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<br />I <br />'f <br />II <br />: j <br />I <br />j <br />:- <br />j <br />\-1 <br />II <br />I <br />I <br />i1 <br />Ii <br /> <br />WATER SUPPLY ANALYSIS <br /> <br />11 <br />I: <br />I <br /> <br />The study was conducted by simulating future VVCWD water use patterns with <br /> <br />streamflow conditions representative of "wet", "normal". and "dry" water years. <br /> <br /> <br />This analysis concentrates on that portion of Gore Creek between its <br /> <br /> <br />confluences with Black Gore Creek and Red Sandstone Creek. The study <br /> <br /> <br />concentrates on this section of Gore Creek because: (1) this se~ent includes <br /> <br /> <br />the VVWCD snowmaking diversion, and (2) municipal diversions are physically <br /> <br /> <br />removed from the stream channel between the various raw-water intakes snd the <br /> <br /> <br />wastewater treatment plant at Red Sandstone Creek (see Figure 1). The <br /> <br /> <br />methodology used in completing the study required: (1) defining all possible <br /> <br /> <br />VVCWD diversion locations and subdividing them into groups corresponding to <br /> <br /> <br />stream sub-sections or reaches, (2) relating. future demand, return flow, stream <br /> <br />loss, and tributary inflow to each reach, and (3) combining all the above data <br /> <br /> <br />into a simple streamflow model to produce an estimate of streamflow depletion. <br /> <br />Water use data and diversion locations used in this analysis were obtained <br /> <br /> <br />primarily from VVCWD's application for water service from Green Mountain <br /> <br /> <br />Reservoir. Other data was obtained from Tipton and Kalmbach, Inc. of Denver, <br /> <br />consultants to the VVCWD. <br /> <br />;1; <br /> <br />Gore Creek Hydrology <br /> <br />,..~ <br />I <br />Iii <br />11 <br /> <br />Streamflow on Gore Creek exhibits characteristics similar to other high <br /> <br /> <br />elevation watershed.s in the Rocky Mountain Region. The flows are primarily <br /> <br /> <br />derived from snowmelt runoff which usually peaks in Mayor June. Historically, <br /> <br /> <br />the U. S. Geological Survev (USGS) has maintained several streamflow gaging <br /> <br />stations within the Gore Creek drainage bssin. Table 1 shows the statio.ns <br /> <br /> <br />which existed during the three study years (1970,1972,1977). The data from <br /> <br />chese stations was used to define flow conditions on Gore Creek. <br /> <br />r] <br />Ii <br /> <br />Five critical points on Gore Creek were selected for streamflow analysis. <br /> <br /> <br />The positions of the points correspond to a former gaging station location, <br /> <br />points just upstream of significant tributary stream confluences, and a poirit <br /> <br /> <br />at the lower end of the critical segment. Figure 1 illustrates these five <br /> <br />points. Point A corresponds to the location of the USGS station on Gore Creek <br /> <br />at Vail (No. 09066250). Table 1 shows that data for this station is available <br /> <br />'i <br />I; <br />t <br /> <br />1 <br /> <br />I <br /> <br />-3- <br />