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Watershed Management Plan - Mason County

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Appendix<br />

A Sub-basin Summaries<br />

HABITAT<br />

The Skokomish sub-basin provides habitat for many anadromous fish<br />

species including chum, chinook, coho, steelhead, and cutthroat and trout.<br />

Bull trout, resident cutthroat trout, and rainbow trout are also present.<br />

Historically, sockeye stocks were also present. Individual sockeye are<br />

observed every year in the lower Skokomish basin, but biologists don’t<br />

believe a viable population is currently present. A landlocked (Kokanee)<br />

sockeye population exists in Lake Cushman and Lake Kokanee and is<br />

supported by hatchery augmentation. Landlocked chinook salmon are also<br />

present in Lake Cushman. Following is a discussion of fish habitat in the<br />

North, South, and Main forks of the Skokomish River.<br />

• The North Fork of the Skokomish River provides habitat for<br />

resident and anadromous fish. Assessment of habitat quality is<br />

limited due to litigation surrounding the Cushman Dam. Several<br />

culverts block resident fish migration on Dow Creek, Big Creek, and<br />

near the Tacoma Utility Power House. An earthen dam on the<br />

Enetai Creek also blocks fish passage (WCC, 2003). In addition,<br />

McTaggert Creek has two partial fish barriers and an impassable<br />

structure that diverts the entire flow into the hydropower facility<br />

(Skokomish Tribe, personal communication, December 23, 2004).<br />

• Habitat quality in the upper and middle reaches of the South Fork<br />

of the Skokomish River is good. The U.S. Forest Service is restoring<br />

riparian corridors near Lebar Creek and Cedar Creek, as well as other<br />

riparian zones under their ownership. Erosion at the abandoned<br />

hydropower development, near Lebar Creek and Brown Creek, is a<br />

potential problem (WCC, 2003).<br />

Habitat quality in the lower reaches of the South Fork is<br />

compromised by sediment aggradation, channelization, and loss of<br />

riparian vegetation. The source of built-up sediment is likely the<br />

result of mass wasting and road failures related to forestry practices<br />

upstream, including in Vance Creek. The lower reaches of the South<br />

Fork flowing through the Skokomish Valley have been channelized,<br />

armored, and diked and riparian vegetation throughout the valley is<br />

sparse due to agricultural land-use. Woody debris is often removed<br />

for private use including firewood and fence posts (WCC, 2003).<br />

• Barriers, channelization, sediment build-up (aggradation), and<br />

riparian loss reduce habitat quality along the Main Stem of the<br />

Skokomish River. A majority of the main stem has been diked and<br />

channelized which has eliminated access to side channel and wetland<br />

habitat and reduced channel complexity. Over half (62%) of the<br />

mainstem is sparsely vegetated and has been cleared for agriculture<br />

(WCC, 2003). One factor that may contribute to an elevated degree<br />

of sediment aggradation in the main stem is the diversion of stream<br />

flow from the North Fork to Cushman Dam. With less water<br />

flowing in the Skokomish River, the river may not be able to carry as<br />

page 84 Final <strong>Plan</strong> for <strong>County</strong> Adoption – May 11, 2006

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