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perennial stream valleys, but under the steep hillslopes. <br />The applicant has submitted analyses of the coals, roof, and floor strata. The <br />analyses of the roof and floor materials performed by the Soils Laboratory of <br />Colorado State University (Appendix 3-I) indicate that these units contain <br />insufficient carbonate minerals to buffer the iron sulfide (e.g., pyrite) <br />contained in these strata. These analyses indicate that these strata are <br />acid-forming and potentially toxic. <br />The inactive North Thompson Creek No. 2 Mine contains both acid and toxic <br />mine waters (see laboratory analysis of Portal No. 2 Mine, dated June 22, <br />1982). This analysis shows that mine water in the No. 2 Mine exceeds <br />receiving stream standards for the following ions: aluminum, cadmium, <br />chloride, copper, iron, manganese, ammonia, sulfate, zinc, and total <br />dissolved solids. A tield measurement of pH by DMG staff obtained a pH <br />value of 2.5 for the No. 2 Mine water. It must be noted that this mine is <br />abandoned and "pre-law"; it is not proposed to be reopened or permitted <br />under this proposed decision. <br />During mining, water that collects in the mine has limited exposure to the <br />affected strata prior to discharge to the surface. Thus, there is little <br />degradation of water quality. However, upon completion of mining, there is <br />a potential for the formation of acidic and toxic mine waters. This <br />degradation of water quality would result from the prolonged exposure of <br />water to fractured roof strata and to the exposed coal and floor strata once the <br />mine pumps are shut off. <br />However, the water quality data for mine water discharges since the cessation <br />of pumping at the North Thompson Creek Mines demonstrates that the <br />discharge water has remained slightly alkaline. Elevated iron concentrations <br />in the mine discharge water are treated before the water is discharged to <br />North Thompson Creek. <br />Ground water quality in overlying and underlying aquifers may become <br />degraded upon closure of the mine through vertical communication of strata <br />caused by faults and fractures. The overlying and underlying aquifers are <br />currently not put to beneficial use and the potential for their future utilization <br />is limited by the difficulty in developing water wells in these strata. Owing to <br />these factors, the mines will not materially damage the ground water of any <br />water user through vertical migration of degraded mine waters. <br />The coal processing wastes from the wash plant are combustible, <br />acid-forming, and potentially toxic. Owing to the nature of these coal <br />processing wastes, the coal refuse pile was constructed to minimize exposure <br />of wastes to air, surface water, and ground water. The exposure to these <br />l6 <br />