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<br />Roughness coefficients (Manning's "n") were estimated by field inspec- <br />tion at each cross section and checked for reasonableness against a <br />recognized standard text (Reference 4). Roughness values for the <br />main channel ranged from 0.03S to 0.040; roughness values for the <br />flood plain ranged from 0.060 to 0.065. <br /> <br />Water-surface profiles of floods of the selected recurrence intervals <br />were developed using the u.s. Army Corps of Engineers HEC-2 computer <br />step-backwater model (Reference 5). <br /> <br />Starting elevations were taken from the upstream elevations of the La <br />Plata County Flood Insurance Study (Reference 6). <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 />The flood profiles shown in this report are based on the effects of <br />flow through unobstructed hydraulic structures and are, thus, consi- <br />dered valid only if these structures remain unobstructed and do not <br />faiL <br /> <br />All elevations are referenced to the National Geodetic vertical Datum <br />of 1929 (NGVD). Elevation reference marks used in the study are <br />shown on the maps. <br /> <br />4.0 FLOOD PLAIN MANAGEMENT APPLICATIONS <br /> <br />A prime purpose of the National Flood Insurance Program is to encourage <br />State and local governments to adopt sound flood plain management pro- <br />grams. Each Flood Insurance Study, therefore, includes a flood boundary <br />map designed to assist communities in developing sound flood plain manage- <br />ment 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 Insurance <br />Administration as the base flood for purposes of flood plain manage- <br />ment measures. The SOD-year flood is employed to indicate additional <br />areas of flood risk in the community. For the stream studied in <br />detail, the boundaries of the 100- and 500-year floods have been <br />delineated using the flood elevations determined at each cross <br />section; between cross sections, the boundaries were interpolated <br />using topographic maps enlarged to a scale of 1:4800, with a contour <br />interval of 20 feet (Reference 7). <br /> <br />Flood boundaries are indicated on the Flood Insurance Rate Map <br />(Exhibit 2). On this map, the 100-year flood boundary corresponds to <br />the boundary of the areas of special flood hazards (Zone A3); and the <br />SOQ-year flood boundary corresponds to the boundary of the areas of <br />moderate flood hazards (Zone B). <br /> <br />6 <br />