Condit Dam Removal Condit Dam Removal - Access Washington
Condit Dam Removal Condit Dam Removal - Access Washington
Condit Dam Removal Condit Dam Removal - Access Washington
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<strong>Condit</strong> <strong>Dam</strong> Hydroelectric Project<br />
Final Supplemental EIS<br />
Deschutes River at RM 0.3 and RM 43 (Sherars Falls). Approximately 60–70 percent of the<br />
steelhead detected within the mouth of the Deschutes were later detected in other watersheds,<br />
and 30–40 percent of steelhead detected near Sherars Falls were later detected in other<br />
watersheds. Up to 25 percent of the radio-tagged steelhead known to have traveled as far<br />
upstream as Sherars Falls were later found in the Snake River. Although these “drop-in”<br />
steelhead are primarily hatchery steelhead from the Snake River basin, the lower portion of<br />
the Deschutes was famous in the 1950s for sports catches of large wild B-run steelhead trout<br />
of 20 pounds or more (Migdalski 1962) that were likely “drop-in” fish from the Snake River<br />
basin. Based on this information, it is likely that “drop-in” steelhead (and other andromous<br />
salmonids) from Columbia River and Snake River ESUs upstream of the White Salmon<br />
River will utilize pools for refuge from high summer water temperatures in the Bonneville<br />
pool throughout the reaches of the White Salmon River that become accessible after the<br />
removal of <strong>Condit</strong> <strong>Dam</strong>.<br />
Although Snake River steelhead are not residents of the White Salmon River, adults are<br />
attracted to and stray into the cooler waters of the White Salmon River during the summer.<br />
The lower White Salmon River provides an excellent thermal refuge for summer steelhead<br />
migrating upstream in the Columbia River (WDFW 2000), and the Peery and Keefer research<br />
presented in Cramer et al. (2003) indicates that Snake River basin steelhead will likely utilize<br />
thermal refuge as far upstream as RM 16.2 after dam removal. Migrating juveniles also are<br />
expected to use the lower White Salmon River for thermal refuge.<br />
Upper Columbia River Steelhead<br />
The ESA listing status came under review and down-listing the ESU from endangered to<br />
threatened has been proposed. A new critical habitat designation has been proposed and<br />
finalized.<br />
Upper Columbia River steelhead are not residents of the White Salmon River; however, they<br />
may use pools in the White Salmon River as thermal refuge (as described above under Snake<br />
River basin steelhead). Migrating juveniles also are expected to use the lower White Salmon<br />
River for thermal refuge.<br />
Middle Columbia River Steelhead<br />
Although the ESA listing status came under review, the listing as threatened was retained in<br />
the proposed listing. A new critical habitat designation has been proposed and finalized.<br />
Migrating adults and juveniles from other sub-basins are expected to use the lower White<br />
Salmon River for thermal refuge.<br />
Bull Trout<br />
Critical habitat for the Columbia River bull trout DPS has been proposed and a final rule<br />
published. Adult and sub-adult bull trout using the Columbia River as a migratory corridor<br />
between spawning, foraging, and wintering habitat in other sub-basins are expected to use the<br />
lower White Salmon River for thermal refuge. The White Salmon River is currently thought<br />
to be used by bull trout from other sub-basins as foraging, wintering, and thermal refuge<br />
habitat. After dam removal, migratory fluvial bull trout may establish a new spawning<br />
population in the upper White Salmon River that utilizes habitat in the lower White Salmon<br />
River, Bonneville pool, and nearby sub-basins. Bull trout are the salmonid species most<br />
4.3-14