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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 />SEDIMENT TRANSPORT STUDIES OF TIlE UTILE SNAKE, <br />YAMPA, AND GREEN RIVER SYSTEMS <br /> <br />INTRODUCTION <br /> <br />1.1 Study O~jectives <br /> <br />The objective of this study was to establish baseline hydrologic and sediment transport information <br />on the Uttle Snake, Yampa, and Green River systems. These river systems are part of the upper Colorado <br />River basin and are an integral part of the Recovery Implementation Program for Endangered FISh Species <br />(USFWS, 1987). One concern of the Recovery Program is the potential for adverse modification of <br />threatened and endangered fish habitat as a result of morphological changes. Various rare fish species <br />utilize different river channel habitats during their respective life stages; two habitats focused on to date <br />include spawning and backwater areas. Both of these habitat areas are known to exist in the Yampa and <br />Green Rivers. Morphological changes that could adversely impact these habitats include: <br /> <br />Significant reductions in transport capacity of the mainstem Yampa River may result in <br />sedimentation of the cobble spawning bars, or sedimentation of the pool/riffle habitat. Clean <br />cobble substrate may be required for successful spawning. <br /> <br />Significant reductions in transport capacity of the Green River may allow aggradation in backwater <br />areas resulting in the loss of backwater habitat through merging of islands and bars with stream <br />banks. <br /> <br />Significant reductions in sediment supply to the Green River may allow channel degradation and <br />narrowing, with concurrent alteration of backwater habitats. <br /> <br />In order to understand and predict potential morphological response resulting from both natural <br />and man-induced changes, it is important to first understand existing conditions and river response <br />mechanisms. This report relies on previous research efforts, supplemented by additional field and <br />analytical investigations, in an effort to consolidate and establish important baseline information related to <br />hydrology and sediment transport processes in the Uttle Snake, Yampa, and Green River systems. <br /> <br />1.2 Drainage Areas and Existin~ Water Development Pr~ects <br /> <br />The Green River is a major tributary of the Colorado River with a drainage area of 44,700 square <br />miles (Fig. 1.1). The Yampa River is a major tributary to the Green River with a drainage area of about <br />8,000 square miles in northwestern Colorado and south central Wyoming (Fig. 1.2). The Little Snake <br />River is a major tributary to the Yampa with a watershed area of about 3,730 square miles, joining the <br />Yampa River at Deerlodge Park. <br /> <br />The Green River originates in southwestern Wyoming and is controlled by two mainstem <br />reservoirs, Fontenelle and Flaming Gorge. Flaming Gorge is located 410 miles upstream of the Colorado <br />River confluence and was completed in 1962. Fontenelle Reservoir is about 150 miles upstream of Flaming <br />Gorge and was completed in 1964. <br /> <br />1-1 <br />