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Last modified
7/14/2009 5:02:36 PM
Creation date
5/22/2009 7:28:33 PM
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UCREFRP
UCREFRP Catalog Number
9556
Author
Bestgen, K. R., K. A. Zelasko and C. T. Wilcox.
Title
Non-native fish removal in the Green River, Lodore and Whirlpool canyons, 2002-2006, and fish community response to altered flow and temperature regimes, and non-native fish expansion.
USFW Year
2007.
USFW - Doc Type
115,
Copyright Material
NO
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STUDY AREA <br />The Green River Basin drains mountainous and high desert portions of southern Wyoming, <br />eastern Utah, and northwestern Colorado (Fig. 1) and is the largest tributary of the Colorado <br />River. The study area encompassed the Green and Yampa rivers in and above Dinosaur National <br />Monument and included highly regulated and regulation-attenuated river reaches. The Green <br />River below Flaming Gorge Dam downstream to near Jensen, Utah, was the primary focus of the <br />study. The river below Flaming Gorge Dam flows for 22 km through Red Canyon, enters the <br />48-km-long low gradient Browns Park valley, and then flows for 32 km through high-gradient <br />Lodore Canyon before entering Echo Park at the Yampa River confluence. From Echo Park, the <br />Green River flows 18 km mostly through Whirlpool Canyon, another 11 km through Island- <br />Rainbow Park, and another 13 km through Split Mountain Canyon before emerging into the <br />alluvial Uintah Basin valley reach near Jensen. <br />Extent of river meandering (river plan form) and habitat types in the major reaches of river <br />are controlled by local geology. In Lodore, Whirlpool, and Split Mountain canyons the <br />Green River is generally confined to a single, relatively narrow channel. Canyon river reaches <br />constricted by debris fans form riffles and rapids with cobble and boulder substrate. These river <br />reaches generally have higher current velocities and deeper runs and pools than lower gradient <br />areas without debris fans. In lower gradient alluvial reaches such as Browns and Island- <br />Rainbow parks, river plan form is characterized by restricted meanders (Grams 1997), and the <br />channel is relatively wide, shallow, and sometimes interspersed with islands. Lower velocity <br />runs with sand and cobble substrate predominate. <br />Flaming Gorge Dam in northeastern Utah impounds the mainstem Green River at the <br />upstream end of the study area. With a storage capacity of 3.74 million acre-ft (4,624 million <br />m'), it is the largest reservoir in the Green River Basin. Upstream Fontenelle Reservoir, the only <br />other mainstem Green River reservoir, does not appreciably affect releases from Flaming Gorge <br />Dam. Flaming Gorge Dam was closed in 1962 as part of the Colorado River Storage Project <br />(CRSP) to store water so that states of the Upper and Lower Colorado River basins (Wyoming, <br />7 <br />
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