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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 />I <br /> <br />THE RAPIDS AND WAVES OF THE COLORADO RIVER <br />GRAND CANYON, ARIZONA <br /> <br />The hydraulics and geomorphology of 12 rapids on the <br />Colorado River are described in this report, on a 20- <br />min VHS videotape1 (U.S. Geological Survey [USGS] Open <br />File Report 86-503), and on ten hydraulic maps (USGS <br />Miscellaneous Investigations map 1-1897, parts A-J). <br /> <br />By Susan Werner Kieffer <br />Branch of Igneous and Geothermal Processes <br />U.S. Geological Survey <br />Flagstaff, Arizona <br /> <br />INTRODUCTION <br /> <br />Each rapid of the Colorado River is unique, but the <br />major rapids have many hydraulic features in common. <br />In this report, I describe the general features of 12 <br />of the major rapids of the river in Marble Canyon and <br />Grand Canyon, and address the following topics: (1) <br />definition of the hydraulic and geomorphic features at <br />rapids: (2) location of the rapids in terms of geologic <br />structures of the Colorado Plateau: (3) channel geom- <br />etry and hydraulic structures: (4) causes of rapids, <br />pools, and scour holes: (5) a generalized hydraulic <br />model for rapids: (6) hydraulic nature of pools and <br />backwaters: (7) hydraulic nature of tongues and lateral <br />waves: (8) breaking waves in the rapids: (9) behavior <br />of water near large rocks within rapids: (10) movement <br />of boulders and erosional contouring of the river chan- <br />nel at rapids: (11) the relation of rapids to rock <br />gardens below them: and (12) minor effects, such as <br />curvature of the river at rapids. <br /> <br />OBJECTIVES <br /> <br />Work on the Colorado River by Howard and Dolan (1976), <br />related work by Graf (1980) on similar rivers, and pre- <br />liminary work done at Crystal Rapid by Kieffer in 1983 <br />(Kieffer 1985) has demonstrated that Grand Canyon ra- <br />pids have changed since Glen Canyon Dam was closed in <br />1963. Data on the shape of the river channel and the <br />material that lines it are conspicuously absent and <br />are needed before response of the rapids to discharges <br /> <br />1 The video may only be obtained by requesting it <br />from the author (U. S. Geological Survey, 2255 Gemini <br />Drive, Flagstaff, Arizona 86001. <br /> <br />19 <br />