdictional status of upstream and downstream portions of the
same ditch would have to be assessed based on the specific facts and
under the terms of the rule to determine flow characteristics and
whether or not the ditch is excavated in or relocates a tributary. This
approach reasonably balances the exclusion with the need to ensure that
covered tributaries, and the significant functions they provide, are
preserved. A ditch that relocates a stream is not an excluded ditch
under paragraph (b)(3), and a stream is relocated either when at least
a portion of its original channel has been physically moved, or when
the majority of its flow has been redirected. A ditch that is a
relocated stream is distinguishable from a ditch that withdraws water
from a stream without changing the stream's aquatic character. The
latter type of ditch is excluded from jurisdiction where it meets the
listed characteristics of excluded ditches under paragraph (b)(3). The
agencies will determine historical presence of tributaries using a
variety of resources, such as USGS and state and local maps, historic
aerial photographs, local surface water management plans, street
maintenance data, wetlands and conservation programs and plans, as well
as functional assessments and monitoring efforts.
The rule also excludes ditches with intermittent flow except where
a ditch is excavated in or relocates a covered tributary, or drains
wetlands. Where an excluded ditch drains a wetland, the segment of the
ditch that physically intersects the wetland would be considered
jurisdictional. The jurisdictional status of upstream and downstream
portions of the same ditch would have to be assessed based on the
specific facts and under the terms of the rule to determine flow
characteristics and whether or not the ditch drains a wetland. The
provision of paragraph (b)(3) addressing draining of wetlands is
specific to ditches with intermittent flow. As discussed previously,
features that are ephemeral will flow only in response to precipitation
events, such as rainfall or snowmelt. Ditches with ephemeral flow,
therefore, do not typically have the flow characteristics
characteristic of ditches that drain wetlands. The agencies have
accordingly focused on intermittent ditches that drain wetlands.
In addition, the agencies clarify that a ditch drains a wetland
when it physically intersects the wetland. If the ditch has been cut to
carry only ephemeral flows, such as those following a storm event, the
effect of the ditch is minimal as it carries only that flow that
overtops the wetland during and immediately following the rain event.
However, if the ditch has been cut to carry intermittent or perennial
flows from the wetland, the ditch is serving as a conduit for
transferring flow from the wetland to a downstream tributary. As a
result of the cut ditch, the wetland's hydrologic regime is modified
and can generally affect the natural functions performed by the
wetland. When the ditch has been cut to carry intermittent or perennial
flow from the wetland to the downstream tributary, the wetland soils
and vegetation can shift into a community that supports less hydric
soils and a mix of riparian or upland vegetation. Consequently, the
ditch is draining the wetland and the wetland quality degrades and may
cease to exist over time. Therefore, a ditch that carries intermittent
flow and physically intersects with a wetland is not excluded under
this provision.
A number of commenters expressed concern that a ditch could be
viewed as both a point source and a ``water of the United States.''
However, the approach that ditches can be considered both reflects the
CWA itself as well as longstanding agency policy.
Paragraph (b)(4) of the rule identifies features and waters that
the agencies have identified as generally not ``waters of the United
States'' in previous preambles or guidance documents. Codifying these
longstanding practices supports the agencies' goals of providing
greater clarity, certainty, and predictability for the regulated public
and the regulators. The agencies' 1986 and 1988 preambles indicated
that these waters could be determined on a case-specific basis to be
``waters of the United States.'' This rule does not allow for this
case-specific analysis to be used to establish jurisdiction--these
waters are categorically excluded from jurisdiction. Some of the
exclusions have been modified slightly to address public comments and
improve clarity. The following features are not ``waters of the United
States'':
Artificially irrigated areas that would revert to dry land
should application of irrigation water to that area cease
Artificial, constructed lakes or ponds created by
excavating and/or diking dry land such as farm and stock watering
ponds, irrigation ponds, settling basins, log cleaning ponds, cooling
ponds, or fields flooded for rice growing
Artificial reflecting pools or swimming pools created by
excavating and/or diking dry land
Small ornamental waters created by excavating and/or
diking dry land for primarily aesthetic reasons
Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand or gravel that fill with water
Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways
Puddles
Several of these exclusions use the phrase ``dry land.'' This
phrase appears in the 1986 and 1988 preambles, and the agencies believe
the term is well understood based on the more than 30 years of practice
and implementation. But in keeping with the goal of providing greater
clarity, the agencies state that ``dry land'' refers to areas of the
geographic landscape that are not water features such as streams,
rivers, wetlands, lakes, ponds and the like. However, it is important
to note that a ``water of the United States'' is not considered ``dry
land'' just because it lacks water at a given time. Similarly, an area
remains ``dry land'' even if it is wet after a rainfall event. The
agencies received comments suggesting that the
[[Page 37099]]
final rule provide a definition of ``dry land'' as it relates to the
exclusion for stormwater control features. The agencies considered the
request and determined that there was no agreed upon definition given
geographic and regional variability. The agencies concluded that
further clarity on this issue can be provided during implementation.
In the exclusion for artificial lakes or ponds, the agencies have
removed language regarding ``use'' of the ponds, including the term
``exclusively.'' In most cases, the ``use'' of the pond is captured in
its name. More importantly, the agencies recognize that artificial
lakes and ponds are often used for more than one purpose and can have
other beneficial purposes, such as animal habitat, water retention or
recreation. For example, rice growing is typically facilitated by land
leveling and inundation that floods vast areas. The fields are flooded
for the purpose of weed control and to facilitate rice cultivation, but
these rice fields are often extensively used by waterfowl and other
wildlife. The agencies agree with commenters who raised concern that
rice fields ``used'' both for rice growing and waterfowl habitat should
continue to be excluded even where they are not used ``exclusively''
for a single purpose. The change to the exclusion reflects the
agencies' practice and ensures that waters the agencies have
historically not treated as jurisdictional do not become so because of
another incidental beneficial use.
The agencies have also added farm ponds, log cleaning ponds, and
cooling ponds to the list of excluded ponds in the rule based on public
comments. The list of ponds has always been illustrative rather than
exhaustive, and the additions respond to requests to clarify that farm
ponds, and log cleaning ponds \12\ created in dry land are excluded.
The agencies have also added cooling ponds created in dry land to the
list of excluded waters. The agencies also note that cooling ponds that
are created under section 404 in jurisdictional waters and that have
NPDES permits are subject to the waste treatment system exclusion,
which is not changing. Cooling ponds created to serve as part of a
cooling water system with a valid state permit constructed in waters of
the United States prior to enactment of the Clean Water Act and
currently excluded from jurisdiction remain excluded under the new
rule. Additional ponds will also likely fall under the exclusion based
on site specific evaluation, including, for example, fire control ponds
and fishing ponds excavated from dry land. Artificial lakes and ponds
created in dry land that do not connect to jurisdictional waters are
covered by this exclusion. Where these ponds do connect and discharge
to jurisdictional waters, the agencies will evaluate factors such as
the potential for introduction of pollutants and coverage under an
issued NPDES permit. As a general matter, ponds created in dry land
that discharge to ``waters of the United States'' are covered by the
exclusion where such discharge is regulated under a NPDES permit.
Conveyances created in dry land that are physically connected to and
are a part of the excluded feature are also excluded. These artificial
features are working together as a system, and it is appropriate to
treat them as one functional unit. The agencies emphasize that ponds
excluded from ``waters of the United States'' can, in some
circumstances, be point sources of pollution subject to section 301 of
the Act.
---------------------------------------------------------------------------
\12\ Log cleaning ponds are used to float logs for removal of
twigs, branches, and large knots.
---------------------------------------------------------------------------
The rule includes several refinements to the exclusion for water-
filled depressions created as a result of certain activities. In
addition to construction activity, the agencies have also excluded
water-filled depressions created in dry land incidental to mining
activity. This change is consistent with the agencies' 1986 and 1988
preambles, which generally excluded pits excavated for obtaining fill,
sand or gravel, and there is no need to distinguish between features
based on whether they are created by construction or mining activity.
The agencies also here clarify their longstanding view that only
the specific land being directly irrigated that would revert to dry
land should irrigation cease is exempt; it is not the case that all
waters within watersheds where irrigation occurs are exempt.
The rule identifies all erosional features, including gullies and
rills, as non-jurisdictional features. While the proposed rule
specifically identified gullies and rills, the agencies intended that
all erosional features would be excluded. The final rule makes this
clear. Erosional features are not jurisdictional under the terms of
paragraph (a) and the definitions in paragraph (c), especially the
definition of tributary. These features are specifically excluded in
the rule to avoid confusion, because preceding guidance identified them
as non-jurisdictional and many commenters stated these exclusions were
important to maintain in the rule.
Tributaries can be distinguished from erosional features by the
presence of bed and banks and an ordinary high water mark. Concentrated
surface runoff can occur within erosional features without creating the
permanent physical characteristics associated with bed and banks and
ordinary high water mark. See Technical Support Document. It should be
noted that some ephemeral streams are colloquially called ``gullies''
or the like even when they exhibit a bed and banks and an ordinary high
water mark; regardless of the name they are given locally, waters that
meet the definition of tributary are not excluded erosional features.
The rule also excludes lawfully constructed grassed waterways.
Grassed waterways are lawfully constructed for purposes of this rule
either where they are on dry land and replace non-jurisdictional
erosional features or, more commonly, where they have been lawfully
converted from an intermittent or ephemeral stream under a CWA permit.
Once converted to grassed waterways, these former streams segments no
longer exhibit a bed and banks or ordinary high water mark and are
excluded because they do not meet the definition of ``tributary.''
However, such conversion does not sever jurisdiction over the entire
length of the tributary above and below the grassed waterway. Instead,
the grassed waterway is considered a constructed break in the bed and
banks and ordinary high water mark. This is reflected in the definition
of tributary, which specifically addresses natural or man-made breaks
in bed and banks and ordinary high water mark.
The final rule adds an exclusion for puddles. The proposed rule did
not explicitly exclude puddles because the agencies have never
considered puddles to meet the minimum standard for being a ``water of
the United States,'' and it is an inexact term. A puddle is commonly
considered a very small, shallow, and highly transitory pool of water
that forms on pavement or uplands during or immediately after a
rainstorm or similar precipitation event. However, numerous commenters
asked that the agencies expressly exclude them in a rule. The final
rule does so.
The agencies include an exclusion for groundwater, including
groundwater drained through subsurface drainage systems. As discussed
in the preamble to the proposed rule, the agencies have never
interpreted ``waters of the United States'' to include groundwater. The
exclusion does not apply to surface expressions of groundwater, as some
commenters requested, such as where groundwater emerges on the surface
and
[[Page 37100]]
becomes baseflow in streams or spring fed ponds.
The final rule includes a new exclusion in paragraph (b)(6) for
stormwater control features constructed to convey, treat, or store
stormwater that are created in dry land. The agencies stated in the
proposed rule that the exclusions were guided by decisions of the
Supreme Court and were intended to further the agencies' goal of
providing clarity and certainty. The agencies in the proposed rule
sought to provide a ``full description'' of the waters that will not be
``waters of the United States.'' 79 FR at 22218. In response to the
agencies' proposal, several commenters indicated additional clarity was
needed, particularly with respect to stormwater control features and
wastewater recycling facilities. This exclusion responds to numerous
commenters who raised concerns that the proposed rule would adversely
affect municipalities' ability to operate and maintain their stormwater
systems, and also to address confusion about the state of practice
regarding jurisdiction of these features at the time the rule was
proposed.
The agencies' longstanding practice is to view stormwater control
measures that are not built in ``waters of the United States'' as non-
jurisdictional. Conversely, the agencies view some waters, such as
channelized or piped streams, as jurisdictional currently even where
used as part of a stormwater management system. Nothing in the proposed
rule was intended to change that practice. Nonetheless, the agencies
recognize that the proposed rule brought to light confusion about which
stormwater control features are jurisdictional waters and which are
not, and agree that it is appropriate to address this confusion by
creating a specific exclusion in the final rule for stormwater controls
features that are created in dry land.
Many commenters, particularly municipalities and other public
entities that operate storm sewer systems and stormwater management
programs, expressed concern that various stormwater control measures--
such as stormwater treatment systems, rain gardens, low impact
development/green infrastructure, and flood control systems--could be
considered ``waters of the United States'' under the proposed rule,
either as part of a tributary system, an adjacent water, or as a result
of a case-specific significant nexus analysis. This exclusion should
clarify the appropriate limits of jurisdiction relating to these
systems. A key element of the exclusion is whether the feature or
control system was built in dry land and whether it conveys, treats, or
stores stormwater. Certain features, such as curbs and gutters, may be
features of stormwater collection systems, but have never been
considered ``waters of the United States.''
Stormwater control features have evolved considerably over the past
several years, and their nomenclature is not consistent, so in order to
avoid unintentionally limiting the exclusion, the agencies have not
included a list of excluded features in the rule. The rule is intended
to exclude the diverse range of control features that are currently in
place and may be developed in the future.
Traditionally, stormwater controls were designed to direct runoff
away from people and property as quickly as possible. Cities built
systems to collect, convey, or store stormwater, using structures such
as curbs, gutters, and sewers. Often, cities used existing stream
networks as part of the stormwater drainage network. Retention and
detention stormwater ponds were built to store excess stormwater until
it could be more safely released.
Recently, treatment of stormwater has become more prevalent to
remove harmful pollutants before the stormwater is discharged. Even
more recently, cities have turned to green infrastructure, using
existing natural features or creating new features that mimic natural
hydrological processes that work to infiltrate or evapo-transpirate
precipitation, to manage stormwater at its source and keep it out of
the conveyance system. These engineered components of stormwater
management systems can address both water quantity and quality
concerns, as well as provide other benefits to communities. This rule
is designed to avoid disincentives to this environmentally beneficial
trend in stormwater management practices. This exclusion does not cover
transportation ditches; those ditches are addressed under paragraph
(b)(3) of the rule. As discussed above, the exclusion in paragraph
(b)(6) is intended to address engineered stormwater control structures
in municipal or urban environments. Stormwater control features are
designed to address runoff that occurs during and shortly after
precipitation events; as a result, stormwater features that convey
runoff are expected to only carry ephemeral or intermittent flow. For
ease of implementation, the agencies want water features to be dealt
with under only one provision of the rule. However, the agencies do not
expect the scope of ditches excluded to be different under paragraphs
(b)(3) and (b)(6), so there should be little practical need to
distinguish between the two.
Paragraph (b)(7) of the rule clarifies that wastewater recycling
structures constructed in dry land are excluded. This new exclusion
clarifies the agencies' current practice that such waters and water
features used for water reuse and recycling are not jurisdictional when
constructed in dry land. The agencies recognize the importance of water
reuse and recycling, particularly in areas like California and the
Southwest where water supplies can be limited and droughts can
exacerbate supply issues. This exclusion responds to numerous
commenters and encourages water reuse and conservation while still
appropriately protecting the chemical, physical, and biological
integrity of the nation's water under CWA.
The agencies specifically exclude constructed detention and
retention basins created in dry land used for wastewater recycling as
well as groundwater recharge basins and percolation ponds built for
wastewater recycling. Many commenters noted the growing interest in and
commitment to water recycling and reuse projects. Detention and
retention basins can play an important role in capturing and storing
water prior to beneficial reuse. Similarly, groundwater recharge basins
and percolation ponds are becoming more prevalent tools for water reuse
and recycling. These features are used to collect and store water,
which then infiltrates into groundwater via permeable soils. Though
these features are often created in dry land, they are also often
located in close proximity to tributaries or other larger bodies of
water. The exclusion also covers water distributary structures that are
built in dry land for water recycling. These features often connect or
carry flow to other water recycling structures, for example a channel
or canal that carries water to a percolation pond. The agencies have
not considered these water distributary systems jurisdictional where
they do not have surface connections back into, and contribute flow to,
``waters of the United States.'' In contrast, the agencies have
consistently regulated aqueducts and canals as ``waters of the United
States'' where they serve as tributaries, removing water from one part
of the tributary network and moving it to another. The exclusion in
paragraph (b)(7) codifies long-standing agency practice and encourages
water management practices that the agencies agree are important and
beneficial.
The agencies also received other suggestions for new exclusions
that
[[Page 37101]]
were not adopted in the final rule. The agencies determined that it was
not appropriate or necessary to add certain requested exclusions for
one or more reasons, including: (1) The requested exclusion was so
broadly characterized as to introduce significant confusion and
potentially have the effect of excluding waters that the agencies have
consistently determined should be covered as ``waters of the U.S.,''
(2) the requested exclusion was so site-specific or activity-based as
to lack illustrative value, or (3) the requested exclusion was likely
covered by another exclusion in the final rule.
It is important to note that while the waters listed in the
exclusions are not ``waters of the United States,'' they can serve as a
hydrologic connection that the agencies would consider under a case-
specific significant nexus under paragraphs (a)(7) and (a)(8). For
example, a wetland may be directly hydrologically connected to a
covered tributary via flow through an excluded non-wetland swale. While
the swale itself is excluded from jurisdiction, the connection of the
wetland to the tributary is relevant for determining whether the
wetland has a significant nexus to downstream traditional navigable
waters, interstate waters, or the territorial seas. In addition, these
geographic features may function as ``point sources'' under CWA section
502(14), such that discharges of pollutants to waters through these
features would be subject to other CWA regulations (e.g., CWA section
402).
V. Economic Impacts
This rule establishing the definition of ``waters of the United
States,'' by itself, imposes no direct costs. The potential costs and
benefits incurred as a result of this rule are considered indirect,
because the rule involves a definitional change to a term that is used
in the implementation of CWA programs (i.e., sections 303, 305, 311,
401, 402, and 404). Entities currently are, and will continue to be,
regulated under these programs that protect ``waters of the United
States'' from pollution and destruction. Each of these programs may
subsequently impose direct or indirect costs as a result of
implementation of their specific regulations.
While the rule imposes no direct costs, the agencies prepared an
economic analysis for informational purposes. In preparing the economic
analysis to accompany the final rule, the agencies considered what
should be the appropriate baseline for comparison. Existing regulations
and historic practice in implementing them represent one appropriate
baseline for comparison, and because the final rule is narrower in
jurisdictional scope than the existing regulations, there would be no
additional costs in comparison to this baseline. A comparison to recent
field practice following the 2008 guidance is also an appropriate
baseline, and the agencies prepared illustrative estimates of how the
costs and benefits of various CWA programs may change with an increase
in positive jurisdictional determinations relative to that baseline.
To estimate changes in potential costs and benefits of different
CWA programs, the economic analysis utilizes available program data to
estimate the extent to which assertion of jurisdiction might change
under the associated final policies. The proposed rule analysis
utilized CWA Section 404 jurisdictional determination and permit data
from fiscal years 2009-2010 (post SWANCC and Rapanos), following
issuance of program guidance in 2008 by the EPA and the Corps. The
analysis for the final rule has been updated using data from fiscal
years 2013-2014, providing a comparison to a more recent year of data,
which responds to public comments. An estimate of how assertion of
jurisdiction may change compared to the recent practice baseline,
developed using updated data from fiscal years 2013-2014 jurisdictional
determinations, is then applied to cost and benefit information for
affected CWA programs. Additional updates to the economic analysis
include a refined approach to calculating benefits from section 404
compensatory mitigation, differentiating between emergent and forested
wetlands, as well as presenting results in ranges to reflect
uncertainty. The agencies' economic analysis yielded the following key
conclusions:
Compared to the current regulations and historic practice
of making jurisdictional determinations, the scope of jurisdictional
waters will decrease, as would the costs and benefits of CWA programs.
Compared to a baseline of recent practice, the agencies
assessed two scenarios. Those scenarios result in an estimated increase
of between 2.84 and 4.65 percent in positive jurisdictional
determinations annually.
The agencies' analysis indicates that for both scenarios,
the change in benefits of CWA programs exceed the costs by a ratio of
greater than 1:1.
The economic analysis estimates that incremental annual
costs for scenario 1 will range from $158M-$307M and incremental annual
benefits will range from $339M-$350M and, for scenario 2, costs will
range from $237M-$465M and benefits will range from $555M-$572M.
The agencies conducted this economic analysis to provide the public
with information on the potential changes to the costs and benefits of
various CWA programs that may result from a change in the number of
positive jurisdictional determinations. The economic analysis was done
for informational purposes only, and the final decisions on the scope
of ``waters of the United States'' in this rulemaking are not based on
consideration of the information in the economic analysis. The economic
analysis fulfills the requirements of Executive Orders 13563 and 12866.
An explanation of the data, methods, and assumptions used to estimate
indirect costs and benefits can be found in the Economic Analysis for
the Clean Water Rule; Definition of ``Waters of the United States''
Under the Clean Water Act (Final Rule) in the accompanying docket.
VI. Related Acts of Congress, Executive Orders, and Agency Initiatives
A. Executive Order 12866: Regulatory Planning and Review and Executive
Order 13563: Improving Regulation and Regulatory Review
Under Executive Order 12866 (58 FR 51735, October 4, 1993), this
action is a ``significant regulatory action.'' Accordingly, EPA and the
Army submitted this action to the Office of Management and Budget (OMB)
for review under Executive Orders 12866 and 13563 (76 FR 3821, January
21, 2011) and any changes made in response to OMB recommendations have
been documented in the docket for this action.
In addition, EPA and the Army prepared an analysis of the potential
costs and benefits associated with this action. This analysis is
contained in Economic Analysis of the EPA-Army Clean Water Rule. A copy
of the analysis is available in the docket for this action.
B. Paperwork Reduction Act
This action does not impose any information collection burden under
the provisions of the Paperwork Reduction Act, 44 U.S.C. 3501 et seq.
Burden is defined at 5 CFR 1320.3(b). An agency may not conduct or
sponsor, and a person is not required to respond to, a collection of
information unless it displays a currently valid OMB control number.
The OMB control numbers for the CWA section 402 program may be found at
40 CFR 9.1. (OMB Control No. 2040-0004, EPA ICR No. 0229.19). For the
CWA section 404 regulatory
[[Page 37102]]
program, the current OMB approval number for information requirements
is maintained by the Corps of Engineers (OMB approval number 0710-
0003). However, there are no new approval or application processes
required as a result of this rulemaking that necessitate a new
Information Collection Request (ICR).
C. Regulatory Flexibility Act
The Regulatory Flexibility Act (RFA) generally requires an agency
to prepare a regulatory flexibility analysis of any rule subject to
notice-and-comment rulemaking requirements under the Administrative
Procedure Act or any other statute unless the agency certifies that the
rule will not have a significant economic impact on a substantial
number of small entities. Small entities include small businesses,
small organizations, and small governmental jurisdictions.
For purposes of assessing the impacts of this final action on small
entities, ``small entity'' is defined as: (1) A small business that is
a small industrial entity as defined in the U.S. Small Business
Administration's size standards (see 13 CFR 121.201); (2) a small
governmental jurisdiction that is a government of a city, county, town,
school district, or special district with a population of less than
50,000; or (3) a small organization that is any not-for-profit
enterprise that is independently owned and operated and is not dominant
in its field.
After considering the economic impacts of this rule on small
entities, we certify that this final rule will not have a significant
economic impact on a substantial number of small entities. See, e.g.,
Cement Kiln Recycling Coalition v. EPA, 255 F.3d 855 (D.C. Cir. 2001);
Michigan v. EPA, 213 F.3d 663 (D.C. Cir. 2000); Am. Trucking Ass'n v.
EPA, 175 F.3d 1027 (D.C. Cir. 1999); Mid-Tex Elec. Co-op, Inc. v. FERC,
773 F.2d 327 (D.C. Cir. 1985).
Under the RFA, the impact of concern is any significant adverse
economic impact on small entities, because the primary purpose of the
initial regulatory flexibility analysis is to identify and address
regulatory alternatives ``which minimize any significant economic
impact of the proposed rule on small entities.'' 5 U.S.C. 603. The
scope of jurisdiction in this rule is narrower than that under the
existing regulations. See 40 CFR 122.2 (defining ``waters of the United
States''). Because fewer waters will be subject to the CWA under the
rule than are subject to regulation under the existing regulations,
this action will not affect small entities to a greater degree than the
existing regulations. As a consequence, this action will not have a
significant adverse economic impact on a substantial number of small
entities, and therefore no regulatory flexibility analysis is required.
This rule is not designed to ``subject'' any entities of any size
to any specific regulatory burden. Rather, it is designed to clarify
the statutory scope of ``the waters of the United States, including the
territorial seas,'' section 502(7), consistent with Supreme Court
precedent. This question of CWA jurisdiction is informed by the tools
of statutory construction and the geographical and hydrological factors
identified in Rapanos v. United States, 547 U.S. 715 (2006), which are
not factors readily informed by the RFA.
Nevertheless, the scope of the term ``waters of the United States''
is a question that has continued to generate substantial interest,
particularly within the small business community, because permits must
be obtained for many discharges of pollutants into those waters. In
light of this interest, the EPA and the Army determined to seek wide
input from representatives of small entities while formulating the
proposed and final definition of this term that reflects the intent of
Congress consistent with the mandate of the Supreme Court's decisions.
Such outreach, although voluntary, is also consistent with the
President's January 18, 2011 Memorandum on Regulatory Flexibility,
Small Business, and Job Creation, which emphasizes the important role
small businesses play in the American economy. This process has enabled
the agencies to hear directly from these representatives, throughout
the rule development, about how they should approach this complex
question of statutory interpretation, together with related issues that
such representatives of small entities may identify for possible
consideration in separate proceedings. The agencies have prepared a
report summarizing their small entity outreach, the results of this
outreach, and how these results have informed the development of this
rule. This report, Report of the Discretionary Small Entity Outreach
for the Revised Definition of Waters of the United States (Docket Id.
No. EPA-HQ-OW-2011-0880-1927), is available in the docket.
D. Unfunded Mandates Reform Act
This action does not contain any unfunded mandate under the
regulatory provisions of Title II of the Unfunded Mandates Reform Act
of 1995 (UMRA) (2 U.S.C. 1531-1538), and does not significantly or
uniquely affect small governments. The action imposes no enforceable
duty on any state, local, or tribal governments, or the private sector,
and does not contain regulatory requirements that might significantly
or uniquely affect small governments. The definition of ``waters of the
United States'' applies broadly to CWA programs.
E. Executive Order 13132: Federalism
This rule does not have federalism implications. It will not have
substantial direct effects on the states, on the relationship between
the national government and the states, or on the distribution of power
and responsibilities among the various levels of government.
Keeping with the spirit of Executive Order 13132 and consistent
with the agencies' policy to promote communications with state and
local governments, the agencies consulted with state and local
officials throughout the process and solicited their comments on the
proposed action and on the development of the rule.
For this rule state and local governments were consulted at the
onset of rule development in 2011, and following the publication of the
proposed rule in 2014. In addition to engaging key organizations under
federalism, the agencies sought feedback on this rule from a broad
audience of stakeholders through extensive outreach to numerous state
and local government organizations.
Early in the rulemaking process, EPA held two in-person meetings
and two phone calls in the fall and winter of 2011. Organizations
involved include the National Governors Association, the National
Conference of State Legislatures, the Council of State Governments, the
National Association of Counties, the National League of Cities, the
U.S. Conference of Mayors, the County Executives of America, the
National Associations of Towns and Townships, the International City/
County Management Association, and the Environmental Council of the
States. Additionally, the National Association of Clean Water Agencies
and the Association of Clean Water Administrators were invited to
participate. The agencies held many additional calls and meetings with
state and local governments and their associations, in preparation for
the development of a proposed rule.
Similarly to the outreach conducted prior to the development of the
rule, the agencies committed themselves to providing a transparent,
comprehensive, and effective process for taking public comment on the
proposed rule. As part of this consultation, EPA held a meeting on May
13, 2014 to seek technical input on the proposed rule from the largest
[[Page 37103]]
national representative organizations for State and local governments.
During this process the agencies also extended its focused outreach to
include a series of meetings with the Local Government Advisory
Committee, and the Environmental Council of the States in conjunction
with the Association of Clean Water Administrators and the Association
of State Wetland Managers. In addition to engaging these key
organizations, the agencies sought additional feedback on the proposed
rule through broader public outreach to state and local government
organizations during the public comment period.
During the consultation process, some participants expressed
concern that the proposed changes may impose a resource burden on state
and local governments. Some participants urged EPA to ensure that
states are not unduly burdened by the regulatory revisions.
The agencies have prepared a report summarizing their voluntary
consultation and extensive outreach to State, local, and county
governments, the results of this outreach, and how these results have
informed the development of today's rule. This report, Report on the
Discretionary Consultation and Outreach to State, Local, and County
Governments on the Clean Water Rule: Definition of ``Waters of the
United States;'' Final Rule (Docket Id. No. EPA-HQ-OW-2011-0880) is
available in the docket for this rule.
F. Executive Order 13175: Consultation and Coordination With Indian
Tribal Governments
Subject to the Executive Order (E.O.) 13175 (65 FR 67249, November
9, 2000), agencies generally may not issue a regulation that has tribal
implications, (1) that imposes substantial direct compliance costs, and
that is not required by statute, unless the Federal government provides
the funds necessary to pay the direct compliance costs incurred by
tribal governments, or the agencies consult with tribal officials early
in the process of developing the proposed regulation and develop a
tribal summary impact statement, or (2) that preempts tribal law unless
the agencies consult with tribal officials early in the process of
developing the proposed regulation and develops a tribal summary impact
statement.
This action does not have tribal implications as specified in E.O.
13175. In compliance with the EPA Policy on Consultation and
Coordination with Indian Tribes (May 4, 2011), the agencies consulted
with tribal officials throughout the rulemaking process to gain an
understanding of tribal views and solicited their comments on the
proposed action and on the development of this rule. In the course of
this consultation, EPA and the Corps jointly participated in aspects of
the process.
The agencies began consultation with federally-recognized Indian
tribes on the Clean Water Rule defining ``waters of the United States''
in October 2011. The consultation and coordination process, including
providing information on the development of an accompanying science
report on the connectivity of streams and wetlands, continued, in
stages, over a four year period, until the close of the public comment
period on November 14, 2014. EPA invited tribes to provide written
input on the rulemaking throughout both the tribal consultation process
and public comment period.
EPA specifically consulted with tribal officials to gain an
understanding of, and to address, the tribal views on the proposed
rule. In 2011, close to 200 tribal representatives and more than 40
tribes participated in the consultation process, which included
multiple webinars and national teleconferences and face-to-face
meetings. In addition, EPA received written comments from three tribes
during the initial consultation period.
EPA continued to provide status updates to the National Tribal
Water Council and the National Tribal Caucus during 2012 through 2014.
The final consultation event was completed on October 23, 2014 as a
national teleconference with the Office of Water's Deputy Assistant
Administrator. Ultimately, EPA received an additional 23 letters from
tribes/tribal organizations by the completion of the consultation
period. The comments indicated that Tribes, overall, support increased
clarity of waters protected by the Clean Water Act, but some expressed
concern with the consultation process and the burden of any expanded
jurisdiction. The agencies considered the feedback received through
consultation and written comments in developing today's rule.
The agencies have prepared a report summarizing their consultation
with tribal nations, and how these results have informed the
development of this rule. This report, Final Summary of Tribal
Consultation for the Clean Water Rule: Definition of ``Waters of the
United States'' Under the Clean Water Act; Final Rule (Docket Id. No.
EPA-HQ-OW-2011-0880), is available in the docket for this rule.
G. Executive Order 13045: Protection of Children From Environmental
Health Risks and Safety Risks
This action is not subject to Executive Order 13045 (62 FR 19885,
April 23, 1997) because the environmental health or safety risks
addressed by this action do not present a disproportionate risk to
children.
H. Executive Order 13211: Actions Concerning Regulations That
Significantly Affect Energy Supply, Distribution, or Use
This action is not a ``significant energy action'' as defined in
Executive Order 13211 (66 FR 28355, May 22, 2001) because it is not
likely to have a significant adverse effect on the supply,
distribution, or use of energy.
I. National Technology Transfer and Advancement Act
Section 12(d) of the National Technology Transfer and Advancement
Act of 1995 (``NTTAA''), Public Law 104-113, 12(d) (15 U.S.C. 272 note)
directs federal agencies to use voluntary consensus standards in
regulatory activities unless to do so would be inconsistent with
applicable law or otherwise impractical. Voluntary consensus standards
are technical standards (e.g., materials specifications, test methods,
sampling procedures, and business practices) that are developed or
adopted by voluntary consensus standards bodies. NTTAA directs federal
agencies to provide Congress, through OMB, explanations when the agency
decides not to use available and applicable voluntary consensus
standards.
This rule does not involve technical standards. Therefore, the
agencies are not considering the use of any voluntary consensus
standards.
J. Executive Order 12898: Federal Actions To Address Environmental
Justice in Minority Populations and Low-Income Populations
Executive Order (E.O.) 12898 (59 FR 7629, Feb. 16, 1994)
establishes Federal executive policy on environmental justice. Its main
provision directs Federal agencies, to the greatest extent practicable
and permitted by law, to make environmental justice part of their
mission by identifying and addressing, as appropriate,
disproportionately high and adverse human health or environmental
effects of their programs, policies, and activities on minority
populations and low-income populations in the United States.
The agencies have determined that the rule will not have
disproportionately high and adverse
[[Page 37104]]
human health or environmental effects on minority or low-income
populations, because it does not adversely affect the level of
protection provided to human health or the environment.
The rule defines the scope of waters protected under the CWA. The
increased clarity regarding the definition of ``waters of the United
States'' is intended to benefit all regulators, stakeholders, and
interested parties. In addition, this rule is national in scope and,
therefore, is not specific to a particular geographic area.
In the spirit of E.O. 12898, input from environmental justice
stakeholders was requested during the rule development process, through
a series of stakeholder meetings between April and November 2014. On
May 12, 2014, EPA held a focused teleconference with non-traditional
stakeholders, including environmental justice and faith-based
stakeholders, to solicit their individual input on the proposed rule.
The agencies have used the feedback from public outreach as the source
of early guidance and recommendations for refining the proposed rule.
Stakeholder input received during public outreach events in combination
with the written comments received during the public comment period
have reshaped each of the definitions included in today's rule, and
incorporate increased clarity for regulators, stakeholders, and the
regulated public to assist them in identifying waters as ``waters of
the United States.''
The agencies prepared a report summarizing their outreach to the
environmental justice community, analysis of potential impacts, and how
these results informed the development of the rule. This report,
Environmental Justice Report for the Clean Water Rule: Definition of
``Waters of the United States'' Under the Clean Water Act; Final Rule
(Docket Id. No. EPA-HQ-OW-2011-0880), is available in the docket for
this rule.
K. Congressional Review Act
This action is subject to the Congressional Review Act (CRA), and
the agencies will submit a rule report to each House of the Congress
and to the Comptroller General of the United States. This action is a
``major rule'' as defined by 5 U.S.C. 804(2) based on potential
indirect costs.
L. Environmental Documentation
In this joint rulemaking, the agencies establish a definitional
rule that clarifies the scope of the Clean Water Act. The definition
will apply to all provisions of the Act, and this regulation
specifically amends EPA regulations implementing sections 301, 304,
306, 311, 402 and 404, while the Army is making substantively identical
revisions to its regulations under section 404 of the CWA. Section
511(c) of the Clean Water Act provides that, except for certain actions
not relevant here, no action by EPA constitutes `a major federal action
significantly affecting the quality of the human environment within the
meaning of [NEPA]''.
The Army has prepared a final environmental assessment and Findings
of No Significant Impact consistent with the National Environmental
Policy Act (NEPA). The Army has determined that the rule is not a major
federal action significantly affecting the quality of the human
environment that would require the preparation of an environmental
impact statement. The assessment is contained in the record for this
rulemaking. Furthermore, appropriate environmental documentation,
including an EIS when required, is prepared by the Corps for general
permits and specifically for each and every standard individual permit
application before making final permit decisions.
M. Judicial Review
Section 509(b)(1) of the CWA provides for judicial review in the
courts of appeals of specifically enumerated actions of the
Administrator. The Supreme Court and lower courts have reached
different conclusions on the types of actions that fall within section
509. Compare, E.I. du Pont de Nemours and Co. v. Train, 430 U.S. 112
(1977); NRDC v. EPA, 673 F.2d 400 (D.C. Cir. 1982); National Cotton
Council of Amer. v. EPA, 553 F.3d 927(6th Cir. 2009) cert denied 559
U.S. 936 (2010) with, Northwest Environmental Advocates v. EPA, 537
F.3d 1006 (9th Cir. 2008); Friends of the Everglades v. EPA, 699 F.3d
1280 (11th Cir. 2012) cert denied 559 U.S. 936 (2010).
See DATES section for information regarding the timing for seeking
judicial review of this rule.
List of Subjects
33 CFR Part 328
Environmental protection, Administrative practice and procedure,
Intergovernmental relations, Navigation, Water pollution control,
Waterways.
40 CFR Parts 110, 112, 116, 117, 122, 230, 232, 300, 301, and 401
Environmental protection, Water pollution control.
Dated: May 27, 2015.
Gina McCarthy,
Administrator, Environmental Protection Agency.
Dated: May 27, 2015.
Jo-Ellen Darcy,
Assistant Secretary of the Army, (Civil Works), Department of the Army.
Title 33--Navigation and Navigable Waters
For the reasons set out in the preamble, title 33, chapter II of
the Code of Federal Regulations is amended as follows:
PART 328--DEFINITION OF WATERS OF THE UNITED STATES
0
1. The authority citation for part 328 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
2. Section 328.3 is amended by revising paragraphs (a) through (c),
removing paragraphs (d) and (e), and redesignating paragraph (f) as
paragraph (d) to read as follows:
Sec. 328.3 Definitions.
* * * * *
(a) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(b) of this section, the term ``waters of the United States'' means:
(1) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(2) All interstate waters, including interstate wetlands;
(3) The territorial seas;
(4) All impoundments of waters otherwise identified as waters of
the United States under this section;
(5) All tributaries, as defined in paragraph (c)(3) of this
section, of waters identified in paragraphs (a)(1) through (3) of this
section;
(6) All waters adjacent to a water identified in paragraphs (a)(1)
through (5) of this section, including wetlands, ponds, lakes, oxbows,
impoundments, and similar waters;
(7) All waters in paragraphs (a)(7)(i) through (v) of this section
where they are determined, on a case-specific basis, to have a
significant nexus to a water identified in paragraphs (a)(1) through
(3) of this section. The waters identified in each of paragraphs
(a)(7)(i) through (v) of this section are similarly situated and shall
be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(a)(1)
[[Page 37105]]
through (3) of this section. Waters identified in this paragraph shall
not be combined with waters identified in paragraph (a)(6) of this
section when performing a significant nexus analysis. If waters
identified in this paragraph are also an adjacent water under paragraph
(a)(6), they are an adjacent water and no case-specific significant
nexus analysis is required.
(i) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(ii) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(iii) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(iv) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(v) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(8) All waters located within the 100-year floodplain of a water
identified in paragraphs (a)(1) through (3) of this section and all
waters located within 4,000 feet of the high tide line or ordinary high
water mark of a water identified in paragraphs (a)(1) through (5) of
this section where they are determined on a case-specific basis to have
a significant nexus to a water identified in paragraphs (a)(1) through
(3) of this section. For waters determined to have a significant nexus,
the entire water is a water of the United States if a portion is
located within the 100-year floodplain of a water identified in
paragraphs (a)(1) through (3) of this section or within 4,000 feet of
the high tide line or ordinary high water mark. Waters identified in
this paragraph shall not be combined with waters identified in
paragraph (a)(6) of this section when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (a)(6), they are an adjacent water and no case-
specific significant nexus analysis is required.
(b) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (a)(4) through (8) of
this section.
(1) Waste treatment systems, including treatment ponds or lagoons
designed to meet the requirements of the Clean Water Act.
(2) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(3) The following ditches:
(i) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(ii) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(iii) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (a)(1) through (3) of this
section.
(4) The following features:
(i) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(ii) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(iii) Artificial reflecting pools or swimming pools created in dry
land;
(iv) Small ornamental waters created in dry land;
(v) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(vi) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(vii) Puddles.
(5) Groundwater, including groundwater drained through subsurface
drainage systems.
(6) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(7) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(c) Definitions. In this section, the following definitions apply:
(1) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (a)(1) through (5) of this
section, including waters separated by constructed dikes or barriers,
natural river berms, beach dunes, and the like. For purposes of
adjacency, an open water such as a pond or lake includes any wetlands
within or abutting its ordinary high water mark. Adjacency is not
limited to waters located laterally to a water identified in paragraphs
(a)(1) through (5) of this section. Adjacent waters also include all
waters that connect segments of a water identified in paragraphs (a)(1)
through (5) or are located at the head of a water identified in
paragraphs (a)(1) through (5) of this section and are bordering,
contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(2) Neighboring. The term neighboring means:
(i) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (a)(1) through (5) of this
section. The entire water is neighboring if a portion is located within
100 feet of the ordinary high water mark;
(ii) All waters located within the 100-year floodplain of a water
identified in paragraphs (a)(1) through (5) of this section and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(iii) All waters located within 1,500 feet of the high tide line of
a water identified in paragraphs (a)(1) or (a)(3) of this section, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(3) Tributary and tributaries. The terms tributary and tributaries
each mean a water that contributes flow, either directly or through
another water (including an impoundment identified in paragraph (a)(4)
of this section), to a water identified in paragraphs (a)(1) through
(3) of this section that is characterized by the presence of the
physical indicators of a bed and banks and an ordinary high water mark.
These physical indicators demonstrate there is volume, frequency, and
duration of flow sufficient to create a bed and banks and an ordinary
high water mark, and thus to qualify as a tributary. A tributary can be
a natural, man-altered, or man-made water and includes waters such as
rivers, streams, canals, and ditches not excluded under paragraph (b)
of this
[[Page 37106]]
section. A water that otherwise qualifies as a tributary under this
definition does not lose its status as a tributary if, for any length,
there are one or more constructed breaks (such as bridges, culverts,
pipes, or dams), or one or more natural breaks (such as wetlands along
the run of a stream, debris piles, boulder fields, or a stream that
flows underground) so long as a bed and banks and an ordinary high
water mark can be identified upstream of the break. A water that
otherwise qualifies as a tributary under this definition does not lose
its status as a tributary if it contributes flow through a water of the
United States that does not meet the definition of tributary or through
a non-jurisdictional water to a water identified in paragraphs (a)(1)
through (3) of this section.
(4) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(5) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (a)(1) through (3) of this section. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (a)(1) through (3) of this section. For an
effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream paragraph (a)(1)
through (3) waters shall be assessed by evaluating the aquatic
functions identified in paragraphs (c)(5)(i) through (ix) of this
section. A water has a significant nexus when any single function or
combination of functions performed by the water, alone or together with
similarly situated waters in the region, contributes significantly to
the chemical, physical, or biological integrity of the nearest water
identified in paragraphs (a)(1) through (3) of this section. Functions
relevant to the significant nexus evaluation are the following:
(i) Sediment trapping,
(ii) Nutrient recycling,
(iii) Pollutant trapping, transformation, filtering, and transport,
(iv) Retention and attenuation of flood waters,
(v) Runoff storage,
(vi) Contribution of flow,
(vii) Export of organic matter,
(viii) Export of food resources, and
(ix) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (a)(1)
through (3) of this section.
(6) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(7) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
Title 40--Protection of Environment
For reasons set out in the preamble, title 40, chapter I of the
Code of Federal Regulations is amended as follows:
PART 110--DISCHARGE OF OIL
0
3. The authority citation for part 110 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq., 33 U.S.C. 1321(b)(3) and
(b)(4) and 1361(a); E.O. 11735, 38 FR 21243, 3 CFR parts 1971-1975
Comp., p. 793.
0
4. Section 110.1 is amended by removing the definition of ``wetlands''
and revising the definition of ``navigable waters'' to read as follows:
Sec. 110.1 Definitions.
* * * * *
Navigable waters means waters of the United States, including the
territorial seas.
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this section, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
[[Page 37107]]
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition or
within 4,000 feet of the high tide line or ordinary high water mark.
Waters identified in this paragraph shall not be combined with waters
identified in paragraph (1)(vi) of this definition when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (1)(vi), they are an adjacent
water and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this section.
(i) Waste treatment systems (other than cooling ponds meeting the
criteria of this paragraph) are not waters of the United States.
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(1) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (iii) of this definition, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this section), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this definition.
[[Page 37108]]
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 112--OIL POLLUTION PREVENTION
0
5. The authority citation for part 112 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
6. Section 112.2 is amended by removing the definition of ``wetlands''
and revising the definition of ``Navigable waters'' to read as follows:
Sec. 112.2 Definitions.
* * * * *
Navigable waters means waters of the United States, including the
territorial seas.
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this section when performing a significant nexus analysis.
If waters identified in this paragraph are also an adjacent water under
paragraph (1)(vi), they are an adjacent water and no case-specific
significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the
[[Page 37109]]
100-year floodplain of a water identified in paragraphs (1)(i) through
(iii) of this definition or within 4,000 feet of the high tide line or
ordinary high water mark. Waters identified in this paragraph shall not
be combined with waters identified in paragraph (1)(vi) of this
definition when performing a significant nexus analysis. If waters
identified in this paragraph are also an adjacent water under paragraph
(1)(vi), they are an adjacent water and no case-specific significant
nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(ii) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(iii) Groundwater, including groundwater drained through subsurface
drainage systems.
(iv) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(v) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (1)(iii) of this definition,
and all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
[[Page 37110]]
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this section.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 116--DESIGNATION OF HAZARDOUS SUBSTANCE
0
7. The authority citation for part 116 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
8. Section 116.3 is amended by revising the definition of ``Navigable
waters'' to read as follows:
Sec. 116.3 Definitions.
* * * * *
Navigable waters is defined in section 502(7) of the Act to mean
``waters of the United States, including the territorial seas.''
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition or
within 4,000 feet of the high tide line or ordinary high water mark.
Waters identified in this paragraph shall not be combined with waters
identified in paragraph (1)(vi) of this definition when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (1)(vi), they are an adjacent
water and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(ii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(iii) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
[[Page 37111]]
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(iv) Groundwater, including groundwater drained through subsurface
drainage systems.
(v) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vi) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (1)(iii) of this definition,
and all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider
[[Page 37112]]
the characteristics of the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 117--DETERMINATION OF REPORTABLE QUANTITIES FOR HAZARDOUS
SUBSTANCES
0
9. The authority citation for part 117 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq. and Executive Order 11735,
superseded by Executive Order 12777, 56 FR 54757.
0
10. Section 117.1 is amended by revising paragraph (i) to read as
follows:
Sec. 117.1 Definitions.
* * * * *
(i) Navigable waters is defined in section 502(7) of the Act to
mean ``waters of the United States, including the territorial seas.''
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(i)(2) of this section, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (i)(3)(iii) of this
section, of waters identified in paragraphs (i)(1)(i) through (iii) of
this section;
(vi) All waters adjacent to a water identified in paragraphs
(i)(1)(i) through (v) of this section, including wetlands, ponds,
lakes, oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (i)(1)(vii)(A) through (E) of this
section where they are determined, on a case-specific basis, to have a
significant nexus to a water identified in paragraphs (i)(1)(i) through
(iii) of this section. The waters identified in each of paragraphs
(i)(1)(vii)(A) through (E) of this section are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(i)(1)(i) through (iii) of this section. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(i)(1)(vi) of this section when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (i)(1)(vi), they are an adjacent water and no
case-specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in (i)(1)(i) through (iii) of this section and all waters
located within 4,000 feet of the high tide line or ordinary high water
mark of a water identified in paragraphs (i)(1)(i) through (v) of this
section where they are determined on a case-specific basis to have a
significant nexus to a water identified in paragraphs (i)(1)(i) through
(iii) of this section. For waters determined to have a significant
nexus, the entire water is a water of the United States if a portion is
located within the 100-year floodplain of a water identified in
paragraphs (i)(1)(i) through (iii) of this section or within 4,000 feet
of the high tide line or ordinary high water mark. Waters identified in
this paragraph shall not be combined with waters identified in
paragraph (i)(1)(vi) of this section when performing a significant
nexus analysis. If waters identified in this paragraph are also an
adjacent water under paragraph (i)(1)(vi), they are an adjacent water
and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (i)(1)(iv) through
(viii) of this section.
(i) Waste treatment systems, (other than cooling ponds meeting the
criteria of this paragraph) are not waters of the United States.
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (i)(1)(i) through (iii) of
this section.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
[[Page 37113]]
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this paragraph, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (i)(1)(i) through (v) of
this section, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (i)(1)(i) through (v) of this section. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (i)(1)(i) through (v) or are located at the head of a water
identified in paragraphs (i)(1)(i) through (v) of this section and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (i)(1)(i) through (v) of this
section. The entire water is neighboring if a portion is located within
100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (i)(1)(i) through (v) of this section and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (i)(1)(i) or (iii) of this section, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(i)(1)(iv) of this section), to a water identified in paragraphs
(i)(1)(i) through (iii) of this section that is characterized by the
presence of the physical indicators of a bed and banks and an ordinary
high water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (i)(2) of this section. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (i)(1)(i) through (iii) of this section.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (i)(1)(i) through (iii) of this section. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (i)(1)(i) through (iii) of this section. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (i)(1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (i)(3)(v)(A) through (I) of this section. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (i)(1)(i) through (iii) of this section.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (i)(1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
[[Page 37114]]
PART 122--EPA ADMINISTERED PERMIT PROGRAMS: THE NATIONAL POLLUTANT
DISCHARGE ELIMINATION SYSTEM
0
11. The authority citation for part 122 continues to read as follows:
Authority: The Clean Water Act, 33 U.S.C. 1251 et seq.
0
12. Section 122.2 is amended by:
0
a. Lifting the suspension of the last sentence of the definition of
``Waters of the United States'' published July 21, 1980 (45 FR 48620);
0
b. Removing the definition of ``wetlands'' and revising the definition
of ``Waters of the United States'' and
0
c. Suspending the last sentence of the definition of ``Waters of the
United States'' published July 21, 1980 (45 FR 48620).
The revision reads as follows:
Sec. 122.2 Definitions.
* * * * *
Waters of the United States or waters of the U.S. means:
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
section, of waters identified in paragraphs (1)(i) through (iii) of
this section;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (v) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the 100-year floodplain of a water
identified in (1)(i) through (iii) of this definition or within 4,000
feet of the high tide line or ordinary high water mark. Waters
identified in this paragraph shall not be combined with waters
identified in paragraph (1)(vi) of this definition when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (1)(vi), they are an adjacent
water and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) Waste treatment systems, including treatment ponds or lagoons
designed to meet the requirements of the Clean Water Act. This
exclusion applies only to manmade bodies of water which neither were
originally created in waters of the United States (such as disposal
area in wetlands) nor resulted from the impoundment of waters of the
United States. [See Note 1 of this section.]
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
[[Page 37115]]
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (iii) of this definition, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 230--SECTION 404(b)(1) GUIDELINES FOR SPECIFICATION OF
DISPOSAL SITES FOR DREDGED OR FILL MATERIAL
0
13. The authority citation for part 230 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
14. Section 230.3 is amended by:
0
a. Removing paragraph (b) and reserved paragraphs (f), (g), (j) and
(l).
[[Page 37116]]
0
b. Redesignating paragraphs (c) through (e) as paragraphs (b) through
(d).
0
c. Redesignating paragraphs (h) and (i) as paragraphs (e) and (f).
0
d. Redesignating paragraph (k) as paragraph (g).
0
e. Redesignating paragraphs (m) through (q) as paragraphs (h) through
(l).
0
f. Redesignating paragraph (q-1) as paragraph (m).
0
g. Redesignating paragraph (r) as paragraph (n).
0
h. Redesignating paragraph (s) as paragraph (o).
0
i. Revising newly redesignated paragraph (o).
0
j. Removing paragraph (t).
The revision reads as follows:
Sec. 230.3 Definitions.
* * * * *
(o) The term waters of the United States means:
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(o)(2) of this section, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (o)(3)(iii) of this
section, of waters identified in paragraphs (o)(1)(i) through (iii) of
this section;
(vi) All waters adjacent to a water identified in paragraphs
(o)(1)(i) through (v) of this section, including wetlands, ponds,
lakes, oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (o)(1)(vii)(A) through (E) of this
section where they are determined, on a case-specific basis, to have a
significant nexus to a water identified in paragraphs (o)(1)(i) through
(iii) of this section. The waters identified in each of paragraphs
(o)(1)(vii)(A) through (E) of this section are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(o)(1)(i) through (iii) of this section. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(o)(1)(vi) of this section when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (o)(1)(vi), they are an adjacent water and no
case-specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (o)(1)(i) through (iii) of this section and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (o)(1)(i) through
(v) of this section where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs
(o)(1)(i) through (iii) of this section. For waters determined to have
a significant nexus, the entire water is a water of the United States
if a portion is located within the 100-year floodplain of a water
identified in paragraphs (o)(1)(i) through (iii) of this section or
within 4,000 feet of the high tide line or ordinary high water mark.
Waters identified in this paragraph shall not be combined with waters
identified in paragraph (o)(1)(vi) of this section when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (o)(1)(vi), they are an adjacent
water and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (o)(1)(iv) through
(viii) of this section.
(i) Waste treatment systems, including treatment ponds or lagoons
designed to meet the requirements of the Clean Water Act are not waters
of the United States.
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (o)(1)(i) through (iii) of
this section.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this paragraph (o), the following definitions apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (o)(1)(i) through (v) of
this section, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of
[[Page 37117]]
adjacency, an open water such as a pond or lake includes any wetlands
within or abutting its ordinary high water mark. Adjacency is not
limited to waters located laterally to a water identified in paragraphs
(o)(1)(i) through (v) of this section. Adjacent waters also include all
waters that connect segments of a water identified in paragraphs
(o)(1)(i) through (v) or are located at the head of a water identified
in paragraphs (o)(1)(i) through (v) of this section and are bordering,
contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (o)(1)(i) through (v) of this
section. The entire water is neighboring if a portion is located within
100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (o)(1)(i) through (v) of this section and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (o)(1)(i) or (iii) of this section, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(o)(1)(iv) of this section), to a water identified in paragraphs
(o)(1)(i) through (iii) of this section that is characterized by the
presence of the physical indicators of a bed and banks and an ordinary
high water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (o)(2) of this section. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (o)(1)(i) through (iii) of this section.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (o)(1)(i) through (iii) of this section. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (o)(1)(i) through (iii) of this section. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (o)(1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (o)(3)(v)(A) through (I) of this section. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (o)(1)(i) through (iii) of this section.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (o)(1)
through (3) of this section.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 232--404 PROGRAMS DEFINITIONS; EXEMPT ACTIVITIES NOT REQUIRING
404 PERMITS
0
15. The authority citation for part 230 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
16. Section 232.2 is amended by removing the definition of ``wetlands''
and revising the definition of ``Waters of the United States'' to read
as follows:
Sec. 232.2 Definitions.
* * * * *
Waters of the United States means:
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this
[[Page 37118]]
definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition or
within 4,000 feet of the high tide line or ordinary high water mark.
Waters identified in this paragraph shall not be combined with waters
identified in paragraph (1)(vi) of this definition when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (1)(vi) of this definition, they
are an adjacent water and no case-specific significant nexus analysis
is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) Waste treatment systems, including treatment ponds or lagoons
designed to meet the requirements of the Clean Water Act are not waters
of the United States.
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
[[Page 37119]]
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (1)(iii) of this definition,
and all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 300--NATIONAL OIL AND HAZARDOUS SUBSTANCES POLLUTION
CONTINTENCY PLAN
0
17. The authority citation for part 300 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
18. Section 300.5 is amended by revising the definition of ``navigable
waters'' to read as follows:
Sec. 300.5 Definitions.
* * * * *
Navigable waters means the waters of the United States, including
the territorial seas.
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition
[[Page 37120]]
where they are determined, on a case-specific basis, to have a
significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition or
within 4,000 feet of the high tide line or ordinary high water mark.
Waters identified in this paragraph shall not be combined with waters
identified in paragraph (1)(vi) of this definition when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (1)(vi), they are an adjacent
water and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) Waste treatment systems (other than cooling ponds meeting the
criteria of this paragraph) are not waters of the United States.
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (1)(iii) of this definition,
and all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is
[[Page 37121]]
characterized by the presence of the physical indicators of a bed and
banks and an ordinary high water mark. These physical indicators
demonstrate there is volume, frequency, and duration of flow sufficient
to create a bed and banks and an ordinary high water mark, and thus to
qualify as a tributary. A tributary can be a natural, man-altered, or
man-made water and includes waters such as rivers, streams, canals, and
ditches not excluded under paragraph (2) of this definition. A water
that otherwise qualifies as a tributary under this definition does not
lose its status as a tributary if, for any length, there are one or
more constructed breaks (such as bridges, culverts, pipes, or dams), or
one or more natural breaks (such as wetlands along the run of a stream,
debris piles, boulder fields, or a stream that flows underground) so
long as a bed and banks and an ordinary high water mark can be
identified upstream of the break. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if it contributes flow through a water of the United States that does
not meet the definition of tributary or through a non-jurisdictional
water to a water identified in paragraphs (1)(i) through (iii) of this
definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this definition.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
0
19. In appendix E to part 300, section 1.5 Definitions is amended by
revising the definition of ``navigable waters'' to read as follows:
Appendix E to Part 300--Oil Spill Response
* * * * *
1.5 Definitions. * * *
Navigable waters means the waters of the United States, including
the territorial seas.
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands
[[Page 37122]]
found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus, the entire water is a water of the United States if
a portion is located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition or
within 4,000 feet of the high tide line or ordinary high water mark.
Waters identified in this paragraph shall not be combined with waters
identified in paragraph (1)(vi) of this definition when performing a
significant nexus analysis. If waters identified in this paragraph are
also an adjacent water under paragraph (1)(vi), they are an adjacent
water and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) Waste treatment systems (other than cooling ponds meeting the
criteria of this paragraph) are not waters of the United States.
(ii) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(iii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(iv) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(v) Groundwater, including groundwater drained through subsurface
drainage systems.
(vi) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vii) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (1)(iii) of this definition,
and all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
[[Page 37123]]
in paragraphs (1)(i) through (iii) of this definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 302--DESIGNATION, REPORTABLE QUANTITIES, AND NOTIFICATION
0
20. The authority citation for part 302 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
21. Section 302.3 is amended by revising the definition of ``Navigable
waters'' to read as follows:
Sec. 302.3 Definitions.
* * * * *
Navigable waters means the waters of the United States, including
the territorial seas.
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(2) of this definition, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (3)(iii) of this
definition, of waters identified in paragraphs (1)(i) through (iii) of
this definition;
(vi) All waters adjacent to a water identified in paragraphs (1)(i)
through (v) of this definition, including wetlands, ponds, lakes,
oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (1)(vii)(A) through (E) of this
definition where they are determined, on a case-specific basis, to have
a significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this definition. The waters identified in each of paragraphs
(1)(vii)(A) through (E) of this definition are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(1)(i) through (iii) of this definition. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(1)(vi) of this definition when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (1)(vi), they are an adjacent water and no case-
specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (iii) of this definition and
all waters located within 4,000 feet of the high tide line or ordinary
high water mark of a water identified in paragraphs (1)(i) through (v)
of this definition where they are determined on a case-specific basis
to have a significant nexus to a water identified in paragraphs (1)(i)
through (iii) of this definition. For waters determined to have a
significant nexus,
[[Page 37124]]
the entire water is a water of the United States if a portion is
located within the 100-year floodplain of a water identified in
paragraphs (1)(i) through (iii) of this definition or within 4,000 feet
of the high tide line or ordinary high water mark. Waters identified in
this paragraph shall not be combined with waters identified in
paragraph (1)(vi) of this definition when performing a significant
nexus analysis. If waters identified in this paragraph are also an
adjacent water under paragraph (1)(vi), they are an adjacent water and
no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (1)(iv) through
(viii) of this definition.
(i) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (1)(i) through (iii) of
this definition.
(ii) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(iii) Groundwater, including groundwater drained through subsurface
drainage systems.
(iv) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(v) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this definition, the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (1)(i) through (v) of this
definition, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (1)(i) through (v) of this definition. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (1)(i) through (v) or are located at the head of a water
identified in paragraphs (1)(i) through (v) of this definition and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (1)(i) through (v) of this
definition. The entire water is neighboring if a portion is located
within 100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (1)(i) through (v) of this definition and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (1)(i) or (iii) of this definition, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(1)(iv) of this definition), to a water identified in paragraphs (1)(i)
through (iii) of this definition that is characterized by the presence
of the physical indicators of a bed and banks and an ordinary high
water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (2) of this definition. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (1)(i) through (iii) of this definition.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (1)(i) through (iii) of this definition. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (1)(i) through (iii) of this definition. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (3)(v)(A) through (I) of this definition. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with
[[Page 37125]]
similarly situated waters in the region, contributes significantly to
the chemical, physical, or biological integrity of the nearest water
identified in paragraphs (1)(i) through (iii) of this definition.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
PART 401--GENERAL PROVISIONS
0
22. The authority citation for part 401 is revised to read as follows:
Authority: 33 U.S.C. 1251 et seq.
0
23. Section 401.11 is amended by revising paragraph (l) to read as
follows:
Sec. 401.11 General definitions.
* * * * *
(l) The term navigable waters means the waters of the United
States, including the territorial seas.
(1) For purposes of the Clean Water Act, 33 U.S.C. 1251 et seq. and
its implementing regulations, subject to the exclusions in paragraph
(l)(2) of this section, the term ``waters of the United States'' means:
(i) All waters which are currently used, were used in the past, or
may be susceptible to use in interstate or foreign commerce, including
all waters which are subject to the ebb and flow of the tide;
(ii) All interstate waters, including interstate wetlands;
(iii) The territorial seas;
(iv) All impoundments of waters otherwise identified as waters of
the United States under this section;
(v) All tributaries, as defined in paragraph (l)(3)(iii) of this
section, of waters identified in paragraphs (l)(1)(i) through (iii) of
this section;
(vi) All waters adjacent to a water identified in paragraphs
(l)(1)(i) through (v) of this section, including wetlands, ponds,
lakes, oxbows, impoundments, and similar waters;
(vii) All waters in paragraphs (l)(1)(vii)(A) through (E) of this
section where they are determined, on a case-specific basis, to have a
significant nexus to a water identified in paragraphs (1)(i) through
(iii) of this section. The waters identified in each of paragraphs
(l)(1)(vii)(A) through (E) of this section are similarly situated and
shall be combined, for purposes of a significant nexus analysis, in the
watershed that drains to the nearest water identified in paragraphs
(l)(1)(i) through (iii) of this section. Waters identified in this
paragraph shall not be combined with waters identified in paragraph
(l)(1)(vi) of this section when performing a significant nexus
analysis. If waters identified in this paragraph are also an adjacent
water under paragraph (l)(1)(vi), they are an adjacent water and no
case-specific significant nexus analysis is required.
(A) Prairie potholes. Prairie potholes are a complex of glacially
formed wetlands, usually occurring in depressions that lack permanent
natural outlets, located in the upper Midwest.
(B) Carolina bays and Delmarva bays. Carolina bays and Delmarva
bays are ponded, depressional wetlands that occur along the Atlantic
coastal plain.
(C) Pocosins. Pocosins are evergreen shrub and tree dominated
wetlands found predominantly along the Central Atlantic coastal plain.
(D) Western vernal pools. Western vernal pools are seasonal
wetlands located in parts of California and associated with topographic
depression, soils with poor drainage, mild, wet winters and hot, dry
summers.
(E) Texas coastal prairie wetlands. Texas coastal prairie wetlands
are freshwater wetlands that occur as a mosaic of depressions, ridges,
intermound flats, and mima mound wetlands located along the Texas Gulf
Coast.
(viii) All waters located within the 100-year floodplain of a water
identified in (l)(1)(i) through (iii) of this section and all waters
located within 4,000 feet of the high tide line or ordinary high water
mark of a water identified in paragraphs (l)(1)(i) through (v) of this
section where they are determined on a case-specific basis to have a
significant nexus to a water identified in paragraphs (l)(1)(i) through
(iii) of this section. For waters determined to have a significant
nexus, the entire water is a water of the United States if a portion is
located within the 100-year floodplain of a water identified in
paragraphs (l)(1)(i) through (iii) of this section or within 4,000 feet
of the high tide line or ordinary high water mark. Waters identified in
this paragraph shall not be combined with waters identified in
paragraph (l)(1)(vi) of this section when performing a significant
nexus analysis. If waters identified in this paragraph are also an
adjacent water under paragraph (l)(1)(vi), they are an adjacent water
and no case-specific significant nexus analysis is required.
(2) The following are not ``waters of the United States'' even
where they otherwise meet the terms of paragraphs (l)(1)(iv) through
(viii) of this section.
(i) Prior converted cropland. Notwithstanding the determination of
an area's status as prior converted cropland by any other Federal
agency, for the purposes of the Clean Water Act, the final authority
regarding Clean Water Act jurisdiction remains with EPA.
(ii) The following ditches:
(A) Ditches with ephemeral flow that are not a relocated tributary
or excavated in a tributary.
(B) Ditches with intermittent flow that are not a relocated
tributary, excavated in a tributary, or drain wetlands.
(C) Ditches that do not flow, either directly or through another
water, into a water identified in paragraphs (l)(1)(i) through (iii) of
this section.
(iii) The following features:
(A) Artificially irrigated areas that would revert to dry land
should application of water to that area cease;
[[Page 37126]]
(B) Artificial, constructed lakes and ponds created in dry land
such as farm and stock watering ponds, irrigation ponds, settling
basins, fields flooded for rice growing, log cleaning ponds, or cooling
ponds;
(C) Artificial reflecting pools or swimming pools created in dry
land;
(D) Small ornamental waters created in dry land;
(E) Water-filled depressions created in dry land incidental to
mining or construction activity, including pits excavated for obtaining
fill, sand, or gravel that fill with water;
(F) Erosional features, including gullies, rills, and other
ephemeral features that do not meet the definition of tributary, non-
wetland swales, and lawfully constructed grassed waterways; and
(G) Puddles.
(iv) Groundwater, including groundwater drained through subsurface
drainage systems.
(v) Stormwater control features constructed to convey, treat, or
store stormwater that are created in dry land.
(vi) Wastewater recycling structures constructed in dry land;
detention and retention basins built for wastewater recycling;
groundwater recharge basins; percolation ponds built for wastewater
recycling; and water distributary structures built for wastewater
recycling.
(3) In this paragraph (l), the following terms apply:
(i) Adjacent. The term adjacent means bordering, contiguous, or
neighboring a water identified in paragraphs (l)(1)(i) through (v) of
this section, including waters separated by constructed dikes or
barriers, natural river berms, beach dunes, and the like. For purposes
of adjacency, an open water such as a pond or lake includes any
wetlands within or abutting its ordinary high water mark. Adjacency is
not limited to waters located laterally to a water identified in
paragraphs (l)(1)(i) through (v) of this section. Adjacent waters also
include all waters that connect segments of a water identified in
paragraphs (l)(1)(i) through (v) or are located at the head of a water
identified in paragraphs (l)(1)(i) through (v) of this section and are
bordering, contiguous, or neighboring such water. Waters being used for
established normal farming, ranching, and silviculture activities (33
U.S.C. 1344(f)) are not adjacent.
(ii) Neighboring. The term neighboring means:
(A) All waters located within 100 feet of the ordinary high water
mark of a water identified in paragraphs (l)(1)(i) through (v) of this
section. The entire water is neighboring if a portion is located within
100 feet of the ordinary high water mark;
(B) All waters located within the 100-year floodplain of a water
identified in paragraphs (l)(1)(i) through (v) of this section and not
more than 1,500 feet from the ordinary high water mark of such water.
The entire water is neighboring if a portion is located within 1,500
feet of the ordinary high water mark and within the 100-year
floodplain;
(C) All waters located within 1,500 feet of the high tide line of a
water identified in paragraphs (l)(1)(i) or (iii) of this section, and
all waters within 1,500 feet of the ordinary high water mark of the
Great Lakes. The entire water is neighboring if a portion is located
within 1,500 feet of the high tide line or within 1,500 feet of the
ordinary high water mark of the Great Lakes.
(iii) Tributary and tributaries. The terms tributary and
tributaries each mean a water that contributes flow, either directly or
through another water (including an impoundment identified in paragraph
(l)(1)(iv) of this section), to a water identified in paragraphs
(l)(1)(i) through (iii) of this section that is characterized by the
presence of the physical indicators of a bed and banks and an ordinary
high water mark. These physical indicators demonstrate there is volume,
frequency, and duration of flow sufficient to create a bed and banks
and an ordinary high water mark, and thus to qualify as a tributary. A
tributary can be a natural, man-altered, or man-made water and includes
waters such as rivers, streams, canals, and ditches not excluded under
paragraph (l)(2) of this section. A water that otherwise qualifies as a
tributary under this definition does not lose its status as a tributary
if, for any length, there are one or more constructed breaks (such as
bridges, culverts, pipes, or dams), or one or more natural breaks (such
as wetlands along the run of a stream, debris piles, boulder fields, or
a stream that flows underground) so long as a bed and banks and an
ordinary high water mark can be identified upstream of the break. A
water that otherwise qualifies as a tributary under this definition
does not lose its status as a tributary if it contributes flow through
a water of the United States that does not meet the definition of
tributary or through a non-jurisdictional water to a water identified
in paragraphs (l)(1)(i) through (iii) of this section.
(iv) Wetlands. The term wetlands means those areas that are
inundated or saturated by surface or groundwater at a frequency and
duration sufficient to support, and that under normal circumstances do
support, a prevalence of vegetation typically adapted for life in
saturated soil conditions. Wetlands generally include swamps, marshes,
bogs, and similar areas.
(v) Significant nexus. The term significant nexus means that a
water, including wetlands, either alone or in combination with other
similarly situated waters in the region, significantly affects the
chemical, physical, or biological integrity of a water identified in
paragraphs (l)(1)(i) through (iii) of this section. The term ``in the
region'' means the watershed that drains to the nearest water
identified in paragraphs (l)(1)(i) through (iii) of this section. For
an effect to be significant, it must be more than speculative or
insubstantial. Waters are similarly situated when they function alike
and are sufficiently close to function together in affecting downstream
waters. For purposes of determining whether or not a water has a
significant nexus, the water's effect on downstream (1)(i) through
(iii) waters shall be assessed by evaluating the aquatic functions
identified in paragraphs (l)(3)(v)(A) through (I) of this section. A
water has a significant nexus when any single function or combination
of functions performed by the water, alone or together with similarly
situated waters in the region, contributes significantly to the
chemical, physical, or biological integrity of the nearest water
identified in paragraphs (l)(1)(i) through (iii) of this section.
Functions relevant to the significant nexus evaluation are the
following:
(A) Sediment trapping,
(B) Nutrient recycling,
(C) Pollutant trapping, transformation, filtering, and transport,
(D) Retention and attenuation of flood waters,
(E) Runoff storage,
(F) Contribution of flow,
(G) Export of organic matter,
(H) Export of food resources, and
(I) Provision of life cycle dependent aquatic habitat (such as
foraging, feeding, nesting, breeding, spawning, or use as a nursery
area) for species located in a water identified in paragraphs (l)(1)(i)
through (iii) of this section.
(vi) Ordinary high water mark. The term ordinary high water mark
means that line on the shore established by the fluctuations of water
and indicated by physical characteristics such as a clear, natural line
impressed on the bank, shelving, changes in the character of soil,
destruction of terrestrial vegetation, the presence of litter and
debris, or other appropriate means that consider the characteristics of
the surrounding areas.
[[Page 37127]]
(vii) High tide line. The term high tide line means the line of
intersection of the land with the water's surface at the maximum height
reached by a rising tide. The high tide line may be determined, in the
absence of actual data, by a line of oil or scum along shore objects, a
more or less continuous deposit of fine shell or debris on the
foreshore or berm, other physical markings or characteristics,
vegetation lines, tidal gages, or other suitable means that delineate
the general height reached by a rising tide. The line encompasses
spring high tides and other high tides that occur with periodic
frequency but does not include storm surges in which there is a
departure from the normal or predicted reach of the tide due to the
piling up of water against a coast by strong winds such as those
accompanying a hurricane or other intense storm.
* * * * *
[FR Doc. 2015-13435 Filed 6-26-15; 8:45 am]
BILLING CODE 6560-50-P