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<br />floods. <br /> <br />Cross Sections <br /> <br />Eleven channel cross-sections were established in the study reach near the <br /> <br /> <br />Watson gage in May 1995, and 3 additional cross-sections were established in April <br /> <br /> <br />1997. Cross-sections were used to characterize channel geometry; we also identified bed <br /> <br /> <br />material at each side. Cross-sections were spaced approximately one channel width <br /> <br />apart, and were oriented perpendicular to the flow. Cross-section endpoints were <br /> <br />monumented with either rebar or fence posts which were pounded to depths such that <br /> <br />about 10-cm were exposed above ground surface. <br /> <br />Transects were measured by attaching a length-calibrated Kevlar tag-line to the <br /> <br />endpoints. A geodetic total station was used to measure ground-surface elevations under <br /> <br />the tag line as well as to measure water-surface elevation and elevations of geomorphic <br /> <br />surfaces near the channel. Elevation of cross-section endpoints were all surveyed to a <br /> <br />common reference datum. Elevation of the bed was measured either using the total <br /> <br />station and a rodman wading under the tagline, or was measured from a cataraft equipped <br /> <br />with a paper-trace echo sounder and outboard motor. When measuring the bed from a <br /> <br /> <br />raft, the boat operator maintained the boat carefully under the tag-line while slowly <br /> <br /> <br />crossing the river. A second individual in the raft measured depth and tag-line position <br /> <br /> <br />using the echo sounder at the marked locations along the tag-line. Measurements made <br /> <br />from the raft were duplicated at least 4 times. Where wading was feasible, bathymetric <br /> <br />. measurements made from the raft were also surveyed with the total station to verify the <br /> <br />accuracy of the echo-sounder. Echo-sounder measurements concurred with total station <br /> <br />12 <br />