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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />t <br /> <br />3.6 Bed Material Data in Yam.pa Canyon <br /> <br />Surface material gradation of the cobble bars in the spawning reach of Yampa Canyon was <br />evaluated based on grid-by-number techniques (see Section 33.2). The results of this analysis are shown in <br />FIg. 3.9. The particle size range of the cobble bar surfaces in the canyon was 30-150 mm. At river mile 16.5, <br />a documented spawning site, the d50 is about 38 mm at the sample location. <br /> <br />The gradations of the sand sized material in the pools above nn 16.5 and 18.5 are shown in Fig. <br />3.10. Note that the d50 of these samples (3-7 mm range) compares favorably with the sand size material in <br />transport in the Little Snake River (see Fig. 3.8). <br /> <br />3.7 Special GeolofPcal Investi~ations <br /> <br />Bed material samples for major ephemeral tributaries to Little Snake River were collected to <br />explore the possibility of using geologic source tracing for predicting sediment supply sources. Samples <br />were collected at the five Little Snake stream gaging/sediment sites as a Helley-Smith bedload sample. In <br />some cases at low flow, bed material grab samples were also collected at these locations. Samples were <br />also collected in the thalweg of major tributaries to the Little Snake close to the points of confluence. <br />Analysis of these samples contributed to the sediment source area investigation (Section 63). <br /> <br />3-9 <br />