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<br />I <br /> <br />I <br /> <br />HYDROLOGIC AND HYDRAULIC DETERMINATIONS <br /> <br />I <br /> <br />History of Flooding <br /> <br />I <br /> <br />I <br /> <br />Flooding along Stone Creek has not been documented. It is likely, <br />however, that floods occured when Beaver Creek flows were particularly <br />high. Beaver Creek is an adjacent drainage basin, immediately to the <br />west of Stone Creek basin, with a drainage area of approximately 16 <br />square miles. A gage near its mouth recorded relatively high streamflows <br />during 1983, 1978, and 1984 (in order of magnitude) during its record <br />since 1974. All of these peak flows occured in the month of June. <br /> <br />I <br /> <br />I <br /> <br />Flood Characteristics <br /> <br />I <br /> <br />All of the highest peak flows in the adjacent basin of Beaver Creek <br />in its record of 1974-1984 occured during the month of June. This <br />indicates snowmelt ruhoff as the probable cause of the largest floods in <br />Stone Creek basin. <br /> <br />I <br /> <br />Hydrologic Analysis <br /> <br />I <br /> <br />The 100-year peak flow on Stone Creek was obtained through use of a <br />regional discharge versus drainage area curve for the Eagle River basin <br />area (Ref. 4). The regional curve was derived through a statistical <br />analysis of records of 18 streamflow gages in the Eagle County area as <br />well as other data. A 100-year peak flow of 250 cfs was calculated by <br />this method. <br /> <br />I <br /> <br />I <br /> <br />Peak flows for other recurrence intervals are also based on the regional <br />relationship curves. Estimated peak discharges for Stone Creek at the <br />mouth are summarized below. <br /> <br />I <br /> <br />I <br /> <br />Peak Flows for Stone Creek at its Mouth <br /> <br />I <br /> <br />Recurrence Interval <br />(years) <br />10 <br />50 <br />100 <br />500 <br /> <br />Peak Discharge <br />(cfs) <br />160 <br />205 <br />250 <br />420 <br /> <br />I <br /> <br />I <br /> <br />A plot of the frequency-discharge curve is shown in Figure 1. <br /> <br />I <br /> <br />It should be noted that the engineering consulting firm of KKBNA <br />(the engineer for the subdivision) had previously estimated a 100-year <br />peak flow of nearly 700 cfs in their drainage calculations for the Stone <br />Creek basin. An examination of the backup calculations deriving this <br />flow revealed a serious error in the estimation of one of the hydrologic <br />parameters. The effect of this error was that the re-routed channel was, <br />in most cases, oversized when it was designed. <br /> <br />I <br />