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Linda J. Bassi April 29, 2008 <br />Page 3 <br />The actual start and finish dates and hours of pumping forsnowmaking operations would <br />vary from year to year depending upon when air temperatures become consistently cold <br />enough for snowmaking operations. Under optimal conditions, allowing well pumping to <br />occur for 10 hours per day, the desired snowmaking would be completed in a period of <br />about 36 days. Under normal operating conditions, it is likely that there will be <br />intermittent 1 to 3 day periods of sub-optimal conditions when no pumping would occur, <br />allowing the streamflow to recover to near natural conditions. As described below under <br />the Hydrologic Analysis, the potential reduction to the ISF would fluctuate from <br />approximately 0.009 cfs to 0.019 cfs, which would result in a 2% to 4% reduction of the <br />estimated dry year natural flow in Two Elk Creek below the Tea Cup Bowl Well at the <br />upperterminus of the CWCB 4 mile ISF reach. <br />The one acre-foot of water pumped from the Tea Cup Bowl Well is assumed to be 100% <br />consumptive to Two Elk Creek and the Eagle River at the time of diversion, with 80% of <br />the snowmaking diversions returning to Two Elk Creek and the Eagle River during the <br />ensuing spring and summer. During winter snowmaking operations, it is expected that <br />there will be a small amount of return flows to Two Elk Creek, which are not included in <br />this analysis. <br />Hydrologic analysis showing why full ISF protection is not possible <br />Based upon an evaluation of alternative water supply sources for snowmaking at the <br />base area around the Tea Cup and Skyline Express Lifts, it was determined that the <br />development of an alluvial well, tributary to Two Elk Creek, would be the most practical <br />and environmentally sound option. The potential hydrologic impacts of the proposed use <br />of the Tea Cup Bowl Well for snowmaking were evaluated using the Glover Parallel <br />Drain Analytical Solution of Groundwater Returns (Glover 1977). The Glover method <br />determines stream depletions from well pumping in an idealized stream-aquifer system. <br />The Parallel Drain method provides a mathematical solution for the stream depletion <br />pattern as a percentage of the pumping rate. The result of the Glover approach is a <br />daily time series of the depletive effect of well pumping on Two Elk Creek. <br />streamflows in Two Elk Creek were estimated based upon correlation with measured <br />flows in Wearyman Creek at the gauging station (USGS 09063200 Wearyman Creek <br />near Red Cliff, CO) for the period of record 1964 through 2005. Low-flow conditions <br />were then adjusted based upon several actual Two Elk Creek flow measurements <br />conducted in January of 2007. <br />Data required to use this method include the boundaries of the alluvial aquifer, the <br />saturated thickness, hydraulic conductivity, and aquifer specific yield. The boundaries of <br />the alluvial aquifer can be roughly estimated based upon topographic mapping of the <br />area. Because there are no other known wells in the Two Elk watershed, there are no <br />boring logs available that would provide site-specific information regarding the <br />characteristics of the aquifer and the alluvium. Based upon well completion reports for <br />wells in the Gore Creek and Eagle River alluvium and geologic mapping of the area, <br />reasonable ranges of conditions that are likely to be present in the vicinity of the <br />proposed well site can be estimated. <br />Well pumping would result in a small reduction to streamflows in Two Elk Creek. The <br />impact on streamflows in Two Elk Creek during continuous well pumping would increase <br />AMEC Earth and Environmental, Inc. <br />