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f': (~ <br />during the winter of 1976-77, water year 1!377 was a dry year. Using <br />the data from Junes 1977 - April 1978 as an indication of 1977 water <br />year conditions, vre have plotted high, low and estimated mean annual . <br />runoff in cornpari<.;on with drainage area on Figure 1. Only the <br />drainage area above the gaging station is plotted in Figure 1. <br />From Figure 1 it is apparent that the percentage of water contribution <br />by basin cannot bey determined solely on the basis of basin areas. On <br />a unit area basis, water yields from South Prang and Horse Creek <rre <br />much higher than water yields from either Lick Creek or Dry Fork. <br />Percentage contrit~ution by basin are best approximat~:d from the mEaan <br />annual runoff estimates given previously. Once the Lower East Fork <br />gaging station is installed, we will be able to better quantify the <br />percentage water <:ontribution by basin for i4innesota Creek above t:he <br />1linnesota and Turner Ditch diversions. The degree of accuracy <br />achievable will depend upon our ability to assess the effects of lone <br />Cabin Ditch and Beaver Dam Ditch on the flow recorded at the East Fork <br />gaging station. <br />South Prong and Horse Creek have higher yields than either Dry Fork or <br />Lick Creek. Flow variation for Dry Fork is affected by storage and <br />release from i4inne~sota Reservoir. Also, Dry Fork flows include Detep <br />Creek Ditch which is not included in the drainage area of Dry Fork. <br />The other surface water bodies associated with the Mt. Gunnison I•t•ine <br />permit area are I~linnesota and Beaver Reservoirs. Both reservoirs are <br />located below the outcrop of the F seam coal and consequently will not <br />be directly affected by mining. <br />Springs located on the mine permit area play a minor role in main- <br />taining low flows. In fact, most springs dry up early during the <br />summer and streamer originating on the permit area are ephemeral. This <br />indicates that groundwater supplying springs is of limited extent. <br />Also, the discharge rates of the springs respond closely to preci;rita- <br />tion events indicz~ting that the recharge areas for the springs are <br /> <br />~4) <br />