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"D" Seam Longwall Subsidence Page 3 August 17, 1998 <br />• The conservatively predicted maximum, worst-case, trough <br />subsidence effects are presented in Table 1. The predictions may <br />be approached but will not be exceeded. Predicted maximum panel <br />group vertical subsidence ranges from 10.02-ft (Panels #10 - #12) <br />to 19.39-ft (Panels #7 - #9). Predicted maximum panel group <br />horizontal tensile strains at the ground surface range from 6385µe <br />(Panels #10 - #12) to 38970µe (Panels #7 - #9). The predicted <br />locations of these maximum tensile and compressive horizontal <br />strain lines are shown on Plates 6 - 10. Tensile strains on the <br />order of 39000µe will result in open fractures approximately 2-ft <br />in width at the ground surface, generally outside the horizontal <br />limits of the individual panel group. Predicted maximum horizontal <br />compressive strains range from 5010µe (Panels #10 - #12) to 30570µe <br />(Panels #7 - #9). Compressive strains of• the magnitude of 30500µe <br />will result in compression ridges being thrust up at the ground <br />surface approximately 250 feet inside the panel group boundaries <br />projected upward to the ground surface. These ridges will approach <br />a maximum height of approximately 1-ft above the subsided ground <br />surface trough. <br />A portion of a landslide area overlies the southwest corner of <br />planned Panel #3 (Plates 1 and 6) and the southeast corner of <br />planned Panel #4 (Plates 2 and 7). This landslide area was <br />identified on the Geologic Hazards Map for the North Fork of the <br />• Gunnison River by the W.R. Junge (1978). The predicted maximum <br />possible subsidence of the affected landslide area for those <br />longwall panel groups is shown on Plates 1 and 2. The affected <br />part of this landslide area will be tilted back into the slope by <br />the planned longwall mining, because mining starts at the north end <br />of each panel and proceeds toward the south. The overall stability <br />of the landslide mass should, therefore, be enhanced by the <br />subsidence accompanying longwall mining of Panels #3 and #4. <br />Some portion of all sixteen planned "D" Seam longwall panels <br />overlying abandoned "C2" Seam, "B" Seam and "B2" Seam room and <br />pillar mine workings, as indicated by the outline of the mine <br />workings shown on Plate 11. The underlying mine workings are <br />present over the shallower southern part of all the planned "D" <br />Seam longwall panels. Planned "D" Seam longwall mining in the <br />Sanborn Creek Mine should not be adversely impacted by either <br />chimney subsidence above room and pillar mine openings or stress <br />concentrations over barrier pillars in the underlying workings. <br />The interburden thickness should be sufficient to eliminate any <br />possibility of a collapse chimney connection between the underlying <br />room and pillar mining (Piggott ~ Eynon, 1977). The stress <br />concentrations above underlying barrier pillars should be laterally <br />distributed and, thereby, dissipated by the thickness of the <br />interburden and the high proportion of sandstone in the <br />• interburden, roughly 60~ (Chanda, 1989). <br />3 <br />