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<br />Somerset Mining Company <br />' 1994 Annual Hydrologic Report <br />area below Old Highway 133. No flow was recorded for Spring 11 in <br />1992 and 1993. In May of 1994, water began to collect in the road <br />cut above Old Highway 133. This was monitored and an elevated <br />conductivity and temperature was measured. Flow was recorded in <br />June and July, but the conductivity and temperature measurements <br />' decreased. Water damage to the pavement of Old Highway 133 had <br />occurred next to the re-emergence of Spring 11, and between the <br />July and August monitoring events, the Colorado Department of <br />' Transportation performed maintenance of the roadway and ditch in <br />the area of Springs 10 & 11. Both Springs 10 and 11 were dry at <br />the time of the August monitoring, with re-emergence of Spring 10 <br />by October and Spring 11 by December. Roadway maintenance impacts <br />' to Springs 10 and 11 by the Colorado Department of Transportation <br />are beyond the control of Somerset Mining Company. <br />The source of all springs, except Spring 6, is precipitation or <br />snowmelt. This water infiltrates and percolates downward until the <br />water encounters a coarse zone or aquiclude which causes the water <br />to surface as a spring. The primary use of the springs is by <br />wildlife. The only spring to consistently contribute to surface <br />flow into the North Fork of the Gunnison is Spring 8. All other <br />spring surface flow, if any, returns to the ground before reaching <br />' the North Fork of the Gunnison. <br />Springs 1 through 7 are accessible from the Coal Gulch trail, a <br />' rough, rocky, steep primitive road. Primary means of <br />transportation to the area is by four-wheel-drive Jeep, ATV, <br />horseback, and foot. Although the trail is public access, it is <br />not maintained. Other users of the trail include hunters, <br />' livestock grazers, and the government. Springs 8 through 11 are <br />located along Old Highway 133 and are readily accessible by normal <br />transportation. <br />' Springs 1 through 6 were monitored April through October. SMC <br />personnel use an ATV to access the spring sites. Springs 7 through <br />' 11 were monitored monthly, although access to Spring 7 during <br />January, February, and December required foot travel through snow <br />and ice conditions and during November required foot travel through <br />the mud. The sample point for Spring 8, the Oliver Mine, was <br />' located at the north end of a culvert in place under Old Highway <br />133. It was frozen and snow covered during both times sampling was <br />attempted during January and February. As a result of Notice of <br />' Violation C-94-007, Spring 8 was monitored at the south (discharge) <br />end of the culvert, which required breaking through the ice to <br />obtain a sample in December. This slight change in monitoring <br />' location probably resulted in the lower temperature measurements <br />for November and December compared to the historical data. <br />' 12 <br />