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<br />6 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />DESCRIPTION OF THE EXISTING ENVIRONMENT <br /> <br />Physical Characteristics <br /> <br />The Green River in the Moon Lake study area is a slow-moving, <br />meandering stream with a shifting sand substrate. This differs from <br />river reaches above and below the study area where canyons and steep <br />gradient turn ;the river into a swift, rapid-filled stream with inter- <br />mixed cobble and sand substrates. The river is generally 200-300 <br />meters wide and relatively shallow. Although holes in eddies may reach <br />depths of 3-5 meters, most of the river is under 2 meters except during <br />spring runoff in May and June when it may rise 2 meters. Summer tem- <br />peratures usually reach about 230 C, although much warmer temperatures <br />are found in backwaters. During winter, most of the study area may be <br />frozen over. The river is generally turbid, but during long dry spells, <br />such as occurred during the summer of 1979, it becomes relatively clear <br />and has a greenish cast rather than the normal brown appearance. <br />Flows in the Green River peak in June at near 15,000 cfs, and then <br />recede to normal low flows of 3,000 cfs during fall and winter. Flows <br />vary on a daily as well as a seasonal basis due to the requlation im- <br />posed by Flaming Gorge Dam, over 160 km upstream from the study area. <br />During natural low flow periods, daily fluctuations created by power <br />generation at the dam may approach 0.5 meter in depth in the study area. <br />Instream habitat in the study area varies with flow, and therefore <br />with season. During high flows, the river is full bank to bank and <br />only a few islands dissect the main channel. Many small eddies are <br />