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2 <br />3) Relate hydraulic and sediment transport data collected in the <br />Yampa Canyon at Mathers Hole and river mile 16.5 to the <br />upstream gaging stations. <br />4) Mathematically simulate the observed flow conditions and <br />sediment transport for the 1983 runoff season. <br />5) Predict the minimum streamflow hydrograph which will sustain a <br />range of natural conditions and processes vital to the <br />riparian ecology in the cobble bed reach. <br />After the investigation was initiated the following additional <br />objectives were appended to the original proposal: <br />1) Perform a physical model study to calibrate the Helley-Smith <br />bedload sampler. This flume investigation would also define <br />the phenomena of sand transport over cobble substrate. <br />2) Describe the morphological characteristics of the observed <br />Colorado squawfish spawning reach. <br />3) Determine the range of discharges that are required to <br />preserve the morphological conditions that were observed or <br />projected to have existed during the 1981-3 Colorado squawfish <br />spawning periods. <br />The report describes how these objectives were accomplished. Background <br />information is provided to acquaint the reader with the morphology and <br />geology of the Yampa River Canyon. In addition, the methods of field <br />data collection and sample analysis are discussed. The results have <br />been divided into several sections including; historical flow, sediment <br />transport, and physical and mathematical modeling. Additional detailed <br />information on some technical aspects of the investigation are provided <br />in the appendices. <br />BACKGROUND <br />Yampa River Geography and Geology <br />Dinosaur National Monument is in the northwestern and northeastern <br />corners of Colorado and Utah, respectively. It lies between Craig, <br />Colorado and Vernal, Utah. The monument is about 70 miles long (east to <br />west), and ranges from 10 to 25 miles wide (north to south). <br />The Yampa River headwaters in the White River National Forest on <br />the western slope of the Rocky Mountains near Yampa, Colorado. The <br />Yampa flows north, then west joining the Green River in Dinosaur <br />National Monument (see Figure 1). It is the Green River's largest <br />tributary and drains approximately 7600 square miles before entering the <br />Monument. <br />An average 1.5 million acre feet of water flow through the Monument <br />each year in the Yampa, contributing on the average 1.5 to 2.0 million <br />tons of sediment per year. Almost all of the sand sediment load is