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Rule Z: Permits <br />• (3) Protection of the Hydrologic Balance <br />In accordance with Rule 2.05.6, a plan for the protection ofthe hydrologic balance must be prepared for <br />the project. In addition, this plan must considerthe effects to the quality and quantity ofsurface and ground <br />water. Baseline data for the surface and ground water is provided in Exhibit Section 2.04.7. This data is <br />the basis for the analyses of the probable effects from the Lorencito Canyon Mine. <br />Water Quantity <br />Effects to water quantity were considered for both ground and surface waters in the permit azea. From the <br />data presented in the surface and ground water reports, the quantities ofwater available at the site appeaz <br />to be limited. Data developed from slug testing indicated relatively low hydraulic conductivities (] 0~' ft/day), <br />and therefore, relatively low pumping rates from wells at the site. Surface water baseline monitoring <br />revealed only two stations (LC-1 and LC-4) that had water throughout the yeaz. In general, the only <br />natural perennial surface water appears to be from springs, which will not be affected by mining operations. <br />Surface water runofffrom disturbed areas will pass through sediment ponds to remove solids, resulting in <br />nominal losses of downstream flow or water quality. <br />GROUND WATER <br />• Mining in the Ciruela coal is topographically higher (approximately 7200 AMSL) than any of the alluvial <br />deposits onsite and wi II not affect these deposits. Ground water in the overburden ofthe Ciruela is also <br />extremely limited and is not in use overthe projected mining areas. Groundwater in the Ciruela itself is not <br />being utilized currently at the site, and is also extremely limited in areal extent. The ground water in the <br />Primero Coal is also topographically isolated (approximately 6800 AMSL) from the Purgatoire River, and <br />does outcrop south of the river. The Primero coal does exist under Lorencito Creek and will be mined in <br />the vicinity of this creek. Between these two tazget coals is a layer ofinterburden material (approximately <br />400-500 feet thick). This material has low hydraulic conductivity and could be considered an aquitazd. <br />Beneath the Primero exists an underburden material that is also considered as a material with a fairly low <br />hydraulic conductivity (see section 2.04.7). Use ofall these water-bearing zones is very li mited, and only <br />a small number ofwindmills were located on and in the vicinity ofthe permit azea. Surface mining is not <br />anticipated to have significant effects on those zones in relation to water quality or quantity, due to the <br />azea's limited extent. Also, no backfill springs or seeps aze anticipated from the mine areas. <br />Contour Mining Cuts and Fitfs <br />At the Lorencito Canyon contour mines, materials will be removed from the coutcrop until a removal ratio <br />of approximately 12:1 exists. Following this removal, the overburden will be replaced to original <br />approximate topographic grade is restored. As partof this process, some fills will be created. Mining. <br />proposed for Lorencito Canyon contour mines will not extend disturbance above an altitude of7,000 feet <br />• <br />~~,~1 <br />2.05-83b (revised 08/30/01) <br />