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<br />22 <br /> <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 />Figure 1 (below) is a hydraulic map of House Rock <br />Rapid, Grand Canyon, Arizona (River Mile [RM] 17). <br />North is to the left; the water is flowing from left to <br />right. The channel of the river occupied by pre-dam <br />discharges extends approximately up to the 925 m <br />contour level. The channel below the discharge of <br />5,000 cfs, shown here, cannot be mapped; however, some <br />fathometer data were obtained to allow estimates of <br />channel depth below the levels filled by a discharge of <br />5,000 cfs. The contours were compiled from aerial <br />photographs flown by the U. S. Bureau of Reclamation <br />during the Glen Canyon Environmental Studies, with <br />control points surveyed by the author. The contour <br />interval is 1 m (solid lines) or 0.5 m (dashed lines). <br />The hydraulic structure of the water and important <br />features of the channel bottom are shown by air brush <br />illustration. The boat on the lower left is 33 ft in <br />length, and is shown only for scale. Like all of the <br />major rapids in the Grand Canyon, House Rock Rapid is <br />formed by constriction of the river channel by debris <br />from a' side canyon (Rider Canyon enters from the west, <br />at the bottom of the figure). The area covered by <br />diagonal pattern is a sandy beach formed by deposits <br />from the eddy in the lower right corner of the figure. <br />Diagonal lines in the opposite direction indicate <br />vegetation. <br /> <br />