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<br />:{:~7f: <br /> <br />001144 <br /> <br />7 <br /> <br />~' <br /> <br />Table 4-1 <br />Growth in Future Basin Depletions <br />Values in AFlyr <br /> <br />Environmental <br />Baseline* <br /> <br />Task 2 <br />year 2015 <br /> <br />Task 2 <br />year 2040 <br /> <br />Total <br /> <br />1,526 <br />760 <br />14.245 <br />o <br />16,531 <br /> <br />3,798 <br />500 <br />2,420 <br />o <br />6,718 <br /> <br />13,728 <br />500 <br />24.076 <br />o <br />38,304 <br /> <br />Municipal <br />Agricultural <br />Thermal-electric <br />Evaporation <br /> <br />>Ie evaporat,ion and irrigation depletions associated with now-existing rescr. <br />voirs has been subtracted <br /> <br />~ <br /> <br />Based on this comparison. it is evident that the future growth in basi~ depletions assumed in <br />the Envlronmental Baseline falls about mid-way between the near-term and long-term depletions <br />projected in Task 2, <br /> <br />HYDROLOGY OF THE YAMPA RIVER BASIN <br /> <br />General Hydrologic Setting <br /> <br />The headwaters of the Yampa River originate on the eastern edge of the White River Plateau in <br />north central Colorado. The river is fed by numerous small tributaries that drain adjoining areas of the <br />plateau and the western slopes of the Sierra Madre,' Park and Gore Ranges. In its upper reaches, the <br />Yampa River is characterized as a high gradient mountain stream flowing through tortuous and narrow <br />canyons. After emerging from the foothills near Steamboat Springs, the Yampa River traverses through <br />open country and flows west past the towns of !-Iayden and Craig, <br /> <br />Downstream of Craig, the river then flows through the narrow canyons formed by two isolated <br />mountains, Juniper and Cross Mountains, which rise abruptly from the Axial basin. Confluence with the <br />Little Snake RIver, the largest tributary to the Yampa River, is just upstream of Dinosaur National <br />Monument and the Uinta Mountains. Within Dinosaur National Monun:tent, the Yampa River once again <br />flows at a high gradient through the deeply incised Bear Canyon. Flow is in a southwesterly direction to <br />the confluence with the Green River at Echo Park, <br /> <br />The Yampa River is the largest tributary to the Green River with its basin covering approximately <br />9,530 square miles, This includes 6,719 square miles in northwestern Colorado and 2,811 square miles <br />in south central Wyoming, This a~ea represents approximately 6 percent and 3 percent of the total areas <br />of the states of Colorado and Wyoming, respectively. The Colorado portion contains most of Moffat and <br />Routt counties and small parts of Rio Blanco, Garfield and Grand counties, The Yampa River basin is <br />128 miles long from west to east and averages 75 miles in width. A location map of the basin is <br />presented in Figure 4-], <br />