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UecFmber L'2003 Paae3-18 <br />Townsend'S Big-eared Bat. Townsend's big-eared bats occur throughout western North America <br />including much of Colorado, normally below 9,600 feet in elevation (Fitzgerald et al., 1994; Armstrong et <br />al., 1984). Roosting colonies are in caves, mineshafts, and other man-made structures. The species <br />forages over most habitat types except dense coniferous forests (Armstrong et al., 1984). Suitable roost <br />and maternity sites are not present within the LBA tract area, and it is unlikely that this species occurs as <br />a local resident. <br />3.6.2 Environmental Consequences <br />Alternative 1 -Proposed Action <br />The only surface disturbance that would occur in the LBA tract is surface subsidence, which could <br />potentially affect wildlife habitat by minor surface cracking and by causing small, isolated changes in <br />vegetation communities or surface topography. Gradual subsidence of six to eight feet is expected to <br />occur on the ground surface overlying longwall mining areas. Surtace cracks up to 12 inches wide and 30 <br />feet deep may occur in soil and rock. Cracks are more likely on ridgetops with bare rocks and cliffs, and <br />less likely in valleys and other areas with deep soils. Soil cracks tend to fill with dirt and debris and heal <br />relatively quickly. Cracks in bare rock are likely to remain longer. <br />Cracks in cliff faces have a slight chance to disturb nesting or roosting wildlife such as peregrine falcons <br />and bats. However, the cracks are likely to be minor, and would be additional to natural cracking and <br />rockfall continuously occurring on the cliffs. Sensitive species such as peregrine falcons and bats occur <br />rarely if at all on the cliffs in the LBA tract, and the chances of measurable disturbance to sensitive <br />species by surface cracking are relatively minor. <br />Little information is available about the potential effects of subsidence on plant communities. Subsidence <br />monitoring by MCC on adjacent coal leases in the 1990s found no obvious changes to the plant <br />communities as a result of subsidence within the region. Minor impacts to plants could occur along the <br />edges of subsidence cracks and in limited areas where surface water flow is altered by surface cracking. <br />However, these minor vegetation changes would be very small and would not be likely to measurably <br />affect wildlife habitats or the continued existence of any federal listed or sensitive species. <br />Subsidence could potentially accelerate mass wasting (landslides and rock falls). Natural mass wasting is <br />locally common in the area particularly landslides and slumps associated with major precipitation events <br />(Bureau of Land Management and Forest Service, 2000). These natural events are difficult to distinguish <br />from possible subsidence-related effects, and many occur below the coal-bearing strata. Where the <br />overburden is thick, such as in the proposed LBA tract, no increase in mass wasting can be considered <br />likely based on available data. <br />Underground mining has the potential to intercept ground water in faults. MCC estimates that about 150 <br />acre-feet of water may be encountered underground in the LBA tract (Koontz, 2003). Also see Section <br />3.4.2, Environmental Consequences (Alternative 1 -Proposed Action). This encountered water would be <br />considered non-tributary ground water, and it would not contribute to water depletion in the Colorado <br />River Basin. Therefore, there would be no effects to the four Colorado River endangered fish species. <br />Because the only surface disturbance resulting from the proposed project would be surface subsidence, <br />individuals and habitats for elk, mule deer, Lewis's woodpecker, northern goshawk, hairy woodpecker, <br />Envirnnr:ent,at >lssessmc!~i <br />Mdest I=latiron LBA i i 8^t <br />r~~_mrison Countv.:;olorado <br />