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Soils <br />• <br />• <br /> <br />oversight from the OSM, which govern all <br />direct effects of coal mining, including those <br />that ,may impact geology. These acts and <br />attendant regulations require that topsoil be <br />removed, stockpiled, and replaced on reclaimed <br />surfaces associated with construction or mining <br />disturbance. Other impacts to the geologic <br />resource that may occur as a result of mining, <br />including landslides and erosion, must be <br />mitigated to stabilize the surface and return the <br />land to an approved post-mining land use. <br />$OI~S <br />Affected Environment <br />The analysis area for soil resources is the <br />i~rn~anf orP~ Qnt~c 7n ttlP T~Yl~I P!`t '.IYPA l~PVPIO7lP(1 <br />from a combination of residual, colluvial, and <br />alluvial materials derived from local. bedrock <br />(Figure 9). The soil. survey (fryer and Hughes <br />1997) describes 12 map units that could be <br />affected. The map unit name, dominant soil. <br />series and attendant percent map unit <br />composition, relative depth, hazard <br />classifications (water erosion., shrink swell, and <br />mass movement), and. considerations described <br />in the soil survey are shown in Table 3-2 and <br />Figure 9. <br />Table 3-2 <br />Summary of Soil Resources <br /> % of Hazard / <br />U <br />it N <br />S <br />il M <br />Soil Map Unit Dominant Depth ame <br />ap <br />n <br />o <br />Name /Number Soil Series Map Class Water Shrink Mass Number <br /> Unit Erosion Swell Movement <br />Broad Canyon -Scout Broad Canyon 50 VD L L L Soil erosion in steeper areas; <br />family complex, and similar soils <br />low water-holding capacity; <br />5 to 25% slopes Scout family and 35 VD L L L subsurface rock fragments. <br />111 similar soils <br />Cerro -Henn Cerro and similar 45 VD L H L High shrink-swell potential; <br />complex, soils slow permeability; clayey <br /> surface soil textures; clayey <br />0 to 15 percent slopes Hern and similar 40 VD L H L subsurface soil textures. <br />116 soils Corrosivity in Cerro soils. <br />Coberly -Falcon, dry Coberly and 45 MD L L L Shallow bedrock; low water- <br />complex, similar soils holding capacity. <br />0-15% slopes dry and <br />Falcon Root limiting layer in Falcon <br />124 , <br />similar soils 40 S L L L dry soils. <br /> Cryochrepts soil <br />35 <br />S - D <br />L - H <br />L <br />L - M Steep slopes in some areas; <br />Cryochrepts - <br />and similar soils <br />high soil erosion hazard in <br />Cryoborolls; rubble the steeper areas; subsurface <br />land complex, Cryoborolls and 30 S - VD H L M rock fragments, moderate <br />15-90% slopes similar soils mass movement potential. <br />130 Large exposures of loose <br /> Rubble land 25 rock. <br /> Limited available water <br />Cumulic Haploborolls, Cumulic capacity; subsurface rock <br />1 to 3% slopes Haploborolls and 85 D - VD L L L fragments; spring runoff <br />131 similar soils flooding; low bearing <br /> ca acit ;subsurface rock <br />Deer Creek Ventilation Shaft and E Seain Methane Drainage Wells FEIS <br />73 <br />