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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 />HYDROLOGY: <br />Montrose, Delta and Mesa Counties, Colorado <br /> <br />discharge index points on the study length were used. If not, the <br />average of the two endpoint flows was used throughout the study <br />length. Table 6 summarizes the 10-, 50-, 100- and 500-year flows <br />used. <br /> <br />Special consideration was given to Plateau Creek at Collbran <br />because of the presence of Vega Dam about 10 miles east of Collbran. <br />The dam has been regulating flow since 1958 when construction began <br />on it. Because of the lack of hydrologic data about the watershed <br />and hydraulic data about the reservoir and dam, a routing procedure <br />was not practical. Instead the gage station data before and after <br />the building of the dam was analysed to estimate the effects of its <br />regulation on the discharges at Col1bran. <br /> <br />The U.S.G.S. stream gage No. 09096500 was used in the analysis. The <br />gage is located approximately 6 miles east of Collbran and 2 miles <br />downstream of the Dam. The drainage area at the gage is 80.4 sq. <br />miles and the drainage area behind the dam is 24.4 sq. miles. The <br />gage data was divided into two groups. The first group includes <br />peak flows up to water year 1958 (unregulated flow) and the second <br />includes flows after 1958 (regulated). <br /> <br />The combined flood flow frequency curves for snowmelt and rainfall <br />were computed for both the unregulated and regulated conditions <br />(See Figure 45). <br /> <br />To find the discharges at Collbran (drainage area 113 sq. miles) <br />the regional flood-frequency study was used to compute the <br />unregulated discharges produced by the drainage basin between the <br />gage and Co11bran, and these flows were added to the regulated <br />discharges at the gage. To account for the time difference between <br />the peaks, the unregulated discharges produced by the 33 square <br />mile basin below the gage were not taken directly off the regional <br />frequency curves for a drainage area of 33 sq. miles. Instead the <br />differences in discharges computed for the entire basin (113 square <br />miles) and the gage (80.4 square miles) were used. Figure 47 <br />summarizes the calculations. <br /> <br />For Plateau Creek below the confluence with Buzzard Creek no flood <br />reduction due to Vega Dam regulation was considered because most of <br />that total watershed is unregulated (270 out of 295 sq. mile). <br /> <br />For comparison purposes flow discharges for key points were <br />computed using two published regional methods. Colorado Water <br />Conservation Board's Technical Manual #1 presents regression <br />equations for natural streams in four general areas of Colorado. A <br />summary of the method and calculations used for this report appears <br />in Figures 42-44. A second method from U.S.G.S. Water Supply Paper <br />1683 Magnitude and Frequency of Floods in the United States was <br /> <br />-7- <br />