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<br />Indian Wash ranged from 0.022 to 0.06 and in the flood plain from <br />0.03 to 0.09. <br /> <br />The starting water-surface elevations for Colorado River, Leach <br />Creek, and Horizon Drive Channel were obtained from the Mesa County, <br />Colorado, Flood Insurance Study (Reference 1). Starting water- <br />surface elevations for Indian Wash were estimated using a rating <br />chart developed for the upstream side of the large culvert passing <br />under the multiple tracks of the Denver & Rio Grande Western Rail- <br />road near the south end of the study reach. <br /> <br />Flood profiles were drawn showing computed water-surface elevations <br />to an accuracy of 0.5 foot for floods of the selected recurrence <br />intervals (Exhibit 1). The results obtained from the HEC-2 computer <br />program were adjusted in the vicinity of bridges to represent <br />more accurately the actual flooding conditions (Reference 11) . <br /> <br />The hydraulic analyses for this study were based on unobstructed <br />flow. The flood elevations shown on the flood profiles are, thus, <br />considered valid only if the hydraulic structures remain unobstructed, <br />operate properly, and do not fail. <br /> <br />All elevations are referenced to the National Geodetic Vertical <br />Datum of 1929 (NGVD). Elevation reference marks used in the study <br />are shown on the maps. <br /> <br />4.0 FLOOD PLAIN MANAGEMENT APPLICATIONS <br /> <br />The National Flood Insurance Program encourages State and local govern- <br />ments to adopt sound flood plain management programs. Therefore, each <br />Flood Insurance Study includes a flood boundary map designed to assist <br />communities in developing sound flood plain management measures. <br /> <br />4.1 Flood Boundaries <br /> <br />In order to provide a national standard without regional discrimina- <br />tion, the 100-year flood has been adopted by the Federal Emergency <br />Management Agency as the base flood for purposes of flood plain <br />management measures. The 500-year flood is employed to indicate <br />additional areas of flood risk in the community. For each stream <br />studied in detail, the boundaries of the 100- and 500-year floods <br />have been delineated using the flood elevations determined at <br />each cross section; between cross sections, the boundaries were <br />interpolated using an orthophoto topographic map at a scale of <br />1:2400, with a contour interval of 2 feet (Reference 10). <br /> <br />Flood boundaries for the 100- and 500-year floods are shown on <br />the Flood Boundary and Floodway Map (Exhibit 2). In cases where <br />the 100- and 500-year flood boundaries are close together, only <br />the 100-year flood boundary has been shown. Small areas within <br /> <br />18 <br />