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facilities. Quarterly total dissolved solids monitoring is still required. <br /> Mine discharge from the Roadside Mines were estimated to increase soluble salts <br /> in the river by 0.1 percent and dissolved iron by 0.2 percent(November 4, 1982 <br /> DMG Findings Document). These predictions have proven to be accurate to <br /> date. <br /> In its 1982 Findings,the Division also predicted that water quality effects would <br /> be "minimal and will not significantly decrease water quality in the Colorado <br /> River." Surface and groundwater monitoring to date have supported these <br /> projections. <br /> Water monitoring conducted by the operator since 1982 has not identified any <br /> unanticipated effects on river water quality. Mine water discharges from <br /> approved CDPS points will continue to be analyzed annually for the list of <br /> parameters in Table 18-2 of the permit. <br /> 2. Surface water runoff from disturbed areas on the mine site previously passed <br /> through sediment ponds, with the exception of the small areas discussed in <br /> Section C.II. A. of this document. Discharges from these ponds historically met <br /> effluent limits in the mines' CDPS permit except for discharges related to severe <br /> storm events. Effects on water quality due to disturbed-area runoff have been <br /> and should continue to be insignificant. All ponds have been reclaimed and have <br /> met the criteria for Phase II Bond Release. Reclaimed areas have demonstrated <br /> that they do not contribute additional sediment to the river. <br /> Groundwater <br /> Groundwater Quality <br /> Four hydrologic units have been identified as aquifers that may be effected by the <br /> mining operation. These are: Colorado River alluvium, strata overlying the Cameo <br /> coal seams, Cameo coal seams, and the Rollins sandstone unit. Each of these will be <br /> addressed below as to the mines'probable hydrologic impact. <br /> Colorado River Alluvium <br /> The Colorado River alluvium consists of silty sand intermixed with gravel along the <br /> canyon and mine facility site. The alluvium varies between 0 and 60 feet in thickness <br /> and has a hydraulic conductivity of 0.01 cm2. The main concern with the alluvial <br /> aquifer is the total dissolved salt(TDS) content that mining contributes to the stream <br /> flow. The diminished quality of water discharged from the mine due to salt and <br /> sediment loading is improved somewhat by allowing the water to settle out the solids. <br /> The discharged mine water is given sufficient time to allow gravity to settle the solids <br /> before discharge occurs to the Colorado River. Three NPDES points discharged the <br /> mine water during active operations (Nos. 001, 002 and 004) and were subject to <br /> 34 <br />