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<br />Peak discharge-drainage area relationships for the South Platte River <br />are shown in Table 1. <br /> <br />Table 1. <br /> <br />Summary of Discharges <br /> <br />Drainage Area <br />(Square 11iles) <br /> <br />Peak Discharges <br />(Cubic Feet per Second) <br />la-Year 50-Year 100-Year 500-Year <br /> <br />Flooding Source <br />and Location <br /> <br />South Platte River <br />37th Avenue <br />U.S. Highway 85 <br /> <br />7,500 <br />7,500 <br /> <br />11,000 <br />11,000 <br /> <br />24,000 <br />24,500 <br /> <br />32,500 <br />32,500 <br /> <br />57,000 <br />57,500 <br /> <br />3.2 Hydraulic Analyses <br /> <br />Analyses of the hydraulic characteristics of streams in the community <br />were carried out to provide estimates of the elevations of floods of <br />the selected recurrence intervals along each stream studied in the <br />community. <br /> <br />Cross section data for the South Platte River in Evans were obtained <br />by field survey and from previous field surveys done by the U.S. Army <br />Corps of Engineers (Reference 5). Locations of selected cross <br />sections used in the hydraulic analyses are shown on the Flood Pro- <br />files (Exhibit 1). For stream segments for which a floodway is <br />computed (Section 4.2), selected cross section locations are also <br />shown on the Flood Boundary and Floodway Map (Exhibit 2) . <br /> <br />All bridges were surveyed by the u.S. Army Corps of Engineers to <br />obtain elevation data and structural geometry. <br /> <br />Roughness coefficients (Manning's "n") were estimated by field <br />inspection. The values used ranged from 0.035 to 0.044 for the <br />channel and from 0.035 to 0.100 for the overbank areas. <br /> <br />The water-surface profiles for the 10-, 50-, 100-, and SOD-year <br />floods were computed using the U. S. Army Corps of Engineers HEC-2 <br />computer program (Reference 7). <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). <br /> <br />Starting water-surface elevations were taken from the u.s. Army <br />Corps of Engineers study (Reference 5). <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 />8 <br />