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<br />1 <br />LJ <br /> <br />1 <br /> <br /> <br /> <br />r <br />LJ <br />[1 <br /> <br /> <br /> <br /> <br />1 <br />r <br />5.0 POST MINING HYDROLOGIC CONDITIONS <br />The hydrogeologic characteristics of the Orchard Valley mine <br />where the coal seams and the sandstone strata are outcropping and <br />dipping out of the valley assure that the abandoned mine will not <br />be discharging water. This is confirmed by water level <br />measurements in the Farmer's mine, in all deep monitoring wells <br />within the permit area and by general development of the <br />potentiometric surface in the deep water bearing strata. <br />After abandonment of the Orchard Valley mine the water will <br />be seeping slowly into the mine and filling the mine to an <br />elevation of approximately 7,100 feet. At the time of mine <br />abandonment the mined out volume will be more than 300 million <br />cubic feet. The mine flooding will be very slow and it would <br />take approximately 130 years to fill the mine to an elevation of <br />7,100 feet with only natural inflow. The mine flooding would be <br />substantially faster if an out-of-mine source of water is used to <br />fill the mine. With an addition of 38.0 gpm available at the CWI <br />well field in Stevens Gulch, the mine filling will be reduced to <br />approximately 61 years. <br />The mine flooding could be altered by the following <br />measures: <br />o commencement of flooding of particular mine <br />sectors during the mine life; <br />o intensified flooding of selected sectors of <br />the mine sealed from the other parts of the <br />mine. <br />Mine flooding will be discussed with the regulatory agencies <br />before the mine abandonment and more detailed flooding plans will <br />be prepared. <br />The time necessary for the filling of particular sectors of <br />the Orchard Valley mine with only natural and natural and <br />artificial sources is expressed in the following table. <br />' I I 11 inuia~.r.r:u Cu~Si cn~T. <br />