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Fm-ev-i99s es: se Frame ~w ~toN a rinm <br />TO ~91303g930213 P.10 <br /> <br />section; between cross sections, the boundaries were interpolated <br />using topographic maps at a scale of ]:2400, with a contour <br />interval of 2 feet {Reference 12). <br />In cases where the i00- and the 500-year flood boundaries are <br />close together, only the 100-year boundary has been shown. <br />Approximate flood boundaries in Some portions of the study area <br />were taken from the Federal Insurance Administration's Flood <br />Hazard Boundary Map (Reference 1). <br />Fiood boundaries for the lOD- and 500-year floods are Shown on <br />the Flood Boundary and Floodway Map. Small areas within the flood <br />boundartes may lie above the flood elevations and, therefore, not <br />be subject to flooding; owing to limitations of the map scale, <br />such areas are not shown. <br />4.2 Floodways <br />Encroachmenfi on flood piains, such as artificial fill, reduces <br />the flood-carrying capacity, increases the flood heights, and <br />increases flood hazards in areas beyond the encroachment itself, <br />One aspect of flood plain management involves balancing Lhe <br />economic gain from flood plain development against the resulting <br />increase in flood hazard. For purposes of the Flood Insurance <br />Program, the concept of a floodway is used as a tool LO assist <br />local conmunities in this aspect of fiood plain management. <br />Under this concept, the area of the i00-year flood is divided <br />into a floodway and a floodway fringe. The floodway is the <br />channel of a stream, plus any aejacent flood plain areas, that <br />must be kept free of encroachment in order that Lhe ]00-year <br />flood be carried without substantiai increases in flood heights. <br />Minimum standards of FftiA limit such increases in flood heights <br />to 1.0 foot, provided that hazardous velocities are not pro- <br />duced, The floodways in this report are presented to total <br />agencies as minimum standards that can be adapted or that can <br />be used as a basis for additional studies. <br />The floodways presented in this study were Computed on the <br />basis of equal conveyance reduction from each side of the flood <br />plain. The results of these computations are tabulated at <br />Selected cross sections for each stream segment for which a <br />floodway was computed (Table 2). <br />A5 shown on the Flood Boundary and Floodx~ay Map, the floodway <br />widths were determined at cross sections; between cross sections, <br />the boundaries were interpolated. In cases where the floodway <br />and 100-year flood are either close together or coincide, only <br />the floodway boundary has been shown. <br />