Laserfiche WebLink
Chapter IV <br />topography. The potential aquifers have limited surface exposure. Recharge <br />effectiveness is further reduced because the recharge areas are well channeled to the <br />east and effectively sealed from above by shales and mudstones in the series. <br />Subsidence would not be expected to change the limited flow of ground water presently <br />flowing into the mines which is pumped to the surface, or which may enter the <br />sandstone occurring below the lower coal seam. There will be no diminution of aquifer <br />recharge caused by subsidence. (See Collins' study at Appendix IV -F -4). <br />3. Determination Statement of the Effects of <br />Subsidence, if it Did Occur, on Material <br />Damage or Diminution of Reasonably <br />Forseeable Use of Structures or Renewable <br />Resource Lands. <br />Mid - Continent believes that subsidence resulting from its mining operations in Coal <br />Basin over the next five year period is highly unlikely. Also, that if subsidence does <br />occur, based on a worst case hypothesis, there will be no material damage or <br />diminution of reasonably foreseeable use of structues or renewable resource lands. <br />Our field observations are that the nature of overlying strata is such that rock strengths <br />are adequate to withstand the gravitational stresses over great widths and tha the voids <br />created by the subsiding material are rapidly filled with overburden material which <br />increases in volume with sufficient strength to choke off subsidence before the surface <br />is breached. An extensive area of B Bed, nearly six miles along strike and one mile <br />downdip, has been mined 400 to 500 feet vertically below the Middle Bed. Total <br />amount of the cover above the B Bed should have generated subsidence effects in the <br />Middle Bed above the areas mined, but no subsidence has been detected therein. <br />There is no conceivable possibility that the Middle Bed area has subsided en toto <br />because no indications of such occurrence appear in the main drifts, development <br />entries, or on the ground surface in transition areas. The summary of opinion is that <br />subsidence will not reach the ground surface over the federal leased areas. This <br />opinion is derived from the historic factors cited and a comparison of probable <br />subsidence as illustrated: <br />Depth /Feet Subsidence Coal Bed <br />Ratio Thickness <br />Feet <br />2200 0.55 24 <br />2800 0.55 24 <br />32 <br />Maximum Percent of <br />Subsidence Depth <br />Feet <br />13.2 0.6 <br />13.2 0.47 <br />The normal bulking factor resulting from excavated rock is 35 to 50 percent before <br />compaction or settling. Therefore, a void of 24 feet would be filled and the supplying <br />