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83 <br /> The 1975 SCS soil map was referenced for this updated east pit <br /> survey. Map units were delineated by relating the soils to land- <br /> forms and topography, geology, drainage patterns, vegetation, and <br /> visible surface soil features. Map unit names contained in the <br /> SCS legend (1975) and used later by Fly and Associates (1979) in the <br /> west pit area (Section 25) were correlated to east pit (Section 31) <br /> soils. The SCS map unit boundary lines were transferred to high <br /> quality black and white stereo prints that were flown October 26, <br /> 1979. Soil boundaries were refined in an office photo-interpretive <br /> study using a mirror stereoscope. The refined mapping was then <br /> transferred to a revised and updated 1" = 400' topographic base <br /> map. <br /> SURVEY RESULTS <br /> Three map lusts were identified within the field soil survey area <br /> (see Exhibit 9-1) . These are 9904/D2, Persayo clay loam and sandy <br /> clay loam, 10 to 20% slopes; 9904/F2, Persayo clay loam and sandy <br /> clay loam, >25% slopes; and 18/F2, Torriorthent-Rock Outcrop Com- <br /> plex, >25% slopes. The Persayo soils occupy the moderately steep <br /> ridgetops and steep north facing sideslopes. The Torriorthent-Rock <br /> Outcrop Canplex occupies steep to very steep stoney south facing <br /> sandstone ridges, sideslopes, bluffs, and sharp rolling lands. <br /> The Persayo map unit and series descriptions with laboratory analysis <br /> data are found in the Soil Survey Text, Tab 9. The steep Persayo <br /> soil is very similar to the moderately steep Persayo soil. However, <br /> slopes are slightly steeper and the soil profile is somewhat thinner. <br /> All pit disturbance in Section 31 will occur within the moderately <br /> steep Persayo map unit. Disturbance associated with highwall re- <br /> duction will extend further to the northwest into the steep Persayo <br /> map unit. There will be no additional disturbance in the Torriorthent- <br /> Rock Outcrop Canplex. <br />