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<br />Grams and Schmidt 27 <br /> <br />List of Tables <br />Table 1. -- Length of geomorphic and lithologic subreaches within study area showing the <br />bedrock resistance classification for each formation. <br /> <br />Table 2. -- Abundance of stream bank material and bed material for each geomorphic <br />subreach. Bank material determined by GIS analysis of surficial geologic maps <br />made for this study. Bed material determined from surveyed channel cross sections. <br />Fine-grained alluvium includes all sand, silt, and clay. <br /> <br />Table 3. -- Distribution of alluvial deposits by reach, determined from surficial geologic <br />maps. <br /> <br />Table 4. -- Median particle diameter and lithology of the gravel bar surface layer for <br />gravel bars within two fan-eddy complexes in Lodore Canyon. <br /> <br />Table 5. -- Reach average channel geometry at bankfull discharge and reach average slope <br />(U.S. Geological Survey, 1924). Channel geometry calculated from surveyed <br />channel cross sections. <br /> <br />Table 6. -- Channel constricting feature responsible for the formation of rapids, by <br />geomorphic subreach. Data collected from 1 :5000 scale aerial photographs taken <br />during low discharge. <br />! <br /> <br />::- <br />