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Last modified
7/14/2009 5:02:30 PM
Creation date
5/22/2009 12:54:35 PM
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UCREFRP
UCREFRP Catalog Number
7394
Author
Grabowski, S. J. and S. D. Hiebert.
Title
Some Aspects of Trophic Interactions in Selected Backwaters and the Main Channel of the Green River, Utah 1987 - 1988.
USFW Year
1989.
USFW - Doc Type
Denver, Colorado.
Copyright Material
NO
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<br />METHODS AND MATERIAL <br /> <br />Study Area <br /> <br />Three widely separated areas in an 84-mile reach of the Green River, near <br />Vernal, Utah, with a range of backwater types and with previously reported <br />differing populations of larval Colorado squawfish were selected for the study <br />with assistance of USFWS and USBR personnel. The three study areas were <br />located at Island Park in Dinosaur National Monument, at Jensen downstream <br />from the Route US 40 bridge over the Green River, and at Ouray on the Ouray <br />National Wildlife Refuge (fig. 1). Previous studies by the USFWS and the Utah <br />Department of Natural Resources indicated increasing abundance of larval <br />Colorado squawfish in backwaters downstream from Island Park to Ouray. <br />Abundance of larval Colorado squawfish was greatest in Ouray area backwaters. <br /> <br />In 1986, USFWS personnel familiar with the river designated certain backwaters <br />that apparently persisted from year to year as "reference" backwaters, <br />cnadidates for long-term study. They also defined five categories of <br />backwaters, including ephemeral, deep side channel, tributary, wash, and <br />flooded bottom. In 1987, the "reference II backwater at Island Park did not <br />develop, however, so a main river site and two backwaters were selected <br />upstream near the confluence of Garden Creek (BA 332.2) and at Big Island <br />(BA 333.2). Garden Creek backwater was initially large but decreased <br />substantially in size as river flows decreased during the summer and <br />eventually became the "small" backwater at Island Park. Initially the small <br />backwater was a backwater off a side channel of the river; this backwater <br />dried up as riverflows dropped, resulting in a cut-off side channel. This was <br /> <br />12 <br />
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