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<br />Probable Hydrologic Consequences-Groundeater <br />The eater table in the permit area and adjacent area Correlates directly co <br />the elevation of the Colorado River. Rock formations and alluvium below the <br />level of the river are recharged by the Colorado River and have piezometric <br />levels equal to that of the rivet at the recharge zone. <br />Three stratigraphic units may be defined as aquifers and each transmits water <br />to or is recharged by, the river. The first unit is the strata overiyi~ the <br />coal seam. This unit consists of interbedded sandstones and shales of dis- <br />continuous lateral extent. The stratigraphy of this unit indicates that the <br />strata overlying the coal zone behaves as a single hydraulic unit containing <br />localized perched aquifers recharged by the river in some areas. Ground eater <br />move slowly through and between interconnected sandstone and shale leases and <br />beds. <br />The second unit is the Cameo coal seam. The coal seam receives recharge eater <br />from the river where the seam dips below the river at an elevation of 4750 <br />feet within the Cameo Hine. The 114 feet thick Rollins Sandstone formation is <br />the thickest and most continuous sandstone in the project area. <br />The Rollins Sandstone is the third eater-bearing unit and constitutes the best <br />potential aquifer in the region. The Rollins Sandstone underlies the entire <br />permit area, except within De beaus Canyon, where it outcrops. Recharge to the <br />Rollins Sandstone occurs primarily is the subcrops below the alluvium of the <br />•, Colorado River. <br />Ia addition to the above, the alluvial deposits of the Colorado River flood <br />plain may also be classified as an aquifer. The alluvium contains eater from <br />the river and recharges eater to permeable units beneath it. <br />The strata in the Roadside `Sine plan area dips towards the Colorado River, <br />whereas the strata is the Cameo mine plan area dips away from the Colorado <br />River. The ground eater from the Roadside mine plan area located strati- <br />graphically higher than the Colorado River will discharge into the Colorado <br />River, whereas the Colorado River will recharge the strata located strati- <br />graphically lover than the Colorado River system in the Cameo Mine plan <br />axe a. The company will have to submit evidence that adequate water rights <br />have been secured to replace the valet that is lost from the Colorado River <br />prior to mine closure. <br />The major effect of mining on the quality of eater is an increase in the sol- <br />uble saltwater levels. The mine discharge eater has roughly a 3-4 fold higher <br />content of soluble salts than the Colorado River. These discharges are di- <br />luted by receiving eaters, resulting in a total Increase in the soluble salt <br />level of the river by O.1S the underground disposal of coal processing waste <br />at the Roadside mine should have an insignificant effect on ground eater <br />quality, since it is similar in nature to the material presently exposed in <br />the xiae. The water used to transport the waste material into the abandoned <br />underground vork'_ags -.rill be drained and reused, and except for loss, this <br />eater should have an insignificant effect '_n around eater. <br />-~- <br />