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be decreased by as much as the maximum subsidence-induced tilt <br />change. See Figures 9B. <br />3. Horizontal tensile strain values generally greater than approximately 1 <br />percent (10000 us) at 500-foot overburden depths and less also may <br />accelerate natural landslide movement or rockfall, particularly during <br />periods of high or increased precipitation. Figure 18. Ribside Tension <br />Cracks in Road Fill and Cliff Face, York Canyon Mine shows a <br />location where a sandstone cliff face failed after some of the shale <br />underlying a sandstone cliff face had been removed for the pioneer road <br />and then the headgate end of the longwall panel was mined past at <br />approximately 360 feet below but over 50 feet to the right of the cliff. The <br />estimated non-maximum tensile strain acting on the cliff face was about <br />0.5 percent (5000 us). <br />8.2 Mining Beneath Stream Courses <br />The only permanent stream courses indicated on the Garvey Canyon Quadrangle and <br />Howard Canyon Quadrangle for the Project Area are Big Salt Wash and East Salt <br />Creek. Big Salt Wash is the only perennial stream that overlies planned Red Cliff Mine <br />workings in the Cameo Seam. East Salt Creek does not cross over any part of the <br />Cameo Seam within the Existing Coal Lease or Coal Lease Application area. The <br />Cameo Seam outcrop crosses Big Salt Wash approximately 7,800 feet upstream from <br />the southern boundary of the Coal Lease Application area, as shown on Figure 13. <br />Overburden and Outcrop Map for the Project Area. <br />Within the Existing Coal Lease area, the Cameo Seam outcrop crosses the intermittent <br />stream course in Stove Canyon, Section 2, T. 8 S., R102 W. northwest of Big Salt Wash <br />and the intermittent stream courses in Munger Canyon and its southeast tributary, <br />Sections 22 and 27, S. 7 S., R. 102 W. These Cameo Seam outcrops are within the <br />Project Area. <br />Within the Coal Lease Application area the Cameo Seam outcrop crosses the <br />intermittent stream course in Buniger Canyon approximately 4,500 feet upstream from <br />where it meets the perennial stream in Big Salt Wash. <br />In order to mitigate potential subsidence impacts in the Coal Lease Application area and <br />the immediately adjacent north, east and south parts of the Project Area, it was <br />necessary to have a conceptual mining plan. The goals of the conceptual plan were to <br />maximize safety, then mitigate to the extent possible subsidence impacts and finally to <br />maximize resource recovery. The proposed portal is the anchor for the concept. The <br />conceptual plan that follows involves at least two sets of east-west mains driven off the <br />Big Salt Wash mains. A bleeder entry may well be necessary along the south boundary <br />of the Project Area. Either a bleeder entry or a third set of mains would probably be <br />required along the northern boundary of the Project Area. <br />It will be necessary to drive the main access entries approximately 5,000 feet N 45° E <br />from the planned Red Cliff Mine portal to where it will cross under the overlying <br />intermittent stream course in Stove Canyon at a depth of less than 200 feet., The main <br />entries will probably continue to a distance of approximately 9,000 feet where it will cross <br />beneath the intermittent stream course in Buniger Canyon at a depth of slightly less than <br />C-40 <br />DBMS 332 <br />