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<br />remain separated from the main channel downstream to the yicinity <br />of cross section B (Reference 6). The extent and depth of this <br />shallow flooding were determined using normal-depth calculations. <br /> <br />The approximate 100-year flood elevations along the South Platte <br />River were developed by the COE, Omaha District (Reference 9). <br /> <br />Locations of selected cross sections used in the hydraulic analyses <br />are shown on the Flood Profiles, (Exhibit 1). For stream segments <br />for which a floodway was computed (Section 4.2), selected cross <br />section locations are also shown on the Flood Boundary and Floodway <br />Map (Exhibit 2). <br /> <br />The hydraulic analyses for this' study were based on unobstructed <br />flow. The flood elevations shown on the profiles are thus con- <br />sidered valid only if 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 this <br />study are shown on the maps. ' <br /> <br />4.0 FLOOD PLAIN MANAGEMENT APPLICATIONS <br /> <br />The National Flood Insurance Program (NFIP) encourages State and local <br />governments to adopt sound flood plain management programs. Therefore, <br />each Flood Insurance Study produces maps designed to assist communities <br />in developing flood plain management ~easures. <br /> <br />4.1 Flood Boundaries <br /> <br />To provide a national standard without regional discrimination, <br />the 1 percent annual chance (lOO-year) flood has been adopted <br />by FEMA as the base flood for flood plain management purposes. <br />The 0.2 percent annual chance (500-year) flood is employed to <br />indicate additional areas of flpod risk in the community. For <br />each stream studied in detail, the 100- and SOO-year flood plain <br />boundaries have been delineated! using the flood elevations determined <br />at each cross section. Between! cross sections, the boundaries <br />were interpolated using topographic maps at a scale of 1:1,200, <br />with a contour interval of 2 feet (Reference 8). <br /> <br />Boundaries for the shallow flooding areas were delineated using <br />topographic maps at a scale of ~:1,200, with a contour interval <br />of 2 feet (Reference 8) in conj~nction with previously determined <br />elevations. <br /> <br />Approximate flood boundaries alpng the South Platte 'River were <br />taken from the Flood Insurance ,Rate Maps for the CitY of Sheridan <br />and Arapahoe County (References, 10 and 11). <br /> <br />8 <br />