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West Elk Mine <br />• data, the actual subsidence measurements and subsidence profiles predicted by the influence <br />function model compaze favorably. <br />Baseline subsidence measurements in the current West Elk Mine subsidence monitoring <br />area were selected such that subsidence parameters from longwall mining in the B Seam <br />were obtained with as little influence from prior room-and-pillar mining as possible. In <br />this way, the longwall mining subsidence parameters from the monitoring area could be <br />used to most accurately project longwall mining subsidence parameters into the SOD <br />mining area. The baseline subsidence measurements selected for both conceptual modeling <br />and computer modeling were October 1991, which was before B Seam longwall mining <br />began and after F Seam room-and-pillar mining was completed in the subsidence <br />monitoring network area. <br />Once the computer program was calibrated to the West Elk Mine subsidence data, subsidence was <br />projected into the SOD mining azeas using representative coal extraction thicknesses and <br />overburden depths for the respective panels in order to obtain an independent check on the <br />subsidence projections based on the conceptual model (Table 1 and Figure 7, Exhibit 60B). <br />Apache Rocky and Box Canvon Minin Areas -Comparison of the two models shows that <br />subsidence values above the chain pillars and panel centers of the computer model for the Apache <br />Rocks mining area aze approximately at the median point of the conceptual model data presented <br />for the eastern and western panels (Table 2 and Figures 7a and 76, Exhibit 60). Subsidence above <br />the chain pillars and panel centers for the Box Canyon mining area is also at about the median point <br />• of the conceptual model for the first four panels (Table 3 and Figure 7C, F_xhibit 60). <br />South of Divide Mining Area -Comparison of Mr. Dunrud's conceptual model calculations <br />and the influence function computer model of Peng and Luo (which were done by the <br />WWEs staff in Figures 7 and 8, Exhibit 60B) show the following: <br />1. Maximum vertical displacement (subsidence) above the chain pillars in the transverse <br />profile (Figure 7, Exhibit 60B) is close to the maximum values predicted in the <br />conceptual model calculations (0.8 to 4.2 feet). Maximum vertical displacement above <br />the longwall panel centers, however, is about equal to the median values projected in <br />the conceptual model calculations (4.8 to 11.2 feet). <br />2. The ranges calculated for vertical displacement in the conceptual model are <br />conservative. The ranges account for changing rapidly changing overburden thickness <br />in the local rugged terrain of the South of Divide mining area and for changing <br />lithology such as lenticular sandstones, coal seams, and shales in the overburden rocks. <br />Effects of Topography and Structure on Subsidence Processes <br />In contrast to subsidence of rock units behaving asfixed-end, laterally constrained, multiple <br />plates, subsidence in steep topography will typically occur as non-fixed end, laterally <br />unconstrained multiple plates (rock units). This lack of lateral confinement may locally cause <br />• reversals of horizontal displacement and excessive tensile strain on steep slopes. Peng and <br />Hsuing (1986) found that horizontal displacement is affected by slopes greater than 20 percent. <br />1.05-123 RevrsedNwember 2004 PRIO <br />