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<br />Research emphasis will be placed on stream reaches between elevations of <br />7,000 to 10,000 feet above mean sea level (8,000 to 11,000 feet above mean sea <br />level in the Arkansas River basin) and at major tributaries. A tentative schedule <br />for research activities for several foothill basins is presented in table 5. <br /> <br />Table 5.--Basins in which research studies on channel geometry, <br />geomorphology, and botany will be conducted <br /> <br />lA, Arkansas River basin; C, Colorado River basin; <br />5, South Platte River basin] <br /> <br />Basin <br /> <br />Boulder Creek (5)* <br />Bear Creek (5)* <br />Big Thompson River (5)* <br />Fountain Creek (A)* <br />Animas River (C)* <br />Sweetwater Creek (C)* <br />San Juan River (C) <br />St. Vrain Creek (5) <br />Purgatoire River (A) <br />Clear Creek (5) <br />Huerfano River (A) <br />Turkey Creek (5) <br />Cache la Poudre River (5) <br />Cucharas River (A) <br />Roaring Fork River (C) <br />Grape Creek (A) <br />Whi te River (C) <br />Fourmile Creek (A) <br />Beaver Creek (A) <br />Yampa River (C) <br />Eagle River (C) <br />Dolores River (C) <br />San Miguel River (C) <br />St. Charles River (C) <br /> <br />*Research studies started in 1978. <br /> <br />Studies of channel hydraulics and geometry.--The operational hypothesis in <br />this part of the study is that discernible changes occur in channel features as <br />elevation increases in foothill basins, and that these changes can be related to <br />the type of flood-producing event. Field measurements of channel features such as <br />width, depth, and slope are being made at selected locations along foothill <br />streams. These data are being studied to identify channel-characteristic changes <br />with elevation or to reject the hypothesis that discernible patterns exist. If <br />the hypothesis is accepted, additional study will be made of the degree of <br />association of channel-characteristic changes among basins. <br /> <br />19 <br />