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<br /> <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 />basins governed by flash flooding events due to short periods of intense rainfall, as seen along <br />the Colorado Front Range. <br /> <br />Table 2.2 <br /> <br />Elk River Watershed Drainage Areas <br /> <br />ELK RIVER BANK STABILIZATION -ICON PROJECT NO. 99-041-ELK-415 <br />HYDROLOGY - ELK RIVER WATERSHED <br /> <br />BASIN DA % Total Comments % Watershed <br /> sq.mi in Park Range <br />Mad Creek 40,1 9 Park Range <br />Big Creek 40,5 10 Park Range <br />S, Fork Elk 33.9 8 Park Range <br />M, Fork Elk 20,8 5 Park Range <br />N, Fork Elk 40,5 10 Park Range 41 <br />Hinman/Coulton Creeks 23.5 6 <br />Willow Creek 72,8 17 <br />Sand Creek/Cottonwood Gulch 27,3 6 <br />Deep Creek/Long Gulch 55,7 13 <br />Salt Creek 16,7 4 <br />Farnsworth Creek/Dry Gulch Areas 29.4 7 <br />Mise, Areas along Mainstem 23,5 6 <br />Steamboat Lake" 35,7 8 <br />Total Elk River Watershed 424.7 100 <br /> <br />'Areas from USGS 30x60 Minute Series <br />"Area included in Willow Creek Drainage Area <br /> <br />Estimating the percentage of average basin runoff that ongmates in the Park Range was <br />performed as a part of this study, In 1990, W, P. Stanton presented information relating the <br />mean logarithm of peak flows from snow to both basin area and mean watershed elevation for <br />both the Upper San Juan River and St. Vrain Creek basins, Assuming that a regression analysis <br />for the Elk River basin would result in a similar relationship for peak flows from snow, an <br />effort was made to determine the percentage of runoff from the Park Range based on both basin <br />area and mean watershed elevation. . <br /> <br />Mean watershed elevations for both the Elk River watershed and the combined watersheds <br />having headwaters in the Park Range were estimated from the 30 x 60-minute quadrangle <br />mapping (USGS), Results indicated that the mean watershed elevations are similar, therefore. <br />the peak discharges would be proportional to the basin areas, Since the combined watershed <br />area originating in the Park Range makes up approximately 4 I percent of the total drainage <br />area for the Elk River basin, it is estimated that approximately 41 percent of the average basin <br />runoff would also originate in this portion of the watershed, This estimation also assumes a <br />uniform snowfall distribution over the entire watershed, A copy of the supporting information <br />is included in Appendix B, <br /> <br />7 <br />