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<br />I <br /> <br />I <br /> <br />14 <br /> <br />I <br /> <br />I <br /> <br />The lower portion of Fourmile Gulch was analyzed using HEC-2 computer model. The <br />100-year event in the lower reach of the Gulch is wholly carried within a storm sewer, <br />thus, there is no floodplain in this area of Fourmile Gulch. The approximate floodplain <br />delineated on the 1984 FIRM is used to estimate the 100-year floodplain upstream of the <br />floodplain~identified-by the~Jj0MR-~ nThis-floodplain~ is-also~shown-on~~Figures"~5 A~and~~~~. ~~~~~ <br />5B <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Updated 100-year floodplain delineation in the City of Black Hawk for North Clear <br />Creek, Chase Gulch, and Gregory Gulch uses the HEC-2 (USACE, 1991) hydraulic <br />model and is presented in the recently submitted Physical Map Revision to FEMA. The <br />North Clear Creek model begins downstream at the Richman Street Bridge and extends <br />upstream to the City limits. The North Clear Creek floodplain extending downstream <br />from the Richman Street Bridge to the City boundary was addressed in two studies <br />submitted to FEMA, including FEMA Case No. 03-08-0439R (Mardi Gras Casino) and <br />98-08-258R (Riveria Casino); and a CLOMR prepared for Jackpot Springs (including an <br />HEC-2 analysis) which has not yet been submitted to FEMA. These data represent the <br />best available information on the 100 year floodplain along North Clear Creek <br />downstream of the PMR and are incorporated in the Flood Information Report. The 100- <br />year floodplain obtained from the detailed hydraulic analysis within the City of Black <br />Hawk is shown of Figures SA and 5B. <br /> <br />I <br /> <br />I <br /> <br />Hvdraulic Anal <br /> <br />Flood peak discharges for the 10-, 50-, 100-, and 500-year events for North Clear Creek, <br />Gregory Gulch, and Chase Gulch used in the floodplain study is summarized in Table 1. <br /> <br />sis <br /> <br />I <br /> <br />The approximate floodplain for Fourmile Gulch identified in the 1984 FIRM was updated <br />near the confluence with a LOMR (Carroll & Lange, 2001). Flood peaks for the 100- <br />year event were estimated using SCS methodology and the HEC-1 computer model at <br />various design points. The flood peaks were approved by CWCB. <br /> <br />I <br /> <br />I <br /> <br />Q <br />Q <br />A <br />A <br /> <br />I <br /> <br />2 <br /> <br />I <br /> <br />2 <br /> <br />= projected flood peak, cfs, <br />= known flood peak, cfs, <br />= drainage area at projected site, mi2 <br />= drainage area at known site, me. <br /> <br />and, <br /> <br />I <br /> <br />where; <br /> <br />QI =Q2 {A <br /> <br />/ <br /> <br />A 2 } 0,79 <br /> <br />0.5 < <br /> <br />{A <br /> <br />/ <br /> <br />A <br /> <br />2 } <br /> <br /><2 <br /> <br />(McCain et al <br /> <br />1976) <br /> <br />I <br /> <br />Scattered development is occurring within the North Clear Creek valley downstream <br />Black Hawk. Flood peak estimates below City limits at the confluence with Clear <br />are calculated using the area ratio equation suggested by McCain et aI., <br /> <br />of <br />Creek <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />events are reduced by the 200 cfs which <br />of Gregory Gulch in Black Hawk. <br /> <br />is carried within the flume for the entire length <br />