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Last modified
7/14/2009 5:02:29 PM
Creation date
6/1/2009 12:39:52 PM
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UCREFRP
UCREFRP Catalog Number
7163
Author
Haynes, C. M. and J. R. Bennett.
Title
Relationship between the Preservation of Wilderness Values and Endangered Species
USFW Year
1985.
USFW - Doc Type
A Case-Study from the Upper Colorado River Basin, U.S.A.
Copyright Material
NO
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0 <br />STUDY AREA <br />The primary study area was the White River (Figure 1) <br />between 0-rkm at the confluence of the Green River to 206.0-rkm <br />just downstream of the White River and Yellow Creek confluence. <br />The White River is a tributary to the Green River in the Upper <br />Colorado River Basin. It arises in western Colorado in the Flat <br />Top Mountains and flows westerly for about 402-rkm (250 mi) <br />before entering the Green River, draining almost 1.3 million ha <br />(3.2 million acres) of northwestern Colorado and eastern Utah. <br />The expanded study <br />193-rkm near Green Rive <br />downstream of the Gates <br />Colorado, and the Yampa <br />Yampa rivers confluence <br />(Figure 1). <br />area encompassed the Green River between <br />r, Utah, to 567-rkm at Triplet Falls, <br />of Lodore in Dinosaur National Monument, <br />River between 0-rkm at the Green and <br />to 81-rkm at Cross Mountain, Colorado <br />The White River flows through arid pinion-juniper, <br />sagebrush, and barren land habitat on public, private, and tribal <br />reservation lands (Lanigan and Berry 1979, Martinez 1986, Miller <br />1982, Trammell 1991). It is a coolwater/warmwater system that is <br />subject to extremes in discharge and frequently carries a heavy <br />silt load. The high-gradient river reaches are dominated by <br />riffles, runs, and rapids that flow through canyon areas with <br />sheer cliffs and boulder-strewn banks. The substrate consists of <br />large to medium cobble. The low-gradient areas are characterized <br />by deep eddies, pools, and runs that meander through slower warm <br />and turbid waters with shorelines vegetated with cottonwood, <br />willow, and saltcedar. Summer water temperatures often reach <br />201C. Sand, silt, and some gravel substrates are formed from <br />shale rock and are easily moved by seasonal floods from desert <br />tributaries. Most tributaries to the river are intermittent. <br />Peak spring discharge ranges between 4,000-6,000 cfs. <br />The areas around the White River are primarily used for oil <br />and gas production, agriculture, livestock grazing, water <br />development, and recreation. Taylor Draw Dam, near Rangely, <br />Colorado, was constructed in 1985 for agricultural water storage, <br />municipal water needs, recreational use, and some flood control <br />(personal communication, Mr. Jim Gyler, Taylor Draw Dam Manager). <br />In the spring of 1993 a generator was retro-fitted to the Taylor <br />Draw Dam to provide hydroelectric power. <br />Seven endemic and thirteen exotic fish species (Table 1) are <br />found in the White River (Martinez 1986, Lanigan and Berry 1979). <br />The only endangered species collected to date in the White River <br />is the Colorado squawfish. <br />0 <br />3 <br />0
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