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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 />I <br /> <br />Big Thompson River - This river flows into the South Platte River <br /> <br /> <br />approximately 3 miles south of laSalle, Colorado. It drains an area <br /> <br /> <br />of about 830 square miles, 70 percent of which is mountainous. The <br /> <br /> <br />Little Thompson River is its principal tributary. Mean annual runoff <br /> <br /> <br />for the Big Thompson at its mouth near laSalle, Colorado, for the 1928 <br /> <br /> <br />through 1979 water year period was nearly 52,900 acre-feet <br /> <br /> <br />(Table 8). The Big Thompson River gage at laSalle is located <br /> <br /> <br />downstream of many water diversion structures in the sub-basin. <br /> <br />Consequently, the mean annual runoff at this point in the sub-basin is <br /> <br /> <br />considerably smaller than for the St. Vrain Creek at Platteville. II. <br /> <br />significant shift in mean annual flows from those recorded between the <br /> <br /> <br />1928 through 1952 water year period (36,600 acre-feet) and those <br /> <br /> <br />recorded between the 1953 through 1978 water year period (68,000 acre- <br /> <br />feet), is probably because of increased transbasin imports from the <br /> <br /> <br />Colorado-Big Thompson Project beginning about 1953. <br /> <br />Cache 18 poudre River - This is the largest of the mountain <br /> <br /> <br />tributaries. It drains an area of about 1,900 square miles, which <br /> <br />varies in elevation from over 13,000 feet at the Continental Divide to <br /> <br /> <br />4,600 feet in the plains where it joins the South Platte River near <br /> <br /> <br />Greeley, Colorado (Figure 1). Nearly all of the native surface water <br /> <br /> <br />supply of the river is derived from melting snowpack in the <br /> <br /> <br />mountains. Mean annual runoff at the gage located near Greeley was <br /> <br />73,200 acre-feet for the 1928 through 1979 water year period <br /> <br /> <br />(Table 8). The mean annual runoff of the Cache la poudre River near <br /> <br /> <br />Greeley is also smaller than would be expected for its drainage area <br /> <br /> <br />because of many water diversions and consumptive use upstream of the <br /> <br />gage. The flow of the Cache la Poudre near its mouth has increased <br /> <br /> <br />appreciably since 1952, from an average of 52,500 acre-feet per year <br /> <br /> <br />during the 1928 through 1952 water year period to 92,500 acre-feet <br /> <br /> <br />during the 1953 through 1979 water year period (Table 8). This shift <br /> <br /> <br />is due largely to increased transbasin imports of the Colorado-Big <br /> <br />Thompson Project during the latter period. <br /> <br />-31- <br />