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<br />. <br /> <br />Introduction <br /> <br />. <br /> <br />. <br /> <br />The Duchesne'River originates from headwaters on the south slope of the Uinta <br />Mountains in northeastern Utah. It includes two major drainages, the Strawberry and Duchesne, <br />which together encompass over 1000 square kilometers (4,247 square miles), Major tributaries <br />to the Duchesne River include the Whiterocks River, Uinta River, Dry Gulch, Yellowstone <br />River, Lake Fork, Rock Creek, North Fork Duchesne River, West Fork Duchesne River, <br />Antelope Creek and the Strawberry River. Flows in the Duchesne River are affected by the <br />Strawberry Aqueduct and Collection System (SACS) and Starvation Reservoir which are both <br />components of the Bonneville Unit of the Central Utah Project (CUP). Starvation Reservoir, <br />located on the Strawberry River approximately 6 miles upstream from the confluence with the <br />Duchesne river, stores both Strawberry River and Duchesne River water and regulates flow into <br />the lower Strawberry River. Water diverted from the Duchesne River at the Knight Diversion is <br />delivered directly to Starvation Reservoir, The SACS diverts water from the West Fork ofthe <br />Duchesne River and two of its tributaries, tributaries of the North Fork ofthe Duchesne River, <br />Rock Creek, and several tributaries of Rock Creek (IABAT 1994). Operation of these CUP <br />facilities and additional water depletions through several irrigation diversions results in daily, <br />monthly, and yearly flow changes of the Duchesne River which have the potential to affect the <br />quantity and quality of aquatic resources within the affected streams. <br />The Duchesne River has changed significantly during the past 100 years. These changes <br />can be correlated to changes in the hydrology of the river (Brink and Schmidt 1996). Duchesne <br />River flows, unlike the Yampa River and White River, have been drastically altered, Total <br />annual discharge of the Duchesne River has been reduced from historical levels of over 768,000 <br />acre feet to approximately 400,000 acre feet (CH2M Hill 1997). <br />The endangered Colorado pikeminnow (Ptychocheilus lucius) and razorback sucker <br />(Xyrauchen texanus) along with native bluehead sucker (Catostomus discobolus), flannelmouth <br />sucker (C. latipinnis), and roundtail chub (Gila robusta), listed as sensitive by the state of Utah, <br />have been captured regularly in the lower Duchesne River (Archer et aL 1986, Cranney 1994), <br />The lower 2.5 miles of the Duchesne River was designated as critical habitat for razorback <br />sucker in 1994 (Fed. Reg.NoL 59, No. 54/Monday, march 21, 1994). Recent captures of <br />Colorado pikeminnow and razorback sucker upstream of designated critical habitat (Cranney <br />1993) suggest that the Duchesne River may have a greater role in recovery than previously <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />1 <br /> <br />. <br />