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<br />, <br /> <br />It 4220 <br /> <br />It <br /> <br />. <br /> <br />, <br /> <br />the east side of the Continental Divide in the Arkansas River <br />Basin is not as high as its adjacent west slope. The drainage <br />area above the gage on Halfmoon Creek near Malta, elevation 9830, <br />has averaged 16.7 inches annually. The average annual yield for <br />the 23.6 square miles above this station is 21,080 acre-feet. <br /> <br />The average annual discharge for the period 1928 through 1965 <br />at the Arkansas River at Granite gate with all transmountain <br />diversions taken out, was 219,400 acre-feet. Drainage area <br />above that gage is 427 square miles. <br /> <br />Floods in the Fryingpan River Basin, such as the one which <br />occurred in the spring of 1957, are often the result of heavy <br />rain on an abnormally heavy snowpack. In that particular year <br />the snowmelt was late in starting, the Fryingpan River peaked <br />much higher and later than usual, and there was an internal <br />rain on the snowpack. On June 30, 1957, the Fryingpan River <br />at Norrie peaked at 1,780 cubic feet per second (ft3/s), and <br />the North Fork of the Fryingpan River near Norrie peaked at <br />1,140 ft3/s. <br /> <br />The Fryingpan River at Norrie normally ranges from 15 ft3/s to <br />40 ft3/s during December. The recorded low there was 8.0 ft3/s <br />in December 1962, but may have been less during periods of no <br />record. <br /> <br />The native flow of Lake Fork as measured at the gage 1,000 feet <br />upstream from original Sugar Loaf Reservoir has averaged 25,400 <br />acre-feet annually. The flows have ranged from winter average <br />of about 4 ft3/s to a June average of about 180 ft3/s. The <br />Busk-Ivanhoe transmountain diversions from the Fryingpan River <br />to Lake Fork have averaged about 5,000 acre-feet annually. <br />These transmountain diversions and the native flows were to <br />some extent regulated by the original 17,416 acre-foot capacity <br />Sugar Loaf Reservoir which was owned and operated by the CF&I <br />Steel Corporation. The outflow from this reservoir is esti- <br />mated to have ranged from 1 to 500 ft3/s. The historic end-of- <br />month water surface elevations are shown in Figure II-53. As <br />a feature of the Fryingpan-Arkansas Project, Turquoise Lake was <br />created by construction of a new and larger Sugar Loaf Dam <br />(completed in 1968), providing a storage capacity of 120,490 <br />acre-feet and inundating the original CF&I Sugar Loaf Reservoir. <br />Under Bureau of Reclamation operation the outlet structures have <br />the capability of discharging as much as 1,120 ft3/s to Lake <br />Fork and 500 ft3/s to the Mt. Elbert Conduit. Under normal <br />operation, minimum bypass flows to Lake Fork of 10 ft3/s May <br /> <br />111-32 <br />