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Last modified
7/14/2009 5:02:29 PM
Creation date
5/20/2009 9:30:44 AM
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UCREFRP
UCREFRP Catalog Number
7136
Author
Johnson, J. E., et al.
Title
Flaming Gorge Tailwater Fisheries Investigations
USFW Year
1987.
USFW - Doc Type
Trout Growth, Harvest, Survival, and Microhabitat Selection in the Green River, Utah, 1978-82
Copyright Material
NO
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Study area <br />The Green River drains southward from the Wind River Range in <br />west-central Wyoming, joining the Colorado River as its largest tributary <br />in southeast Utah. Upon entering Utah from Wyoming, the river bends <br />sharply eastward, exits into the northeast corner of Colorado (Figure 1) <br />and, passing through Dinosaur National Monument, bends back westward, <br />reentering northeast Utah near the City of Vernal. <br />Flaming Gorge Dam is located 33 river miles downstream of the <br />Utah-Wyoming state line. The study area is composed of the 29 mi <br />(47.2 km) tailwater extending from Flaming Gorge Dam to the Colorado <br />state line (Figure 1). The upper 15.5 mi (24.9 km) is bounded by the <br />steep walls of Red Canyon. Consequently, access to this upper reach is <br />limited to raft and foot trails between three vehicle access points -- <br />Tailrace, Little Hole, and Indian Crossing. Little Hole and Indian <br />Crossing are raft ramps located 7.2 and 15.7 mi (11.6 and 25.3 km), <br />respectively, below Flaming Gorge Dam. Approaching Indian Crossing from <br />upstream, the steep walls of Red Canyon are gradually replaced by the <br />wide valley bottom known as Browns Park. Vehicle access to the river is <br />relatively unrestricted in Browns Park, except where the bottom is <br />briefly interrupted by Swallow Canyon, near the Utah-Colorado state line. <br />The elevation of the tailwater ranges from 5,594 ft. (1,705 m) at <br />Tailrace to 5,375 ft. (1,638 m) at the Utah-Colorado state line. Mean <br />gradient of the study area is 7.6 ft/mi (1.4 m/km). Above Red Creek, the <br />river's gradient is stairstepped at regular intervals by rapids and large <br />pools. In contrast, below Red Creek Rapids (4.2 mi downstream of Little <br />Hole) gradient is seemingly unbroken by distinct hydraulic controls. <br />-12-
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