DRAFT, last updated 3/15/05
Salt Creek Watershed Page – WRIA
19, Tier 2
A. Watershed Information:
-
General
Watershed Description: From
2004
Salt Creek Assessment, p. 12: Salt Creek is an independent tributary
to the Strait of Juan de Fuca (SJF) located 15 miles west of Port Angeles
(Figure 1). The watershed is 19.1 mi2 in size and includes 23.4 miles
of streams accessible to anadromous salmonid (Phinney and Bucknell 1975).
The watershed has little relative relief and drains a series of low hills
(maximum elevation 3000’/917 m) paralleling the SJF. Base rocks
in Salt Creek include primarily those of sedimentary origin including
the Twin River Formation (Tabor and Cady 1978), which is dominated by
sandstones, siltstones and conglomerates. An area of basalt origin is
located at the northeast portion of the drainage at Striped Peak. Salt
Creek has been strongly influenced by the most recent continental glaciation
(Vashon Stade~25,000 years ago). During the peak of this glacial advance,
much of Salt Creek was buried by as much as 3000’ of ice. Salt
Creek is dominated by glacial outwash features and associated soil types.
Drainage patterns have also been affected by glacial features as well:
a series of glacial striations are clearly visible on aerial photographs
across the west side of the watershed. Several small tributaries and
wetland complex drain these features.
Salt Creek receives between 35-55” (89-1,397 mm) of precipitation
annually depending upon elevation, predominately as rainfall (SCS 1965).
The majority of precipitation occurs between October and March, and the
annual hydrograph is dominated by peak flows in winter associated with
storms of maritime Pacific origin. Low base flows are common during the
spring and summer months when stream flows are almost entirely supported
by groundwater contributions. Although Salt Creek has not been assessed
for flow by continuous gauging, estimates of peak flow and low flow can
be estimated. Using relationships developed by Amermann and Orsborn (1987)
we estimated peak discharge in the vicinity of 2,000 cfs and average
annual low flow at less than 2.0 cfs.
Almost the entire Salt Creek watershed is located within the western
hemlock zone (Henderson et al. 1989). Within this forest association
Douglas fir is typically the dominant tree species in younger stands,
with late successional forests shifting toward western hemlock and red
cedar (though no significant older forest stands remain in the basin).
Land ownership patterns in Salt Creek are a complex blend of state and
industrial forest land, agricultural and rural residential uses. State
forest lands are mostly located in the headwaters, while agricultural
and rural residential lands are strongly clustered in low gradient landforms
in the middle and lower watershed.
Salt Creek has a rich cultural history supporting several significant
Klallam cultural sites, including: teu’ dlt (Agate Point-translates “abounds
in mussels”), TL sEent (Crescent Bay-translates “deep”),
Klte-tun-ut (Salt Creek), Tsatso-Al sEnt (Tongue Point-translates “close
by the deep place”) (James 1993). Three camp/village sites have
been documented in the vicinity (Waterman 1920). Klte-tunut was the site
of a large permanent village. The Salt Creek watershed was settled by
Euro-Americans in the late nineteenth century and Port Crescent was a
thriving town during the initial logging of the area’s renowned
cedar and Douglas fir stands. Large scale clearing was conducted to support
agriculture. During World War II, gun emplacements were constructed at
Camp Hayden. Prior to this, access to Salt Creek was limited to unimproved
dirt roads.
- Hatchery impacts:
- Harvest impacts:
- Stakeholders: Lower Elwha Klallam
Tribe is co-manager of fisheries with WDFW; Public landowners include
WDNR and Washington
Department of Transportation (SR 112). Major
private landowners include Merrill
and Ring. There are approximately 300 private landowners in the Salt
Creek Basin.
- Tier explanation (from NOPLE Salmon Habitat Recovery Strategy): Historically,
the Salt basin was considered to have moderately high productivity
levels (i.e., relative productivity level of 4 with 5 being the highest)
with current productivity decreased due to a variety of reasons (i.e.,
from 4 to 3). Due to its limited size, limited number of historic populations
(4), and lack of ESA listed stocks, Salt Creek was determined to be
a Tier 2.
- Bibliography:
B. Salmon Habitat Recovery Priorities:
- Salmonid stocks & their status. From State
of Our Watersheds Report 2004, NWIFC SSHIAP, p. 132:
From 2004
Salt Creek Assessment:
• Winter Steelhead:
declined to critically low levels
• Chum Salmon: teetering on the verge of extirpation
• Coho Salmon: static or declining, showing no signs of recovery
- Priority salmon stocks. Recovery efforts
will be focused on the following
salmonid stocks for the stated reasons:
a) Coho because of high productive potential due to high proportion of
low-gradient stream habitat in the Salt basin
b) Chum should be reintroduced/rebuild because instream habitat restoration
can be designed to restore lateral reconnection of floodplains, making
Coho/Chum habitat recovery complimentary and simultaneous.
- Priority Limiting Watershed Process & Habitat Features. The
following habitat feature(s) and/or watershed processes are responsible
for the
poor PVCs identified above:
a) Chronic lack of large woody debris has caused fundamental changes
in the functional condition of stream types
b) Riparian forest conditions are currently inadequate to fully support
habitat forming processes with current riparian forest dominated by
young to medium aged stands of deciduous species and with a total of
9.3 miles of stream (out of 51.6 miles surveyed) adjacent to roads;
c) 8 total and 21 partial barriers limit access to 25 miles (approximately
one-half) of historically accessible stream habitat
d) Low flow conditions have resulted in closure of new water rights.
A total of 37 perfected water rights totaling 2.7 cfs have been issued
to date.
- Major actions to protect and improve:
a) Restoration in Salt Creek should be conducted sequentially over
time by the following categories:
i) Linear reconnection of historically accessible habitats
ii) Lateral reconnection of floodplain habitats
iii) Restoration of riparian/wetland functions; instream habitat
restoration
iv) Removing/reducing current ecosystem stressors
b) In addition to these active restoration efforts, protection
of existing functional habitats through acquisition/easement
or other means should
be considered as an equal priority with restoration where possible
- Priority actions and areas:
Specific actions by location that will implement the identified
priorities within the Salt basin are set forth in the 2004
Salt Creek Assessment.
Many of these actions are complimentary and could be conducted simultaneously.
- Community issues:
From Landowner Survey, 2004
Salt Creek Assessment, p. 62: "There was a remarkable amount of
consensus among the observers, who almost unanimously attributed
the decline of salmon in Salt Creek to a combination of increased
fishing mortality and habitat degradation." From p. 89: "In Salt
Creek we found
that the overwhelming majority of landowners were supportive of salmon
and salmon habitat. However their support was often overshadowed
by a fear that their property rights might be threatened."
While the technical group working to
restore Salt Creek fisheries believes reintroduction of chum is essential
for
nutrient
enhancement
and
streambed restoration, during a December 13, 2004 NOPLE CFG meeting
introducing the 2004
Salt Creek Assessment to the Salt Creek community, the local citizens
expressed they were not in favor of re-introducing chum because they
believe it would compete with their preferred fisheries of coho and
steelhead.
C. Recovery Projects:
D. Monitoring:
E. Emerging Issues:
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