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<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 />Snake River Basin <br /> <br />The Snake River Basin forms the easternmost section of the Blue River Basin. The <br />Snake River Basin drains in a westerly direction, from an elevation of 14,270 <br />feet at Grays Peak along the Continental Divide south of Loveland Pass, to Dillon <br />Reservoir at an elevation of 9,000 feet. The basin is approximately 7 miles wide <br />throughout and 12 miles long with a drainage area of 76 square miles at Dillon <br />Reservoir. The channel slope ranges from 5.7% in the upper basin above the Town <br />of Montezuma to 1.1% in the study reach near Keystone Ski Area (Fig. 1). The <br />study reaches within the Snake River Basin include a portion of the North Fork <br />of the Snake River and a portion of the Snake River near Keystone (Fig. 3). <br /> <br />Tenmile Creek Basin <br /> <br />The Tenmile Creek Basin drains to the north, then northeast into Lake Dillon from <br /> <br />the Fremont Pass vicinity. This basin parallels the Upper Blue River basin with <br /> <br /> <br />the Tenmile Range dividing the two. The western boundary of the basin is formed <br /> <br />by the Gore Range and Vail Pass, and the southern boundary is the Continental <br /> <br /> <br />Divide. The upper basin is characterized by an open rolling terrain. In <br /> <br />contrast, the lower basin consists of the narrow winding Tenmile Canyon. The <br /> <br />total drainage area is 94 square miles at Frisco, with 35 square miles lying in <br /> <br />the upper basin above the confluence with West Tenmile Creek. The basin width <br /> <br />is 7 miles and the total basin length is about 14 miles. The Creek slopes at <br /> <br />about 1. 4% at Fri sco, 2% in the canyon, and 2.7% in the upper bas in. The <br /> <br />elevations in the basin range from 13,000 feet above Copper Mountain to 9,000 <br /> <br />3 <br />