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Fe bruary 1, 2(J()()
File '\0. 24-l)l)-(J14-()()I-(Jl
\11. Randy Kline
Jefferson County Department of Community Development
1'12 I Sheridan Street
Port TCl\vnsencL W;\ l)x3nX
Subject: Port Ludlo\\ Marina Expansion Project
Dear \1r. Kline:
This is a follow up to my phone conversation and e-mails to you regarding the above
referenced project. Port Ludlow Marina proposes to expand its existing 3S0-slip marina
by adding I (J(J slips.
We will be holding a site visit for this project on February 9,2000, from 10:45 a.m. to
12:3() p.m. at the Port Ludlow Marina. We will first view the site then move to a
nearby conference space to discuss the project in greater detail. There is a ferry from
Seattle to Bainbridge leaving at 9:25 a.m. that would allow you to arrive at Port Ludlow
about ]()AS. From Edmonds, the 9:25 a.m. ferry will allow you to arrive at about
l(U(J. We will meet at the Marina Offices. Driving directions from the Hoods Canal
Bridge to Port Ludlo\N are enclosed.
ALso, enclosed is a copy of the preliminary site plan and draft Biological Evaluation
(BE) for your ITVIC\\. The BE document contains the project description, project
location, and biological impacts associated with the proposed project. We will provide
you with additional information about the project at our site visit. Please note these are
all In preliminary form, subject to change based on the outcome of our conversation.
There will be a pre-conference meeting for this project with the Corps of Engineers on
Wednesday, February IS, 2(J(J(J, at 9:3(J a.m.
SII1cerely,
Reid Middleton, Inc.
'\ ico Ie Faghin
Senior Planner
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Enclosures
cc: Jon Rose
Jon Houghton
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JEfFERSON COUNTY
OEPT. OF COMMUNITY DEVELOPMENT
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Port Ludlow Marina Expansion
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Biological Evaluation
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Preliminary Draft Report
...... Prepared for:
...... Reid Middleton, Inc.
Prepared by:
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Pentec Environmental
i Project No. 007-040
l.... 120 Third Avenue S, Suite 110
Edmonds, W A 98020
..,..., (425) 775-4682
February 1, 2000
.......
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Port Ludlow Marina Expansion
Biological Evaluation
Preliminary Draft Report
Prepared for:
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Reid Middleton, Inc.
728 - 134th Street SW, Suite 200
Everett, W A 98204
Prepared by:
Pentec Environmental
Project No. 007-040
120 Third Avenue S, Suite 110
Edmonds, W A 98020
(425) 775-4682
February 1, 2000
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TABLE OF CONTENTS
1.0 I ntrod uction .... ........................ ........... ....... ...... ....... ...... ...... ..... ...... ...... ............ ........ 1
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2.0 Project Descri ption ..... ........ ..... ..... ..... ............... ......... ........ .... ...... ... ...... ...... ............ .3
2.1 Location and Description of Project Area ........................................................................ 3
2.2 Action Area................ ......... .......... ..... ....... .................... ............... ........... ....... ...... .......... '" 3
2.3 Project Description .............................. ............................................................................. 3
3.0 Species and .Habitat... ...... ..... .......... ........................ ....... ...... .... ....... .......... ..... ......... 7
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3.1 Species Information.......................................................................................................... 7
3.1.1 Chinook Salmon .................................................................................................... 8
3.1.2 Coho Salmon.. .......... .......... ..... ......................... ....... ............... .......... .......... ......... 10
3.1.3 Chum Salmon ...... ..... ........... .......... ..................................... ..... ........ ....... ............. 11
3.1.4 Bull Trout....... ..... ...... ..... ...................... ............................... ............... .......... ....... 12
3.1.5 Bald Eagle....... ............ ........... ...... ...... .................... ~. ............... .......... ....... ........... 13
3.1.6 Marbled Murrelet........................ .... ........ ....... ........... ......... ..... ........ ......... ........ .... 15
3.2 Existing Environmental Conditions..... ...................'.. ...... ............ ........... ........ ........ ......... 17
3.2.1 Water Quality and Stormwater ............................................................................ 17
3.2.2 Sediment Quality.. ............... .................... ............... ............... .......... .............. ...... 19
3.2.3 Habitat....... ........ ..... ............. ..... ............ ......... ..... .............. .................. .......... ....... 20
3.2.4 Biota....... ..................... ......... ........ ............ ...... .......... ............... .......... ..... ....... ...... 22
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4.0 Effects of the Action ............................................................................................ 25
4.1 Effects Analysis.......... ........... ............ ...... ........ ..... ............ ........ ......... ................. ............ 25
4.1.1 Construction Disturbances............................. ............ .......... ................ .......... ...... 25
4.1.2 Water Quality.... ............................. ...... .............. .......... .... ...... ................... .......... 27
4.1.3 Sediment Quality......... .................... ........ ....... .......... ............ ... .............. ........ ...... 28
4.1.4 Habitat Conditions.... ............... ....... ...................... .................................... ........... 29
4.1.5 Biota............... .................................................. ...................... ................. ............ 29
4.1.6 Net Effects of Action ............................................................................................ 30
4.1.7 Cumulative, Interdependent, and Interrelated Effects ......................................... 31
4.2 Take Analysis ..... ....... ........... ............ ....... ..... ......... ..... ........ ............. ........... ...... .............. 31
4.3 Conservation Measures........ ......... ............... ..... ...... .......... ........... ........... ....... ......... ........ 32
4.4 Determination of Effects......... ............ ............ ....... ...... ...... ....... ............... ......... ........ ...... 32
4.4.1 Salmonids...... ............. ........... ................. ......... ...... .............. ............... ................. 33
4.4.2 Birds.................................................................................................................... 33
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5.0 References .................. ....... ..... ...... ...... ...... ........ .............. ..... ...... ...... ............. ........ 35
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LIST OF FIGURES
Figure 1 Site vicinity map...... ....... ........ .......... ..... ................. ........ ........... ..... ....... ................ ........ 4
Figure 2 Plan view of proposed XXXX ...................................................................................... 5
Figure 3 Timing of salmon freshwater life phases in the Quilcene Basin................................... 9
LIST OF TABLES
Table 1 Pathways and indicators for evaluating salmon habitat in the urban estuary.............. 18
Table 2 Summary of sediment metals concentrations (mg/kg) in Port Ludlow
Marina sediments collected between 1987 and 1995 compared with
their respective Sediment Quality Standards ..............................................................20
Table 3 Net effects of the action on relevant pathways and indicators.................................... 26
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PORT LUDLOW MARINA EXPANSION
BIOLOGICAL EVALUATION
1.0 INTRODUCTION
The National Marine Fisheries Service (NMFS) formalized the listing of Puget Sound
chinook salmon (Oncorhynchus tshawytscha) and Hood Canal summer-run chum salmon
(0. keta) as threatened under the Endangered Species Act (ESA) on May 24, 1999, and
March 25, 1999, respectively. NMFS has designated the coho salmon (0. kisutch) as a candidate
for listing. The US Fish and Wildlife Service (USFWS) listed bull trout (Salvelinus confluentus)
in Puget Sound as threatened, effective December 1, 1999. Section 7 of the ESA requires that
any action by a federal agency is "not likely to jeopardize the continued existence of any [listed]
species or result in the destruction or adverse modification of habitat of such species...." The
Port Ludlow Marina Expansion project qualifies as such an action. Under ESA Section 7(c), the
lead federal agency, in this case the Corps, must prepare a biological evaluation (BE) of the
potential influence of its action (permitting the expansion of the Port Ludlow Marina) on listed
species or their critical habitat. Depending on the conclusion of the BE, the Corps may be
required to confer formally with NMFS or USFWS regarding the project.
This BE is being prepared for Corps review and possible submittal to NMFS and USFWS as
an aid to ESA decision-making regarding the potential effects of the Port Ludlow Marina
Expansion project. This BE addresses the potential effects of the proposed project on chinook
salmon, coho salmon, and bull trout, and their habitat. In addition, the bald eagle (Haliaeetus
leucocephalus) and marbled murrelet (Brachyramphus marmoratus) are federally listed
threatened species that may occur in the project area and are addressed in this BE.
Other threatened or endangered species that may occur in Puget Sound include the Steller sea
lion (Eumetopias jubatus; threatened), the humpback whale (Megaptera novaeangliae;
endangered) and the leatherback turtle (Dermochelys coriacea; endangered). However, these
species are extremely unlikely to occur in the project area (defined in Section 2.1) and are
therefore not covered in this BE.
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2.0 PROJECT DESCRIPTION
2.1 LOCATION AND DESCRIPTION OF PROJECT AREA
The "project area" is where the proposed action will take place. In this case, Port Ludlow
Marina is located in Port Ludlow Bay, Jefferson County, Washington (Township 28 North,
Range 01 East, Section 16) (Figures 1 and 2). Port Ludlow Bay, located on the west shore of
Admiralty Inlet at the mouth of Hood Canal, is a 2.2-mP, J-shaped tidal basin. The bay extends
from the mouth of Ludlow Creek 3.5 mi to Admiralty Inlet.
The eastern approach to the bay is characterized by a submerged sill having an average depth
of 24 ft mean sea level (MSL). This sill forms a submerged basin open to the north. The
average depth at the mouth of the bay is 82 ft. From this point, the bottom of the basin slopes
upward for a distance of 0.5 mi to a depth of 50 to 60 ft. From here, the depth of the bay remains
fairly uniform between 50 and 60 ft throughout most of its length to within 0.5 mi of Ludlow
Creek. The innermost 0.5 mi of the bay has an average depth of 16 ft MSL (Jefferson County
1993).
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2.2 ACTION AREA
The "action area" includes all areas at and around the project that would be affected directly
or indirectly by the proposed action. In this case, the action area is defined as the entire Port
Ludlow Marina, which is open to Port Ludlow Bay.
2.3 PROJECT DESCRIPTION
Port Ludlow Marina has 300 slips in its current configuration and can accommodate vessels
up to 170 ft in length. Under the proposed marina expansion, 100 slips will be added, with slips
varying in length from 35 to 60 ft. Approximately 40 to 60 concrete or steel piles will be
installed using a barge-mounted pile driver. It is anticipated that the work will begin in the fall
of 2001 and will require about 4 to 6 months to complete.
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Map prepared from
USGS 7.5 Minute Quadrangle
Port Ludlow, Washington
APPROXIMATE SCALE IN FEET
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O' 1000' 2000' 4000'
Pentec
Port Ludlow Marina Expansion BE
Port Ludlow, Washington
for Reid Middleton" 0
Figure 1
Site vicinity map.
ENWIONIIENrAL
01/24/00 Fig_1.FH8
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Insert Figure 2 (see attached figure)
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3.0 SPECIES AND HABITAT
3.1 SPECIES INFORMATION
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The action area has been defined as the entire Port Ludlow Marina. Although no studies
have been conducted on the river of origin of juvenile salmonids in Port Ludlow, it expected that
salmonid use of Port Ludlow is extensive. The listed Hood Canal summer-run chum salmon are
known to use the area and Puget Sound chinook salmon likely use Port Ludlow (Cameron, R.,
WDPW, pers. comm., 2000). Port Ludlow is located at the mouth of Hood Canal; thus, chinook
salmon, coho salmon, and summer-run chum from a number of river basins within the Hood
Canal basin may likely use Port Ludlow. The larger rivers within the Hood Canal basin with
summer-run chums, chinook salmon, and/or coho salmon include the Skokomish, Hamma
Hamma, Duckabush, Dosewallips, and Qui1cene River system. The river basin that is closest to
Port Ludlow that contains both Puget Sound chinook salmon and Hood Canal summer-run chum
salmon is the Qui1cene River system, located roughly 38 mi south of Port Ludlow, draining to
Qui1cene Bay on the Hood Canal. The river contains runs of fall chinook, coho, and summer-run
chum salmon (Williams et al. 1975). For purposes of this assessment the Qui1cene River system
is considered to be a representative source of chinook salmon, summer-run chum salmon, and
coho salmon that' occur in the action area.
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Surveys conducted in the Big Qui1cene River indicate that there is not a distinct bull
trout/Dolly Varden (see Section 3.1.4.2) stock in the river (WDPW 1998a). Hood Canal bull
trout/Dolly Varden are currently separated into three distinct stocks, all located within the
Skokomish River basin (WDPW 1998a). Thus, any bull trout that may occur in Ludlow Bay
originate in rivers other than the Qui1cene River system.
In addition to chinook and coho salmon and bull trout, the bald eagle and marbled murrelet
may also occur in the project vicinity. The life histories and stock status of these avian species is
also discussed.
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3.1.1 Chinook Salmon
3.1.1.1
Life History
Chinook salmon prefer to spawn and rear in the main stem of rivers and larger streams
(Williams et al. 1975, Healey 1991). In the Quilcene River system, the Big Quilcene River is the
only system containing sufficient flows during the late summer-early fall spawning migration
period to accommodate a sustained run of fall chinook. Occasionally a few chinook are observed
spawning in the Little Quilcene River, although it is felt that these are strays from the run
destined for the Big Quilcene. This is an introduced stock of chinook and a large portion of adult
returns is attributed to hatchery production (Williams et al. 1975).
The adult chinook spawning migration begins in early September and continues into
mid-October. Spawning commences in mid-September and terminates early in November. The
Federal Fish Hatchery at river mile (RM) 2.8 at the mouth of Penny Creek is the upper limit of
salmon migration. The lower 2 mi of the river provide excellent spawning habitat and is used
extensively by chinook spawners. Following incubation and subsequent emergence, the majority
of chinook fry rear in the system from 90 to 120 days before entering the estuary, with the major
outmigration between April and June (Figure 3) (Williams et al. 1975).
In watersheds with an unaltered estuary, chinook smolts spend a prolonged period (several
days to several weeks) during their spring outmigration feeding in saltmarshes and distributary
channels as they transition gradually into more marine waters (Simenstad et al. 1982). Chinook
fry and subyearlings in saltmarsh and other shallow habitat predominantly prey on emergent
insects and epibenthic crustaceans such as gammarid amphipods, mysids, and cumaceans. As
chinook mature and move to neritic habitat, they feed on small nekton (decapod larvae, larval
and juvenile fish, and euphausiids) and neustonic drift insects (Simenstad et al. 1982; see also
detailed life history review by Healey 1991).
3.1.1.2 Stock Status
No stock status information was found for the Quilcene River system fall chinook stock.
Because hatchery stocks have been mixed with wild chinook populations within the Hood Canal
basin, Hood Canal chinook have been combined into a single stock for the purposes of stock
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assessment (WDFW and WWTIT 1994). As of 1992, the stock status of the Hood Canal
chinook salmon stock was rated as healthy (WDFW and WWTIT 1994).
There is no critical habitat designated for Puget Sound chinook salmon. Critical habitat is
currently proposed by NMFS, though not yet granted specific protection. Proposed critical
habitat includes all marine, estuarine, and river reaches accessible to chinook salmon in Puget
Sound.
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Figure 3 Timing of salmon freshwater life phases in the Quilcene Basin.
Freshwater
Species Life Phase J F M A S 0 N 0
Spring Chinook Upstream migration
Spawning
Intragravel develop.
Juvenile rearing
Juv. outmigration
Summer-Fall Upstream migration
Chinook Spawning
- Intragravel develop.
Juvenile rearing
Juv. outmigration
Coho Upstream migration
Spawning
Intragravel develop,
Juvenile rearing
-- Juv. outmigration
Chum Upstream migration
Spawning
Intragravel develop.
Juvenile rearing
Juv. outmigration
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3.1.2 Coho Salmon
3.1.2.1
Life History
All accessible streams and tributaries draining the upper Hood Canal-Straits basin are utilized
by coho salmon. Spawning occurs in almost every stream area where suitable spawning habitat
and conditions permit, including the mainstem of the Big Qui1cene River up to the diversion dam
barrier at RM 9.4, and in the mainstem Little Qui1cene River up to the City of Port Townsend
diversion dam at RM 7.1 (Williams et al. 1975).
Mature coho begin entering the basin streams in early October, with the peak of migration
occurring in early November; spawning extends over the period from later October until the end
of December. The fry emerge from the gravel starting in early March and generally remain in
the system for more than a year. The normal outmigration occurs in the second year of
freshwater existence from late February to mid-April (Figure 3) (Williams et al. 1975).
Because of their larger size when entering saltwater, coho are generally considered less
dependent on estuarine rearing than chinook or chum salmon (Simenstad et al. 1982). Coho tend
to move through estuaries more rapidly, using deeper waters along shorelines. Feeding is
primarily on planktonic or small nektonic organisms, including decapod larvae, larval and
juvenile fish, and euphausiids (Miller et al. 1976, Simenstad et aI. 1982). Coho also eat drift
insects and epibenthic gammarid amphipods,especially in turbid estuaries (see detailed life
history review by Sandercock 1991).
3.1.2.2 Stock Status
The status of the Hood Canal-Qui1cene/Dabob Bays coho stock was considered depressed as
of 1992 (WDFW and WWTIT 1994).
No critical habitat has been proposed for Puget Sound/Strait of Georgia coho salmon.
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3.1.3 Chum Salmon
3.1.3.1
Life History
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Chum salmon spend more of their life history in marine waters than other Pacific salmonids.
Chum salmon, like pink salmon, usually spawn in coastal areas, and juveniles outmigrate to
seawater almost immediately after emerging from the gravel (Johnson et al. 1997). This
ocean-type migratory behavior contrasts with the stream-type behavior of some other species in
the genus Oncorhynchus (e.g., coho salmon and most types of chinook and sockeye salmon),
which usually migrate to sea at a larger size, after months or years of freshwater rearing. It is
believed that survival and growth in juvenile chum salmon depend less on freshwater conditions
than on favorable estuarine conditions (Johnson et al. 1997).
Chum salmon may enter natal river systems from June to March, depending on
characteristics of the population or geographic location (Johnson et al. 1997). Of primary focus
is the Hood Canal summer chum salmon, with spawning runs occurring between early
September and mid-October (Johnson et al. 1997). In the Quilcene River basin in upper Hood
Canal there are two distinct runs of spawning chum salmon. The early run (summer) enters the
system in later September and spawns from October 1 to 20, while the late-run (fall) spawners
move upstream into the system the first week of November and spawn from mid-November to
mid-December (Figure 3) (Williams et al. 1975).
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Chum salmon juveniles, like other anadromous salmonids, use estuaries to feed before
beginning long-distance ocean migrations. However, chum and ocean-type chinook salmon
usually have longer residence times in estuaries than do other anadromous salmonids. The
period of estuarine residence appears to the most critical phase in the life history of chum salmon
and appears to playa major role in determining the size of the subsequent adult run back to fresh
water (Johnson et al. 1997).
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Simenstad et al. (1982) summarized the diets of juvenile salmonids in 16 estuaries and
concluded that small (S 50- to 60-mm fork length [FL]) juvenile chum salmon fed primarily on
such epibenthic crustaceans as harpacticoids copepods, gammarid amphipods, and isopods,
whereas large juveniles (> 60-mm FL) in neritic habitats fed on drift insects and on such
plankton as calanoid copepods, larvaceans, and hperiid amphipods. However, the early diet of
juvenile chum salmon at localities also consists exclusively of neritic zooplankton.
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3.1.3.2 Stock Status
No stock status information was found for summer-run chum salmon specific to the Quilcene
River system, but instead the stock status for the entire Hood Canal summer-run chum salmon
stock was assessed. Hood Canal summer chum spawn primarily in the Big Quilcene,
Dosewallips, Duckabush, and Hamma Hamma Rivers. As of 1992, this stock was classified as
critical (WDFW and WWTIT 1994).
No critical habitat has yet been designated for Hood Canal summer-run chum salmon.
3.1.4 Bull Trout
3.1.4.1 Life History
Newly hatched anadromous bull trout emerge from the gravel in the spring (WDFW 1998b).
They typically spend 2 years in fresh water before they migrate to saltwater, the mainstem of
rivers, or reservoirs, although there are populations of bull trout that do not exhibit this behavior;
these trout spend their entire lives in the same stretch of headwater stream. These fish may not
mature until they are 7 to 8 years old, and rarely reach sizes greater than 14 inches in length.
(WDFW 1998b).
Bull trout typically use pristine headwater areas to spawn (WDFW 1998b). Spawning begins
in late August, peaks in September and October, and ends in November. Fish in a given stream
spawn over a period of 2 weeks or less. Almost immediately after spawning, adults begin to
work their way back to the mainstem rivers, lakes, or reservoirs to overwinter. Some of these
fish stay in these areas while others move into saltwater in the spring. Bull trout will spawn a
second or even third time. Kelts feed aggressively to recover from the stress of spawning
(WDFW 1998b).
Bull trout are opportunistic feeders, eating aquatic insects, shrimp, snails, leeches, fish eggs,
and fish. Early beliefs that these fish are serious predators of salmon and steelhead are generally
not supported today (WDFW 1998b).
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Any bull trout that may occur in the action area likely originate from rivers other than the
Qui1cene River system, which does not have distinct stock of bull trout/Dolly Varden (WDFW
1998a).
3.1.4.2 Stock Status
The status and occurrence of anadromous populations of bull trout in Puget Sound are subject
to some scientific debate; separation of anadromous bull trout from the closely related
anadromous Dolly Varden char (S. malma) is very difficult and can only be accomplished using
electrophoretic techniques (Leary and Allendorf 1997). Until further resolution is possible, the
Washington Department of Fish and Wildlife (WDFW) has made a decision to manage all Puget
Sound stocks as if they were a single bull trout/Dolly Varden complex (Washington Department
of Wildlife [WDW; now WDFW] 1993).
The USFWS has not established or identified critical habitat for coastal bull trout in Puget
Sound.
3.1.5 Bald Eagle
3.1.5.1
Life History
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Bald eagles historically ranged throughout North America except extreme northern Alaska
and Canada and central and southern Mexico. The bald eagle's habitat includes estuaries, large
lakes, rivers, and coastal areas. In Washington, resident bald eagle populations occur primarily
near large bodies of water west of the Cascade Mountains (Rodrick and Milner 1991). Bald
eagles are known to occur in the Puget Sound area. Nest trees are typically, but not always, tall
conifers with most nest trees located within 1 mi of large bodies of water with adequate food
supplies (Anthony et al. 1982).
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The diet of bald eagles at a site in Puget Sound (Discovery Park) has been studied by
watching birds as they hunt and return with prey to an active nest site (Parametrix 1992-1995 and
1996). Marine and freshwater fish were identified as the preferred prey of these eagles during
five seasons of observation, comprising over 84 percent of all captures and deliveries. Birds
contributed a much smaller proportion (7.3 percent) of the eagles' diet. Fish species that were
identified visually when the adult eagles were observed feeding their young included salmonids,
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catfish, pollock, cod, rockfish, carp, dogfish, sculpin, perch, and hake. Eagle foraging is best
described as opportunistic, as they will take advantage of whatever prey is easiest to obtain.
Bald eagles generally begin courtship activities in November. Copulation occurs from
December to March, with egg laying and incubation during March. Eggs usually hatch in April
and brooding occurs through June. Eaglets generally fledge in June or July. Adults often depart
from the nesting area in August. They return the following fall to commence the nesting cycle.
Time fluctuations in breeding activity can be attributed to weather changes affecting foraging or
nest success (Parametrix 1992-1995 and 1996).
3.1.5.2 Stock Status
After World War II, bald eagle populations declined significantly, largely as a result of the
use of organochlorine pesticides and loss of nesting habitat (USFWS 1999). In 1963, only
417 nesting pairs of bald eagles were known to occur in the lower 48 states. In 1978, the bald
eagle was listed as an endangered species in the continental United States, except in Washington,
Oregon, Minnesota, and Wisconsin, where it was listed as threatened (USFWS 1986).
Due to recovery efforts, there are now an estimated 5,478 nesting pairs in the continental
United States (USFWS 1999). As a result, biologists believe that the bald eagle may no longer
require special protection under the ESA. In July 1999, the USFWS proposed toremove the bald
eagle from the list of threatened and endangered species. A final decision on deli sting is
expected in July 2000.
3.1.5.3 Preliminary Effects Determination
Proposed project activities will be confined to limited intertidal and subtidal 'areas and will
not significantly affect eagle foraging areas or prey. Thus, the proposed action may affect, but is
not likely to directly or indirectly adversely affect, bald eagles that may occur in the project
vicinity. Also, no interrelated or interdependent actions are expected to affect bald eagles. No
further discussion of the effects of the project on the species is warranted or inc.1uded in this
document.
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3.1.6 Marbled Murrelet
3.1.6.1 Life History
The marbled murrelet, a small seabird that nests in the coastal, old-growth forests of the
Pacific Northwest, inhabits the Pacific coast of North America from the Bering Sea to central
California. In contrast to other seabirds, murrelets do not form dense colonies, and may fly
70 Ian or more inland to nest, generally in older coniferous forests. They are more commonly
found inland during the summer breeding season, but make daily trips to the ocean to gather
food, primarily fish and invertebrates, and have been detected in forests throughout the year.
When not nesting, the birds live at sea, spending their days feeding and then moving several
kilometers offshore at night (SEI 1999).
The breeding season of the marbled murrelet generally begins in April, with most egg laying
occurring in late May and early June. Peak hatching occurs in July after a 27- to 30-day
incubation. Chicks remain in the nest and are fed by both parents. By the end of August, chicks
have fledged and dispersed from nesting areas (Marks and Bishop 1999). The marbled murrelet
differs from other seabirds in that its primary nesting habitat is old-growth coniferous forest
within 50 to 75 mi of the coast. The nest typically consists of a depression on a moss-covered
branch where a single egg is laid. Marbled murrelets appear to exhibit high fidelity to their
nesting areas, and have been observed in forest stands for up to 20 years (Marks and Bishop
1999). Marbled murrelets have not been known to nest in other habitats including alpine forests,
bog forests, scrub vegetation, or scree slopes (Marks and Bishop 1999).
Marbled murrelets are presumable long-lived species but are characterized by low fecundity
(one egg per nest) and low nesting and fledging success. Fledging success has been estimated at
45 percent. Nest predation on both eggs and chicks appears to be higher for marbled murrelets
than for other a1cids, and may be cause for concern. Principal predators are birds, primarily
corvids (jays, ravens, and crows) (Marks and Bishop 1999).
At sea, foraging murrelets are usually found as widely spaced pairs. In some instances
murrelets form or join flocks that are often associated with river plumes and currents. These
flocks may contain sizable portions of local populations (Ralph and Miller 1999).
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3.1.6.2 Stock Status
The total North American population of marbled murrelets is estimated to be 360,000
individuals. Approximately 85 percent of this population breeds along the coast of Alaska.
Estimates for Washington, Oregon, and California vary between 16,500 and 35,000 murrelets
(Ralph and Miller 1999). In British Columbia, the population was estimated at 45,000 birds in
1990 (Environment Canada 1999). In recent decades the murrelet population in Alaska and
British Columbia has apparently suffered a marked decline, by as much as 50 percent. Between
1973 and 1989, the Prince William Sound, Alaska, murrelet population declined 67 percent.
Trends in Washington, Oregon, and California are also down, but the extent of the decrease in
unknown. Current data suggest an annual decline of at least 3 to 6 percent throughout the
species' range (Ralph and Miller 1999).
The most serious limiting factor for marbled murrelets is the loss of habitat through the
removal of old-growth forests and fragmentation of forests. Forest fragmentation may be
making nests near forest edges vulnerable to predation by other birds such as jays, crows, ravens,
and great-homed owls (USFWS 1996). Entanglement in fishing nets is also a limiting factor in
coastal areas due to the fact that the areas of salmon fishing and the breeding areas of marbled
murrelets overlap. The marbled murre let is especially vulnerable to oil pollution; in both Alaska
and British Columbia, it is considered the seabird most at risk from oil pollution. In 1989, an
estimated 8,400 marbled murrelets were killed as a result of the Exxon Valdez oil spill (Marks
and Bishop 1999). Marbled murrelets forage in nearshore waters where recreational boats are
most often found. Disturbance by boats may cause them to abandon the best feeding areas
(Environment Canada 1999).
3.1.6.3 Preliminary Effects Determination
Proposed project activities will be confined to limited intertidal and subtidal areas and will
not significantly affect murrelet foraging areas or prey. Thus, the proposed action may affect,
but is not likely to directly or indirectly adversely affect, marbled murrelets that may occur in the
project vicinity. Also, no interrelated or interdependent actions are expected to affect marbled
murrelets. No further discussion of the effects of the project on the species is warranted or
included in this document.
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3.2 EXISTING ENVIRONMENTAL CONDITIONS
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The existing habitat in the action area is described in this section in the context of a series of
"pathways" and "indicators" (NMFS 1999). Pathways represent groups of environmental
attributes important to anadromous fish and their habitats. Indicators may be either metric
(numeric) or descriptive and are measures of how near-optimal the habitat is for the pathway and
species in question. Within the context of this BE, the concept of pathways and indicators is
useful to frame discussions of how the proposed project will influence (improve, maintain, or
degrade) each indicator. A list of pathways and indicators considered in this BE is provided in
Table 1. Relevant pathways and indicators are discussed in the following sections.
3.2.1 Water Quality and Stormwater
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The Washington State Department of Ecology (Ecology) has classified all waters of Port
Ludlow as Class AA. Water quality monitoring of Port Ludlow Bay since 1984 has
demonstrated that overall water quality in Port Ludlow Bay is excellent, consistent with its Class
AA designation (Jefferson County 1993). A program to monitor nonpoint sources of pollutants
to Port Ludlow Bay was initiated by Pope Resources, developers of the Port Ludlow Marina.
Monitoring has continued since 1989, with the objectives of (1) establishing baseline water
quality conditions, (2) evaluating the impacts of development activities and related nonpoint
sources, (3) evaluating the effectiveness of nonpoint source controls such as stormwater
management systems, and (4) monitoring long-term trends of bay water quality (Berryman &
Henigar 1999).
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A National Pollutant Discharge Elimination System (NPDES) point-source monitoring
program for the Port Ludlow Wastewater Treatment Plant was conducted from 1989 through
1997. This monitoring program documented water quality in Port Ludlow Bay during the
environmentally critical months of May through October. The results of the point-source
monitoring demonstrated continued excellent water quality in Port Ludlow Bay. The
point-source monitoring program is no longer required by Ecology and was discontinued in 1998
(Berryman & Henigar 1999).
A nonpoint monitoring program has been in place SInce 1989, with the most recent
monitoring occurring in 1998. The nonpoint-source monitoring program was designed to assess
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Table 1
Pathways and indicators for evaluating salmon habitat in the urban estuary.
Pathway
Construction Disturbances
Water Quality
Stormwater
Sediment
Habitat Conditions
Biota
Indicator
Noise
Entrainment
Stranding
Turbidity
Chemical contam ination/nutrients
Temperature
Dissolved oxygen
Stormwater quality/quantity
Sedimentation sources/rates
Sediment quality
Fish access/refugia
Depth
Substrate
Slope
Shoreline
Riparian conditions
Flow and hydrology/current patterns/saltwater-freshwater interface
Overwater structures
Disturbance
Prey-epibenthic and pelagic zooplankton
Infauna
Prey-forage fish
Aquatic vegetation
Nonindigenous species
Ecological diversity
long-term trends in water quality during baseflow and stormflow conditions in the major
tributaries to Port Ludlow Bay. Baseflow conditions were generally measured May through
October, while stormflow conditions were measured during storm events. During the 1998
monitoring program, stormflow water quality was measured during December. Stations were
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monitored for flow, fecal coliform, conductivity, dissolved oxygen, pH, turbidity, and
temperature. During some years, some stations were monitored for metals and pesticides.
No long-term upward or downward trends in constituent concentrations are evident for any
of the monitoring stations, with the exception of conductivity. Constituent concentrations, for
the most part, have not been increasing along with the increased population density of the
watershed. Concentrations of most constituents, for example fecal coliform, have been higher
during storm events than during baseflows, which is consistent with the findings of other
watershed studies (Berryman & Henigar 1999).
Concentrations of dissolved and total metals continue to be low during storm events and very
low during baseflows (Berryman & Henigar 1999).
Nutrient (phosphorus and nitrogen) concentrations in the freshwater tributaries are in the
typical range for rural watersheds during both baseflow and stormflow. Overall, nutrient loading
to Port Ludlow Bay from these tributaries is extremely low (Berryman & Henigar 1999).
Based on the results of the nonpoint-source monitoring program, water quality conditions in
Port Ludlow Bay do not appear to be adversely impacted by watershed activities (Berryman &
Henigar 1999).
3.2.2 Sediment Quality
As part of the nonpoint-source monitoring program, sediment samples have been collected
from the bay at locations where stormwater discharge is known to occur. Samples were analyzed
for a variety of constituents, including oil and grease, total metals, pesticides, and
polychlorinated biphenyls (PCBs). Results of sediment quality monitoring have demonstrated
sediment quality to be excellent within Port Ludlow Bay. Pesticides and PCBs were not
detected, as were mercury, selenium, and silver. Of those metals that were detected,
concentrations were well below Washington's Sediment Quality Standards (SQS) (Jefferson
County 1993).
Sediment samples collected within Port Ludlow Marina between 1987 and 1995 had
concentrations of metals that were well below their respective SQS (Table 2) (Vasey
Engineering 1995).
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Table 2
Summary of sediment metals concentrations (mg/kg) in Port Ludlow Marina sediments
collected between 1987 and 1995 compared with their respective Sediment Quality
Standards (Vasey Engineering 1995).
Metal 1995 1993 1991 1987 SQS
Arsenic 2.8 1.5 2.8 2.7 57
Cadmium 0.46 0.93 0.3 0.3 5.1
Copper 11.2 9.32 7.0 7.0 390
Lead 4.76 2.56 <10 <10 450
Mercury 0.074 0.053 <0.05 <0.05 0.41
Zinc 20.3 22.8 25.0 25.0 410
3.2.3 Habitat
3.2.3.1 Access/Refugia
Juvenile salmonids have largely unrestricted access to and through the action area. Port
Ludlow Marina has overwater structures that may provide refuge for juvenile salmonids using
nearshore areas in the vicinity. Studies by Pentec (1997), Salo et al. (1980), and Ratte and Salo
(1985) have shown evidence that migrating juvenile salmonids use overwater structures as cover
when they are disturbed by overhead activities. These studies also found no evidence that
overwater structures in Puget Sound concentrate predators on juvenile salmonids.
3.2.3.2 Substrate
Sediments under the marma are relatively fine-grained native sediments (Echelon
Engineering 2000). Sediment samples collected in 1995 near the western end of C-dock were
described as being black and anoxic and composed primarily of sand and shell fragments (Vasey
Engineering 1995). Substrate available to organisms is modified by growth of green algae
(Vlva spp.) and probably several other species on cobbles in the middle and lower intertidal
zone. No eelgrass has been reported in the action area. Eelgrass is generally present on suitable
substrates (sand/silt) at depths between mean lower low water (MLLW) and about -18 ft MLLW
in the central Puget Sound region; however, an underwater survey conducted on December 10,
1999, found no eelgrass under the existing marina or in areas that would be directly affected by
the project (Echelon Engineering 2000). Existing pilings of the dock provide an additional
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substrate type that supports a dense epibiota dominated by barnacles and mussels in the intertidal
zone. Hydroids, tubeworms, and anemones are expected to be the dominant piling organisms
below about MLLW (e.g., Kozloff 1987).
3.2.3.3 Slope
The Port Ludlow Marina was constructed in the late 1970s, and the boat basin was created by
dredging. The slope of the substrate beneath the marina was created as a result of the initial
dredging. From the vertical riprap wall that borders the shoreward side of the marina, the beach
slopes at an approximately 6 percent grade. At the seaward extent of the marina, the slope
decreases, with depths at the outer margin of the marina between 35 ft and 40 ft. From this
point, there is a gradual slope to the middle of Port Ludlow Bay where bottoms depths vary
between 50 and 60 ft. Most of the marina expansion will occur along the outer margin of the
marina in water depths of 35 to 40 ft.
3.2.3.4 Flow/Current Patterns
The location, geometry, and orientation of Port Ludlow Bay is such that the strong offshore
ebb and flood tidal currents in Admiralty Inlet create a large eddy in the outer portion of Port
Ludlow Bay that appears to reverse direction with each tidal stage. Waters from Admiralty Inlet
are drawn into the bay under a wide variety of tidal conditions. Current measurements, drogue
observations, and salt balance calculations made in 1984 and 1986 indicated that the outer bay
eddy is accompanied by a complex pattern of currents that exert influence into the central portion
of the bay. Significantly more water is circulated into and out of the bay due to eddies and
currents than would be the case if only a simple flood/ebb pattern existed. As a consequence, the
bay may be better mixed and better flushed than many bays within Puget Sound. Mixing is
further enhance by vertical currents and upwelling at the entrance and head of Port Ludlow Bay
(Jefferson County 1993).
Flushing of the bay is caused by tidal currents, fresh water from streams and rainfall, wind
mixing of the surface water, and local vertical mixing. Salt balance calculations indicated that
the volume of water exchanged daily between Port Ludlow and Admiralty Inlet average
39 percent per day and vary from 20 percent to 50 percent of the total volume of the bay,
dependent upon the time of year and prevailing tidal range. The time to exchange the water
volume of the bay, including the innermost reaches, was estimated to be between 2 to 5 days.
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Localized portions of the bay may have longer or shorter flushing rates. The flushing time for
the outer bay has been estimated to be 9 hours on average (Jefferson County 1993).
3.2.4 Biota
3.2.4.1
Prey-Epibenthic Zooplankton
Epibenthic zooplankton, primarily crustaceans, along with terrestrial insects are important
prey for juvenile chinook salmon in estuaries (Simenstad et al. 1988, Healey 1991). Several of
the habitat indicators listed above are important in determining the productivity and composition
of the epibenthic community. No studies have been conducted within the action area that have
examined benthic and epibenthic biota.
3.2.4.2 Prey-Pelagic Zooplankton
Calanoid copepods are often abundant in the diet of juvenile chinook salmon in urban
estuaries (Weitkamp and Schadt 1982). Production of calanoids and other potential pelagic prey
of salmonids is largely dependent on water-column processes in Central Puget Sound. Pelagic
zooplankton productivity is dependent on the presence of adequate light and nutrients to
stimulate phytoplankton and is not influenced greatly by conditions along shorelines or in deeper
water in the vicinity of the Port Ludlow Marina.
3.2.4.3 Prey-Forage Fish
Larval, juvenile, and adult herring (Clupea harengus), surf smelt (Hypomesus pretiosus), and
Pacific sand lance (Ammodytes hexapterus) are important forage fish for juvenile, subadult, and
adult salmonids (Healey 1991). Alteration of spawning habitat for these species may directly
affect the abundance of forage for a range of age groups of chinook salmon. Surf smelt and sand
lance spawn within Port Ludlow; however, there are no data that spawniI1g occurs within the
project area (Bargmann, G., WDFW, pers. comm., 2000).
3.2.4.4 Vegetation
Eelgrass beds are recognized as habitats of statewide significance due to their high
production rates of prey for salmonids and other fishes, for the structural diversity they provide,
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and as a site for herring spawning (e.g., Simenstad et al. 1988). Macroalgae also are recognized
as a contributor to habitat complexity and primary productivity. In contrast to eelgrass,
macroalgae readily colonizes all appropriate rocky, cobble, or artificial substrates. Particular
macroalgal beds (e.g., kelp forests) have more specific habitat needs.
Aquatic vegetation occurs in the action area primarily attached to intertidal cobbles, docks,
and pilings. No eelgrass or macrophyte beds occur within the action area (Echelon Engineering
2000).
3.2.4.5 Ecological Diversity
Ecological diversity is an abstract concept relating to the variety of habitats and assemblages
present in a given area. A greater ecological diversity is often considered to reflect a more
stable, productive, and/or healthy ecosystem, although the tie to habitat quality for salmon is
theoretical, not empirical. No studies have been conducted within the action area investigating
ecological diversity.
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4.0 EFFECTS OF THE ACTION
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4.1 EFFECTS ANALYSIS
This section discusses short-term and long-term, direct and indirect effects of the Port
Ludlow Marina expansion project activities, as well as the net effects of those activities on
salmonids listed and proposed for listing under ESA. Only those pathways and their associated
indicators that are likely to be affected by the project in some way are discussed in this section.
A primary factor reducing the risk of impact to juvenile salmonids is the restriction of inwater
activities to periods when few juveniles will be present in the work area. No reports have been
found that suggest that adult salmonids would be vulnerable to impact or take from the types of
activities included in the proposed action.
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Net effect is considered to be the overall effect on the species and habitat in the long term.
The net effects of the proposed project on each indicator are summarized in Table 3.
4.1.1 Construction Disturbances
4.1 .1 .1
Short-Term Effects
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Direct Effects-Approximately 40 to 60 concrete or steel pilings will be installed as part of
the marina expansion project. Piles will be installed using a barge-mounted pile driver. Feist et
al. (1996) investigated the impacts of pile driving on juvenile pink and chum salmon behavior
and distribution in Everett Harbor, Washington. The authors reported that there may be changes
in general behavior and school size, and that fish appeared to be driven toward the acoustically
isolated side of the site during pile driving. However, the prevalence of fish schools did not
change significantly with and without pile driving, and schools were often observed about the
pile-driving rigs themselves. No impacts on feeding were reported. The study concluded that
any effects of pile-driving noise on juvenile salmonid fitness would be very difficult to measure
quantitatively. Because the proposed inwater construction would occur outside of time periods
when significant numbers of juvenile salmonids are expected to be present, no significant effect
or take is expected from project construction activities.
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Table 3
Net effects of the action on relevant pathways and indicators.
Indicators
Noise
Entrainment
Stranding
Water Quality Turbidity
Chemical contamination/nutrients
Temperature
Dissolved oxygen
Stormwater quality/quantity
Sedimentation sources/rates
Sediment quality
Fish access/refugia
Depth
Substrate
Slope
Shoreline
Riparian Conditions
Flow and hydrology/current patterns/
saltwater-freshwater mixing patterns
Overwater structures X
Disturbance X
Prey-epibenthic and pelagic zooplankton X
Infauna X
Prey-forage fish X
Aquatic vegetation X
Nonindigenous species X
Ecological diversity X
1 Action will contribute to long-term improvement, over existing conditions, of the indicator.
2 Action will maintain existing conditions.
3 Action will contribute to long-term degradation, over existing conditions, of the indicator.
Pathway
Construction
Disturbances
Stormwater
Sediment
Habitat
Conditions
Biota
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Effects of Action
Improve1 Maintain2 Degrade3
X
X
X
X
X
X
X
X
X
X
X
X
X
X
X
X
X
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Indirect Effects-No short-term indirect effects due to construction disturbances are
anticipated.
4.1.1.2 Long-Term Effects
No long-term direct or indirect effects due to construction disturbances are anticipated.
4.1.1.3 Net Effects
Pile driving will result in a brief period of increased noise during the Port Ludlow Marina
expansion project, possibly causing salmonids and other species to avoid certain areas in the
vicinity of the marina during active pile driving. This possible impact is only temporary and will
not persist beyond the construction period and will not result in significant or measurable take of
juvenile salmonids. Therefore, the net effect of pile driving and removal is to maintain noise
levels in the project area (Table 3).
4.1.2 Water Quality
4.1.2.1 Short-Term Effects
Direct Effects-Pile driving may produce temporary and localized impacts to water quality.
Elevated turbidity plumes are likely to occur in the immediate vicinity of the pile driving.
However, the majority of the pile-driving activities will occur at water depths of 35 to 40 ft,
away from intertidal areas that are used predominantly by juvenile salmonids. Because of the
depth of the water where pilings will be installed, it is unlikely that any increased turbidity due to
pile driving will affect area frequented by juvenile salmonids. Pile-driving activities are not
expected to appreciably affect dissolved oxygen concentrations in the project area.
Juvenile salmon have been shown to avoid areas of unacceptably high turbidities
(e.g., Servizi 1988), although they may seek out areas of moderate turbidity (10 to 80 NTU),
presumably as cover against predation (Cyrus and Blaber 1987a,b). Feeding efficiency of
juveniles is also impaired by turbidities in excess of 70 NTU, well below sublethal stress levels
(Bisson and Bilby 1982). Reduced preference by adult salmon homing to spawning areas has
been demonstrated where turbidities exceed 30 NTU (20 mg/l suspended sediments). However,
chinook salmon exposed to 650 mgll of suspended volcanic ash were still able to find their natal
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water (Whitman et al. 1982). Based on these data, it is unlikely that the locally elevated
turbidities generated by the proposed action would directly affect juvenile or adult salmonids that
may be present.
Sediment chemistry data from the marina indicate that sediments beneath the marina do not
contain elevated concentrations of any organic chemicals or metals. Pile driving, therefore, will
not compromise water quality by the resuspension of contaminants in the water column.
Indirect Effects-Few, if any, juvenile salmonids are expected in the action area during
construction activities; also, few adult chinook salmon or bull trout are expected in the project
area during construction. Short-term and localized decreases in dissolved oxygen or increases in
turbidity due to project construction may result in avoidance of immediate work areas. Should
this avoidance occur, it would have only insignificant and unmeasurable effects on salmonids.
4.1.2.2 Long-Term Effects
No long-term direct or indirect effects to water quality are anticipated for any of the
construction activities proposed in the project area.
4.1.2.3 Net Effects
Short-term effects resulting from increased turbidity may be expected during pile driving, but
these effects due to sediment resuspension are expected to be only temporary, with no long-term
effects. Therefore, the net effect of pile driving and installation is to maintain water quality in
, the project area (Table 3).
4.1.3 Sediment Quality
4.1.3.1
Short-Term Effects
No short-term direct or indirect effects to sediment quality from pile-driving activities are
anticipated in the project area.
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4.1.3.2 Long-Term Effects
No long-term direct or indirect effects to sediment quality from pile-driving activities are
anticipated in the project area.
4.1.4 Habitat Conditions
4.1.4.1
Short-Term Effects
No short-term direct or indirect effects to habitat conditions from pile driving or other marina
expansion activities are anticipated in the project area.
4.1.4.2 Long-Term Effects
No long-term direct or indirect effects to habitat conditions from pile driving or other marina
expansion activities are anticipated in the project area. The square footage of overwater
coverage in the Port Ludlow Marina will be increased as part of the expansion project.
Approximately 100 slips will be added to the existing marina facilities. Studies by Pentec
(1997), Salo et al. (1980), and Ratte and Salo (1985) have shown evidence that migrating
juvenile salmonids use overwater structures as cover when they are disturbed by overhead
activities. These studies also found no evidence that overwater structures in Puget Sound
concentrate predators on juvenile salmonids.
4.1.4.3 Net Effects
The Port Ludlow Marina expanSIOn will not impact fish access, fish refugia, substrate,
shoreline, riparian conditions, flow and hydrology, current patterns, or saltwater-freshwater
mixing patterns, nor will it result in other habitat disturbances (Table 3).
4.1.5 Biota
4.1.5.1
Short-Term Effects
'--
No short-term effects to biota from the Port Ludlow Marina expansion are expected in the
project area.
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4.1.5.2 Long-Term Effects
Direct Effects-The installation of 40 to 60 concrete or steel pilings in the project area at
water depths of 35 to 40 ft will result in the destruction of benthic habitat within the footprint of
each piling. Assuming that each piling is approximately 60 cm in diameter, the area covered by
the foot of each piling is about 0.283 m2, or about 11.3 to 17 m2 for 40 to 60 pilings. Benthic
habitat within the footprint of each piling will be permanently destroyed. However, the pilings
will provide additional surface area for colonization by marine plants and animals. Colonization
by marine algae will, in turn, provide additional habitat for juvenile fish and invertebrates.
Expansion of the Port Ludlow Marina will result in an increase in the area of overwater
structure within the project area, which will in turn result in increased shading of predominantly
subtidal habitats beneath the structures, although a limited area of intertidal habitat may also be
shaded. Under existing conditions, the action area does not provide substantial habitat for
aquatic vegetation. Increased shading of underlying substrates may result in minor decreases in
microalgae and benthic productivity in the area directly beneath the new floats; however, the
floats will also provide additional surface area for colonization by aquatic vegetation and
invertebrates.
Indirect Effects-No adverse long-term, indirect effects on biota are expected to result from
the proposed action.
4.1.5.3 Net Effects
The expansion of the Port Ludlow Marina will result in biota in the project area being
maintained in their current condition (Table 3).
4.1.6 Net Effects of Action
The net effect of the proposed Port Ludlow Marina expansion will be to maintain all of the
indicators for each of the six pathways in their current conditions. Short-term, localized, and
minimal water quality degradation during pile driving will not impact habitat for juvenile
salmonids because of seasonal work restrictions; thus, current water quality conditions will be
maintained in the long term.
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4.1.7 Cumulative, Interdependent, and Interrelated Effects
4.1 .7.1
Interdependent and Interrelated Effects
Expansion of the Port Ludlow Marina to 100 additional slips will likely result in an increase
in the number of vessels moored in the marina, as well as increased human activity and vessel
traffic within the marina. Increasing the number of vessels moored in the marina will also
increase the area of substrate beneath the vessels that is shaded; however, increased shading is
not expected to adversely affect habitat or biota in the project area. Because substantial boating
activity already occurs within Port Ludlow and the marina, the expected increase in boat traffic is
not anticipated to result in any adverse impacts to listed species in the project area or in Port
Ludlow Bay.
The increase m boating traffic within the marma will increase the potential for water
pollution from boating-related activities (e.g., oil, transmission fluid, gasoline, and diesel spills).
Ecology and the US Coast Guard (USCG) regulate activities (including those that could
negatively impact water quality) of commercial and recreational vessels operating in coastal
waterways. These regulations include prohibiting bilge and sewage discharge, and requiring that
any hazardous material spilled (i.e., diesel, gasoline, oil, and transmission fluid) be reported to
marina authorities, Ecology, and the USCG. In the event a hazardous material is spilled into the
marina, the marina has a hazardous-spill response plan and the appropriate equipment to contain
and cleanup any spills (Port Ludlow Marina 1999).
4.2 TAKE ANALYSIS
Section 3 of the ESA defines take as "to harass, harm, pursue, hunt, shoot, wound, trap,
capture, collect or attempt to engage in any such conduct." The USFWS further defines "harm"
as "significant habitat modification or degradation that results in death or injury to listed species
by significantly impairing behavior patterns such as breeding, feeding, or sheltering," and
"harass" as "actions that create the likelihood of injury to listed species to such an extent as to
significantly disrupt normal behavior patterns which include, but are not limited to breeding,
feeding or sheltering" (NMFS 1999).
There is no critical habitat designated for the Evolutionarily Significant Unit (ESU) of Puget
Sound chinook salmon or the Hood Canal summer-run chum salmon ESU, nor has the USFWS
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established or identified critical habitat for bull trout; therefore, no critical habitat for either
chinook salmon or bull trout has been identified in the project area. The proposed Port Ludlow
Marina expansion project is unlikely to significantly modify or degrade habitat in the action area
and is unlikely to impair or disrupt normal behavior patterns involving breeding, feeding, or
sheltering. Therefore, the proposed Port Ludlow Marina expansion project is not expected to
result in the taking of chinook salmon, Hood Canal summer-run chum salmon, coho salmon, or
bull trout.
4.3 CONSERVATION MEASURES
No significant or measurable effects are predicted from the proposed action. However, a
number of conservation measures have been incorporated in the marina expansion project.
Concrete or steel pilings will be used instead of treated wood pilings to prevent the introduction
of any chemical contaminants that could leach from treated wood pilings. Furthermore,
construction activities will occur when juvenile salmonids are not likely to be present in the
project area.
The existing water and sediment quality monitoring plan, which monitors water and sediment
quality in the marina and throughout Port Ludlow Bay, will continue after the marina expansion
project. Water and sediment quality data collected since 1989 indicate that water and sediment
quality throughout Port Ludlow meet or exceed state standards. Continued monitoring will
provide a means to assess future trends in environmental quality within Port Ludlow Bay.
4.4 DETERMINATION OF EFFECTS
NMFS/USFWS guidelines for the preparation of BEs states that a conclusion of "may affect,
but is not likely to adversely affect" is the".. . appropriate conclusion when the effects on the
species or critical habitat are expected to be beneficial, discountable, or insignificant. Beneficial
effects have contemporaneous positive effects without any adverse effects...." Insignificant
effects, in the NMFS/USFWS definition, ".. . relate to the size of the impacts and should never
reach the size where take occurs... [One would not expect to]...be able to meaningfully measure,
detect, or evaluate insignificant effects." Based on the analyses in this BE, this is the expected
nature and level of impact of implementation of the proposed project.
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4.4.1 Salmonids
-
The Port Ludlow Marina expansion project may affect, but is not likely to adversely affect,
juvenile chinook, Hood Canal summer~run chum salmon, coho salmon, or bull trout, or their
critical habitats. While the conclusion is focused on chinook salmon and chum salmon, it is
applicable to coho salmon and bull trout as well; however, because of their presumed lesser
dependence on nearshore habitat, these species will be less affected by both the negative and
positive aspects of each project component. No measurable effects and no take of salmonids are
expected.
4.4.2 Birds
The proposed action may affect, but is not likely to adversely affect, bald eagles or
marbled murrelets, or their critical habitat.
.....
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.......
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--
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