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• be established will ultimately provide greater cover and erosion control than the native <br />pre-mine vegetation. <br />The Carbon Junction Mine will minimally impact both the quality and quantity of <br />ground and surface waters. A discussion of the probable hydrologic consequences of <br />mining is set forth below as well as in the CDMG findings document for the initial <br />approval of permit C-92-080. The CDMG discussion of probable hydrologic <br />consequences is incorporated by reference into this document. This discussion includes <br />a quantitative analysis of the impacts of the proposed operation on the existing ground <br />and surface water resources, both quantity and qua]ity impacts. <br />There are no regional aquifers that will be interrupted or impacted by the proposed <br />mining activity. Ground water in the area is found in discontinous lenses within <br />lenticular sandstones, fractures and in coal seams. Ground water analysis indicates that <br />the water found in the coal seams is of good quality and has no acid or toxic materials <br />in the analysis. <br />According to test data, little to no water will filtrate to the Pictured Cliff Sandstones, <br />and otherwise, the coals seams and perched water are expected to discharge to the <br />reclaimed pit. Overburden and refuse analysis indicate no acid or toxic materials aze <br />found in the materials. Sulfur materials in the refuse will be placed no less than 20 feet <br />• above the pit water level in reclamation although there is no available information <br />indicating the two to three percent (2 to 3%) sulfur in the reject is acid forming. <br />Regarding the concern for the lower Fruitland Formation and the Pictured Cliffs <br />Sandstone being a regional aquifer, the Division is referred to: Availabilityand <br />Chemical Characteristics of Groundwater in Central La Plata County. Colorado by <br />Robert E. Brogden and T.F. Giles, U. S. Geological Survey Water Resources <br />Investigations 76-69, prepared in cooperation with the Colorado Department of Natural <br />Resources, Division of Water Resources, Open File Report; Lakewood, Colorado; <br />May, 1976. This report maps the locations and summarizes water quality for 38 wells <br />in the Durango area. None of the wells investigated were completed in the referenced <br />formations. Additionally the formations are mentioned as potential aquifers, because <br />no wells completed in either formation could be ]orated by the authors. Mr. Carl <br />Hutchinson with the U.S.G.S. stated that the purpose of this open file report was to <br />supply the State Engineer with data on the various formations acting as aquifers <br />(personal communication February 6, 1983). The results of this report tend to confirm <br />the assertion that the Fruitland Formation and the Pictured Cliffs Sandstone are not <br />being utilized as aquifers in the Durango area (certainly not within 2 miles of the mine <br />site as State Engineer's well records indicate). Indeed, the basic premise that the <br />formations are aquifers in the Durango azea becomes suspect. <br /> <br />Technical Revision 08 (v 1.4) 5-33 Revised 9/1997 <br />