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IRIS <br />MITIGATION AND DESIGN, INC. <br />SCHWARTZWALDER MINE PHASE 1 - UPSTREAM CUTOFF WALL AND LOW FLOW BYPASS <br />PIPELINE - BIOLOGICAL ASSESSMENT <br />include the continued use of an irrigation system to sustain riparian vegetation surrounding Ralston <br />Creek. <br />Phase 3: Characterization and Long -term Reclamation — Phase 3 of the Project will include further <br />Site characterization, which will allow Cotter to develop and implement a long -term, sustainable <br />reclamation plan for the Site. The long -term plan will include returning flows to Ralston Creek and <br />creation of required mitigation. Since the characterization and reclamation activities would be very <br />difficult to complete until the Site is substantially dewatered, many of the details of Phase 3 have not <br />yet been determined. <br />1.3 Schwartzwalder Mine History <br />During active mining operations dating back to the 1950's, Ralston Creek was displaced from its <br />historic, meandering alignment to the north side of the valley to accommodate mining activities on the <br />Site. The Site was an active uranium mine between 1953 and 2000. Between 1966 and 2000 the <br />mine was owned and operated by Cotter. After 2000, active mining operations ceased on the Site; <br />however, the Site remains under Cotter's ownership. Based on geologic evaluations described in the <br />EPP, the alluvial material at the Site and adjacent to Ralston Creek varies in depth from 0 to 36 feet. <br />The alluvial material generally is composed of sand to cobble size material. Groundwater flows in the <br />alluvium from northwest to southeast across the Site, generally following the Ralston Creek riparian <br />corridor alignment. A strong hydrologic connection exists between the creek and the alluvium, <br />especially in the vicinity of the Alluvial Fill Area below the WVVfP, creating the potential for up- gradient <br />water in Ralston Creek to come into contact with materials in the Alluvial Fill Area, resulting in <br />mobilization of uranium. <br />The Site has a water treatment system which includes sumps which collect and pump alluvial <br />groundwater from the Site back to a WWTP to remove uranium before it is discharged to Ralston <br />Creek near the downstream property boundary. <br />The cutoff wall and low flow bypass pipeline will prevent up- gradient flows up to 8 cfs from coming into <br />contact with areas of potential contamination on the Site. Based on hydrology data presented in the <br />EPP, the low flow bypass pipeline would be expected to divert all or most of the flow in the creek from <br />July through March. Cotter anticipates using the low flow bypass pipeline as the primary diversion <br />method for 1 to 2 years while the Phase 2 Temporary Diversion Pipeline (100 cfs) is designed, <br />permitted and constructed to allow for clean -up and reclamation of the Site in Phase 3. The low flow <br />Page 3 August 2011 <br />