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proximity to the shop /office and its human activity. Daylight raptors <br />have been seen migrating through the permit area, but are only <br />occasionally observed perched on fence posts or power poles. <br />E. Coors seeding plan is filed in L -4. It is hoped that this seed mix will <br />improve both the domestic and wildlife range habitat. (See letters on <br />pages 129 and 129a of this Section.) See also Section 2.04.11, Fish <br />and Wildlife Resource Information. <br />Protection of Hydrologic Balance <br />Detailed descriptions, maps and cross - sectional drawings regarding the <br />quality and quantity of surface and subsurface water at the Keenesburg <br />Mine is summarized in Section 2.04.7, Hydrological Description, and at <br />Appendix I of previous permit submittals. The focus of this permit <br />renewal (five year plan) is on reclamation, to the exclusion of further <br />mining operations. The previous mine pits ( "A" and `B ") have both been <br />reclaimed to at least five feet above the ground water level, and are lined <br />with the clay spoils to create an impervious barrier between the ground <br />water and the ash/mine waste rock which is being deposited in those pits. <br />The sub - surface water gradient, to the extent that it exists in the spoil, still <br />. tends to slope to the east. Recharge of the spoil aquifer appears now to be <br />limited to a single source, infiltration by precipitation, since the pit areas <br />have been isolated and any standing water cannot communicate to the sub- <br />surface water interval. There is still no indication that any significant <br />recharge from the Ennis Draw fluvial ground water system exists. Sub- <br />surface water elevations in the wells existing in Ennis Draw, adjacent to <br />the Keenesburg Mine site, are significantly higher than in either spoil <br />monitoring well, as confirmed by both Appendix I -2 of previous permit <br />submittals and the more recent data found in the Annual Hydrology and <br />Reclamation Reports. The lack of recharge of the spoil aquifer system by <br />the subsurface waters in Ennis Draw is thought to be the result of limiting <br />the eastern extent of the mining operation (not penetrating the area of <br />Ennis Draw itself). <br />No appreciable effect on the hydrologic balance of the area is anticipated <br />as a result of the mining and/or reclamation operations, and water levels in <br />the mined area are expected to eventually recover to approximately their <br />original levels following the cessation of mining operations (McWhorter). <br />Water quality information gathered over the past 12 years confirms this <br />(see Appendix J -1, J -2 of the 2 nd Permit Renewal, and the Annual <br />Hydrology and Reclamation Reports. Treatment of the sub - surface and <br />ground water will not be necessary. <br />Appendix M -1, Existing Surface Features Map, shows the location of any <br />significant water diversion, collection, conveyance, storage and discharge <br />structures (these include the perimeter ditches, the Dugout Pond and <br />125 <br />11 /10 <br />Nib <br />