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2. 04 . 7 Hydrology Description <br /> 1. Comment Regional cross-sections should be provided <br /> showing the depth of the alluvial, Pleistocene basalt, <br /> Wasatch, and Mesaverde aquifers below the ground surface. <br /> Site-specific cross-sections should be provided showing <br /> the depth of the alluvial and Mesaverde aquifers below <br /> the ground surface. A map should be provided showing <br /> the location and horizontal extent of the alluvial <br /> aquifers. <br /> Reply Site specific cross-sections and maps showing <br /> the location and horizontal extent of the alluvial <br /> aquifer have been prepared by Willard-Owens and are <br /> included as Exhibits to Section D of Chapter III . <br /> Vol. 5, Chap. III, Sec. D, (Add as Exhibits III- <br /> D-3 (a-c) . <br /> 2. Comment The text mentions one well in the Mesaverde <br /> Formation, p. 21, appendix III-E-1. The location and <br /> use of this well should be provided, and the particular <br /> aquifer unit used in the Mesaverde Formation should be <br /> identified. The uses of the wells in the East Muddy <br /> Creek alluvium should be identified. <br /> Reply Add Willard-Owens explanation (attached) as <br /> referenced below. <br /> Vol. 5, Appendix III-E-1 (Add new information as <br /> Pages 21.1 & 26 . 1 of the ground water section of <br /> the Willard Owens Hydrologic report) <br /> 3. Comment The applicant did not provide any samples of <br /> water quality data for the Mesaverde aquifer and is <br /> lacking recent water quality samples for the Coal Creek <br /> alluvium (only three samples from 1974 were provided) . <br /> The information on water quality data for the Mesaverde <br /> aquifer and Coal Creek alluvium does not provide enough <br /> detail to extrapolate what effects will occur from the <br /> mining operations . Baseline water quality data must be <br /> submitted. <br /> Reply Add Willard-Owens comment (attached) together <br /> with the following Mid-Continent comment to page 21 .1 <br /> of Appendix III-E-1: <br /> There is no doubt in our minds that the Coal Creek <br /> alluvium is shallow, steep and resurfaces many times in <br /> Coal Basin. We believe the water quality of the surface <br /> flows are the same as the alluvium. We have six years <br /> of surface water quality data. We also now have more <br /> ground water quality data (Oct. 80, Jan. 81 and April <br /> 81)which we have included in Appendix III-E-2. <br />