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<br />4.0 FLOOD PLAIN MANAGEMENT APPLICATIONS <br />- -- - -~----------,.- <br /> <br />A prime purpose of the National Flood Insurance ~rogram 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 discrimi- <br />nation, the IOO-year flood has been adopted by the Federal Insurance <br />Administration as the base flood for purposes of flood plain manage- <br />ment. The SOD-year flood is employed to indicate additional areas of <br />flood risk. For streams studied by detailed methods, the boundaries <br />of the 100-year and SOD-year floods were delineated using the flood <br />elevations determined at each cross section; between cross sections, <br />the boundaries were interpolated using topographic maps with a scale <br />of 1:4800 feet, with a contour interval of S feet or less (Refer- <br />ence 10). <br /> <br />For streams studied by approximate methods, the boundary of the 100- <br />year flood was established according to the professional judgment of <br />engineers familiar with the region, taking into account flood eleva- <br />tions from historical flood data, minor hydrologic and hydraulic <br />analyses, correlations with similar stream basins studied in detail, <br />and field observations. <br /> <br />Small areas within the flood boundaries may lie above the flood <br />elevations and, therefore, not be subject to flooding; owing to <br />limitations of the map scale, such areas are not shown. <br /> <br />In cases where the 100- and SOD-year flood boundaries are close <br />together, only the 100-year flood boundary has been shown. In areas <br />where the floodway and 100-year flood are close together, only the <br />floodway has been shown. <br /> <br />Some areas in Steamboat Springs are subject to sheetflowi that is, <br />broad, shallow, overland flooding generally less than 3 feet deep and <br />characterized by unpredictable flow paths. The water-surface eleva- <br />tions of flooding in these areas are essentially independent of those <br />along adjacent streamways and are affected principally by obstructions <br />in the flooded areas. <br /> <br />4.2 F100dways <br /> <br />Encroachment on flood plains, such as artificial fill, reduces the <br />flood-carrying capacity and increases flood heights, thus increasing <br />flood hazards in areas beyond the encroachment itself. One aspect of <br />flood plain management involves balancing the economic gain from <br />flood plain development against the resulting increase in flonn <br /> <br />24 <br />