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<br />Table 1. Summary of Discharges <br /> <br />Flooding Source <br />and Location <br /> <br />Drainage <br />Area <br />(Square <br />Miles) <br /> <br />South Platte River <br />Franklin Street <br />Upstream of Conflu- <br />ence with Sand <br />Creek <br />Interstate 76 <br /> <br />3,8201 <br /> <br />3,8301 <br />4,0251 <br /> <br />Sand Creek <br />Quebec Street 189 <br />Mouth at South Platte <br />Ri ver 196 <br /> <br />Peak Discharges <br />(Cubic Feet per Second) <br /> <br />10-Year SO-Year 100-Year 500-Year <br /> <br />8,500 12,500 17 ,200 26,500 <br />8,500 12,500 17,200 26,500 <br />17,500 29,000 37,200 60,000 <br />10,500 23,300 30,000 33,000 <br />11 ,000 24,200 30,500 36,200 <br /> <br />1 Includes Area Above Chatfield, Bear Creek, and Cherry Creek Dams. <br /> <br />3.2 Hydraulic Analyses <br /> <br />Analyses of the hydraulic characteristics of streams in the <br />community were carried out to provide estimates of the elevations <br />of floods of the selected recurrence intervals along each stream <br />studied in detail. Cross section data for the South Platte River <br />was obtained by field surveys and cross section data for Sand <br />Creek was taken from ael:"ial contour mapping (Reference 3). All <br />bridges and culverts were surveyed or the information was <br />provided by the Colorado Department of Highways to obtain <br />elevation data and structural geometry. Locations of selected <br />cross sections used in the hydraulic analyses are shown on the <br />Flood Profiles (Exhibit 1). For stream segments for which a <br />floodway is computed (Section 4.2), selected cross section <br />locations are also shown on the Floodway Map (Exhibit 2). <br /> <br />Roughness coefficients (Manning's "n") were estimated by field <br />inspection. The range of "n" values used for Sand Creek were <br />from 0.025 to 0.045 and those for the South Platte River were <br />from 0.035 to 0.070. <br /> <br />Water-surface profiles were developed using the HEC-2 step- <br />backwater computer program (Reference 4). Profiles were <br />determined for the 10-, 50-, 100- and 500-year floods. Flood <br />profiles were drawn showing computed water-surface elevations to <br />an accuracy of IO.5 foot. All starting water-surface elevations <br />for the South Platte River were taken from the Adams County, <br />Colorado, Flood Insurance Study (Reference 5). The starting <br />water-surface elevations for Sand Creek were those computed for <br />the South Platte River at the confluence. All elevations are <br /> <br />11 <br />