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Affected Environment and Environmental Consequences <br />Chapter 3 <br />BLM estimates that the coal in the Dry Fork tract <br />averages about of 11,700 BTUs, has an average <br />sulfur content of about 0.5 percent, and an average <br />ash content of about seven percent (BLM 2004). <br />These coals are desirable because they are <br />considered "compliance" coals under standards of <br />the Clean Air Act (CAA). <br />Geologic hazards are present in the LBA tract in the <br />form of rock falls, landslides, and slumps associated <br />with unstable moderate to steep slopes. Areas of <br />instability are typically associated with steep slopes <br />and saturated soil conditions. Slope aspect relative <br />to geologic structure also affects stability, where <br />dipping structure daylights on exposed slopes. <br />Projections from the West Elk Mine indicate that <br />two fault zones may be encountered in the LBA <br />tract. The inferred Gunnison and Deep Creek fault <br />zones are shown on Figure 3-2. The faults have not <br />been confirnied; their presence is inferred from <br />spatial location, some seismic data, and geometric <br />analysis. There are no discernible features of these <br />faults on the lands surface, suggesting that they are <br />buried features if they exist at all (Koontz 2005). <br />Soils <br />Soils in the project area have developed from a <br />combination of residual, colluvial, and alluvial <br />materials derived from local bedrock. The soil <br />survey identified and described six map units within <br />the LBA tract. The map unit name, percentage <br />coverage within the LBA tract, dominant soil series <br />and attendant percent map unit composition, <br />relative depth, hazard classifications (water erosion, <br />shrink swell, and mass movement), and <br />considerations as described in the soil survey are <br />shown in Table 3-1. <br />Soils in the project area are generally deep, fine- <br />textured and well suited for vegetative production <br />with steep slopes being the primary limitation on <br />use. Erosion and mass movement are potential <br />hazards associated with most soils in the area, due <br />to fine textures. Soils on steeper slopes have slower <br />infiltration rates, resulting in more surface flow and <br />erosion. Mass movement on steep slopes is also a <br />potential hazard, with Wetopa and Wesdy soil types <br />having the highest potential hazard rating within the <br />LBA tract (see Table 3-1). Fine textures and high <br />activity clays result in a moderate to high shrink- <br />swell hazard ratings for most soil types. <br />At the leasing stage, the locations of surface uses <br />are not known; therefore more detailed soil <br />information at the sites proposed for disturbance, <br />potential salvage depths, and volumes cannot be <br />estimated. Location-specific soil resource data will <br />be reviewed in more detail following if and when <br />post-leasing surface use is proposed. These uses <br />will be evaluated in subsequent NEPA analysis. <br />3.2.4 Environmental Consequences <br />3.1.4.1 Direct and Indirect Effects <br />Alternative A <br />Topography and Geology <br />The tract would not be leased and no mining would <br />occur; therefore, all topographic and geologic <br />conditions within [hc Dry Fork LBA tract would <br />remain in their current state. Ongoing natural <br />processes, including erosion and mass wasting, <br />would continue. <br />Sails <br />The tract would not be leased and no mining would <br />occur; therefore, soil conditions would exist in their <br />current state without effect. Ongoing natural <br />processes would continue. <br />Alternative B <br />The surface expression of underground coal <br />mining-related subsidence is the development of <br />broad elliptical troughs or basins overlying the <br />mined-out area. This area is defined laterally on the <br />land surface by the angle of draw, overburden type, <br />and thickness (i.e., the kinds and thickness of rocks <br />between the coal seam and the land surface), the <br />width of the longwall panels, and the height of the <br />coal mined. The angle of draw is the angle formed <br />by the vertical line drawn from the edge of the <br />longwall panel or gob area to the point of zero <br />subsidence on ground surface. There are four <br />subsidence zones that develop in [he overburden <br />above mining area (Peng 1992). A generalized <br />schematic of the subsidence zones are shown in <br />Figure 3-4. <br />3-8 Dry Fork Lease-By-Application FENS <br />