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Vantage to Pomona Heights Chapter 3 <br />230 kV Transmission Line Project FEIS Affected Environment <br /> PAGE 3-51 <br />Bull Trout <br />Bull trout (Salvelinus confluentus) was listed as a threatened species under the ESA in June 1998 <br />(USFWS 1998) and is a candidate for state listing by the WDFW (2015a). Critical habitat has been <br />designated for bull trout, including the Yakima River and its tributaries and the mainstem of the Columbia <br />River (USFWS 2010b). Bull trout have specific habitat requirements that influence their distribution and <br />abundance, including water temperature, cover, channel form and stability, spawning and rearing <br />substrate, and migratory corridors (WDFW 2000). Bull trout require cold water to survive, so they are <br />seldom found in waters where temperatures exceed 59 to 64 degrees Fahrenheit (˚F). Bull trout also <br />require stable stream channels, clean spawning and rearing gravel, complex and diverse cover, and <br />unblocked migratory corridors (USFWS 2011a). <br />Historically, bull trout were found throughout the Pacific Northwest, Montana, Idaho, and northern <br />California, as well as Nevada (Knowles and Gumtow 2005). Bull trout are known to occur within the <br />reaches of the Yakima and Columbia Rivers that are located within the Project study area. Aside from the <br />Yakima and Columbia Rivers, bull trout are not known to occur in streams within the Project study area <br />(AECOM Environmental 2010; JBLM YTC 2002). The results of a stream temperature monitoring study <br />indicate that, within the Project study area, Johnson, Lmuma, and Selah Creeks were potentially suitable <br />for bull trout use, but temperatures were generally much higher than preferred spawning temperatures. <br />Bull trout are not known to spawn within JBLM YTC because the streams are too small and not cold <br />enough over a long enough time period to provide suitable spawning and rearing habitat; however, bull <br />trout could use streams for short periods for foraging (AECOM Environmental 2010). In addition, most <br />streams in the Project study area do not have continuous flow to either the Yakima or Columbia Rivers <br />during the time in which bull trout would potentially be spawning or migrating to spawn. Bull trout in the <br />Columbia River DPS enter tributary streams from April to September and spawn from September to mid- <br />October (WDFW 2000; Whitesel et al. 2004). At the time bull trout enter tributary streams north of the <br />Project study area, temperatures in the Columbia River varied from 42 to 67˚F and tributary mean daily <br />temperatures ranged from 46 to 63˚F indicating that water temperatures did not appear to limit bull trout <br />migration (BioAnalysts 2004). <br />Chinook Salmon (Upper Columbia River Spring Run) <br />The Upper Columbia River Spring Run Chinook salmon (Oncorhynchus tshawytscha) Evolutionarily <br />Significant Unit (ESU) was listed as endangered under the ESA in August 1999 (USFWS 1999) and is <br />listed as a candidate species by the WDFW. The ESU includes all naturally-spawned populations <br />occurring in all accessible river reaches in the Columbia River tributaries upstream of Rock Island Dam <br />and downstream from Chief Joseph Dam in Washington. <br />Critical habitat has been designated for the Upper Columbia River Spring Run Chinook salmon ESU and <br />includes the entire Columbia River Corridor downstream from Rock Island Dam, including the reach of <br />the Columbia River within the Project study area. This corridor, which connects the ESU with the Pacific <br />Ocean is used by rearing and migrating juveniles and migrating adults and was deemed by the National <br />Marine Fisheries Service to be of high conservation value to the Upper Columbia River Spring Run <br />Chinook ESU (National Oceanic and Atmospheric Administration [NOAA] 2005). In the Project study <br />area, upriver migration starts in early May and extends through August, with spawning occurring upriver <br />of the Project study area from late August to mid-September. Downstream migration of juveniles occurs <br />primarily in May and June (NOAA 2013). While the migration corridor is adjacent to the JBLM YTC <br />installation, the JBLM YTC is excluded from the critical habitat designation for this ESU pursuant to the <br />National Defense Authorization Act for Fiscal Year 2004 (Public Law 108-136; Army 2010). Tributaries <br />of the Columbia River in and near the Project study area, including the Yakima River, are not part of the <br />Upper Columbia River Spring Run Chinook salmon ESU; they are part of the Mid-Columbia River <br />Spring Run Chinook salmon ESU which is not listed under the ESA (NOAA 2013).