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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />used to compute the lOa-year flow were applied. The SOO-year flow was <br /> <br /> <br />extrapolated based upon the resulting frequency-discharge curve of the 10-, <br /> <br /> <br />50- and lOa-year flow rates. Peak discharges have been presented in <br /> <br /> <br />Table 1. <br /> <br />No existing hydrologic information was found for Forked Gulch, Sand Creek <br />or Southeast Canon Drainage, therefore COM developed these flows using the <br />Soil Conservation Service method. This method was applied in order to <br />achieve a consistency of methodology for the Arkansas River tributaries in <br />Canon City. The resulting peak flow rates were submitted to FEMA and CWCB <br />in the form of a letter (March 16, 1981). The individual stream basins <br />were delineated and the methods as outlined in Reference 9 were applied. <br />Peak flow rates for Forked Gulch, Sand Creek and Southeast Canon Drainage <br />have also been presented in Table 1. / <br /> <br /> <br />Town of Del Norte, Colorado <br /> <br />The stream studied in Del Norte, Colorado was the Rio Grande River. The <br />literature search revealed no existing flood flow information for use,in <br />the flood insurance study for Del Norte, and therefore CDM developed new <br />hydrologic data. A stream gage station analysis as outlined in <br />Reference 15 was applied to the USGS gage station at Del Norte. The <br />resulting frequency-discharge curve is shown in Figure 3. These peak flow <br />rates were recommended for use in the flood insurance study in Del Norte, <br />(reference CDM's letter to FEMA, May 14, 1980, Appendix A). The peak flow <br />rates have been summarized in Table 1. <br /> <br />9 <br />