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transmissivity and storativity appear to be quite low due to the highly lenticular and <br />discontinuous nature of the Mesaverde Group. It is thought that transmissivity and <br />storativity values will be variable over large areas. <br />Two wells remain that aze monitored for water level, S10-WC and S15-WC, both of <br />which are up-gradient of the mining operation. Water in both these wells retained a <br />relatively uniform level throughout the early yeazs of mine life. S10-WC level <br />varied around 79 feet below ground surface (bgs). After 1989, the levels have <br />dropped and appear to have stabilized around 83 feet bgs. S15-WC levels varied <br />around 80 feet bgs until 1993, at which time levels have been erratic, ranging from <br />84 feet bgs to 108 feet bgs. <br />Wells S35-WC and S37-WC were used to monitor water levels until 1996, but have <br />been abandoned. <br />Historic data show that water in the Wolf Creek Coal is a calcium sulfate type with <br />an average TDS of 745 mg/1. <br />Wadge Coal and Overburden <br />The Wadge Overburden is considered to be an aquifer in this area and for purposes <br />of this discussion, is collectively grouped with the Wadge Coal aquifer. Four wells <br />monitor [he Wadge Coal seam and overburden, and two of [he wells are in hydraulic <br />communication with the Wadge Impoundment. Three wells remain in what is <br />referred to as the Wadge Lennox interburden. These wells exhibit normal seasonal <br />variations. <br />Aquifer tests performed in the Wadge Coal seam indicate that the Wadge aquifer <br />exhibits asemi-confined condition with a transmissivi[y value of 377.1 gallons per <br />day per foot (gpd/ft). W adge water levels, dependent upon well proximity to the <br />rechazge area, show some seasonal variation. <br />Alluvium <br />There are three alluvial aquifer systems within the Seneca II permit area: the Grassy <br />Creek alluvial aquifer, the Cow Camp Creek alluvial aquifer system (drainage from <br />below 004 pond to Fish Creek), and the Bond Creek alluvial aquifer (drainage from <br />below 008 pond to Fish Creek). The Fish Creek alluvial aquifer is not within the <br />Seneca II permit azea, but may be affected by water discharging from the permit <br />area. <br />zz <br />