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• <br />6.3.3(1)(i) <br />Impacts to groundwater will be controlled by the recycling of leachate to the process stream, the sealing of joints <br />and fractures in bedrock by the clay content of the hydraulically classified waste stream, and the chemical control of <br />the process water quality as enumerated in 6.3.3(1)(m). <br />A stormwater management plan is created as follows for the construction and operations of the disposal site: <br />1. Construct sedimentation basin. <br />2. Construct earthen lined diversion ditches and connect natural diversion channels to sedimentation <br />basin. <br />3. Construct leachate collection barrier. <br />4. Rip-rap and/or vegetate tailings dam face using appropriate controls, i.e. jute netting and/or hydra <br />mulch using high-altitude roadside seed mix. <br />Temporary storm water management controls using silt fences and/or straw bales will be used during all phases of <br />excavation. <br />Hydrologic Data <br />Clear Creek is the significant surface water feature within 2 miles of the proposed facility; located 2 ,800' to the <br />south and 1,000' in elevation below the Tailings Impoundment affected area. <br />There are no perched zones or traditionally defined aquifers in this mountainous area. The site is completely <br />composed of crystalline Precambrian rocks, i.e. gneisses and schists, and tertiary intrusive rocks such as quartz <br />monzonites overlain by 0-24" of unconsolidated material. <br />Ground water wells within one mile of site boundary are detailed in a map attached at the end of this Exhibit C, <br />sourced from the Colorado Division of Water Resources. It shall also be noted that the groundwater in this area is <br />is unclassified per the Colorado Division of Water Resources. <br />Unconsolidated materials, soils, of between 0 and 18"-24" overlay the crystalline rocks. The rocks themselves have <br />essentially no porosity or permeability. Random, in-identifiable fractures due to jointing and faulting provide the <br />only groundwater transmissivity and relative porosity. The site is underlain by numerous mine openings, the most <br />important of which is the workings of the Shaffer Mine. The vein of the Shafter Mine outcrops within 100 yards of <br />the proposed disposal area, strikes N 40-600 W and dips 78-80° NW. The Shafter vein (along with the Great <br />American and Edgar) is cut by the Big Five Tunnel at 4,250 feet from the portal, and at a depth of 893 feet on the <br />dip of the vein. The mine workings effectively drain the area underneath the site. Refer to USGS Bulletin 1208, <br />Plate 3, Geologic Section Along the Big Five Tunnel Idaho Springs District. Colorado at the end of this Exhibit C. <br />Another example supporting this is the Colorado School of Mines Edgar Mine Facility (approx. 350' south of the <br />proposed Tailings Impoundment). After a meeting with than on August 31, 2009, it was learned that their mine is <br />"dry". So "dry" in fact that they are working on permitting a well on premises to supply a marginal water supply for <br />drilling operations to keep the dust down. The starting elevation of their well is 7,793' and the borehole was drilled <br />to-254'. Water was determined at -172'. This elevation, 7,621', just so happens to match the Big 5 Tunnel <br />elevation. Safe to say another example of the drainage in this area. A copy of this well log is attached in the <br />appendix of this Exhibit C. <br />Hydraulic conductivity for the undisturbed rock types present at the site, in-situ before mining, ranges from 10"2 - <br />10?2 gallons per day per square foot (as reported by Freeze and Cherry (1979)) due to joints and fractures in the <br />rock. These joints and fractures will be sealed with hydraulically applied clay that is part of the waste stream. The <br />existence of the underground mine workings provide a direct hydraulic conduit for groundwater beneath the site. <br />The Big Five tunnel, the major drainage for the area, lies 1,000 feet directly below the site. The Big Five Tunnel <br />drainage is monitored, collected, and pumped to the Argo Tunnel Treatment Facility located in Idaho Springs. It <br />produces on average, 35 gallons per minute. <br />According to the most current FEMA Flood Plain Map (reference FEMA Map #08019C0093D effective March 19, <br />• 2007) the proposed disposal site is in Zone X. Zone X is defined as follows: