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<br />00 <br />~ <br />C"J <br /> <br />FISH AND vvILDLIFE SERVICE; REPORT <br /> <br />Description of Basin and Project Area <br /> <br />1. General. - Rifle Creek, a tributary of the Colorado River is <br />formed by the junction of several small mountain streams which rise <br />on the slopes of the Flat Top,Mountains in the White River National <br />Forest, at elevations of about 10,000' m.s.l., in western Colorado <br />north of the town of Rifle. From this source, the stream flows in <br />a general southerly direction for a distanc e of about Z7 miles to <br />its confluence with the Colorado River near Rifle. Elevation of <br />Rifle Creek at its mouth is about 5,300' m.s.l. <br /> <br />2. Physiography. - From the river sources on th~ White River Plateau, <br />characterized by mesas interspersed with isolated lacolithic mountains <br />covered with a sub-alpine spruce-fir forest type, the streams fall <br />rapidly through narrow V-walled canyons for about 10 miles. Fran this <br />point, the streams flow at a very rapid rate through a rugged, highly <br />erodible terrain for a distance of about 9 miles. This intermediate <br />section is sparsely ti1abered with ponderosa -pine, Douglas fir, and <br />one-seeded juniper with a heavy oat brush, skunk brush, service berry, <br />and mountain mahogany understory. Among the grasses, three awn, cheat <br />grass, needle and thread, and western wheat grasses are dominant. Stream <br />bank cover consists of willow, alder, birch, and narrowleaf cottonwood. <br />Soils in this intermediate section consist of a stony clay loam formed <br />from the weathering of shales which overlay deep sandstone formations. <br />At a point about 8 miles upstream from the mouth of Rifle Creek, the <br />Grand Hogback cut s laterally across the valley. The remaining drainage <br />area of Rifle 'Creek between the Grand Hogback and the Colorado River is <br />characterized by mesas dissected by numerous arroyos resulting from <br />flash floods and the cutting action of primary streams which flow through <br />water gaps in the Grand Hogback. Natural vegetation in tIE area between <br />the Grand Hogback and the Colorado River consists of rabbit brush, salt <br />brush, and sage brush with a preponderantly cheat grass understory. <br /> <br />3. Stream conditions. - Stream characteristics in the upper reaches of <br />the watershed are excellent for fish and wildlife. In these reaches, the <br />streams maintain a relatively large and constant flow of clear, cold <br />water. Pools are abundant, bank cover is good, and riffle areas are <br />adequate in the "park" areas. Downstream from abo ut river mile 12 on the <br />main stream and it s tributaries, flash floods and soil conditions tend <br />to make the streams turbid. This turbid condition, together with irri- <br />gation uses resulting in warmed and silted return flow, lowers stream <br />values appreciably. There is no pollution problem in the watershed. <br />