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<br />.. I <br /> <br />5.0 INSURANCE APPLICATION <br /> <br />In order to establish actuarial insurancli rates, the Federal Insurance <br />Administration has developed a process to transform the data from the <br />engineering study into flood insurance .crheria. This process includes <br />the determination of reaches, Flood Hazard Factors, and flood insurance <br />zone designations for each flooding sourc;estudied in detail affecting <br />the unincorporated areas of Adams County. <br /> <br />5.1 Reach Determinations <br /> <br />Reaches are defined as lengths of \<atercourses having relatively <br /> <br />the same flood hazard, based. on the 'average <br />water-surface elevations between the 110- and <br />difference does not have a variationigreater <br />the following table for more than 20 percent <br /> <br />weighted difference in <br />100-year floods. This <br />than that indicated in <br />of the reach: <br /> <br />Average Difference Between <br />10- and 100-Year Floods <br /> <br />Variation <br /> <br />Less than 2 feet <br />2 to 7 feet <br /> <br />0.5 foot <br />1. 0 foot <br /> <br />Seventeen reaches meeting the abovelcriteria were required for the <br />flooding sources studied in Adams I County. These included four <br />reaches for the South Platte River, ,three reaches each for Big Dry <br />and Little Dry Creeks, two reaches for Comanche Creek, and one <br />reach each for Little Comanche, Niver, Box Elder Creeks, and <br />Northfield Creek. (Downstream oB Devonshire Boulevard) and <br />Northfie1d Creek (Upstream of Devon~hire Boulevard). <br /> <br />5.2 Flood Hazard Factors <br /> <br />The Flood Hazard Factor (FHF) is the Federal Insurance <br />Administration device used to cotrelate flood information with <br />insurance rate tables. Correlatio,!s between property damage from <br />floods and their FHF are used to ~et actuarial insurance premium <br />rate tables based on FHFs fom 005 t6 200. <br /> <br />, <br />I <br />The FHF for. a reach is the average Iweighted difference between the <br />10- and 100-year flood water-sl.1rfaice elevations expressed to the <br />nearest one half foot, and showni as a three-digit code. For <br />example, if the difference between [the water-surface elevations of <br />the 10- and 100-year floods is 0.1 foot, the FHF is 005; if the <br />difference is 1.4 feet, the FHF i~ 015; if the difference is 5.0 <br />feet, the FHF is 050. When the difference between the 10- and 100- <br />year flood water-surface elevatio~s is greater than 10.0 feet, <br />accuracy for the FHF is to the near~st foot. <br />I <br /> <br />28 <br />