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<br /> <br />t 2.04.6 (2) (a) (i) <br />' The lithologies within the overburden above the F seam, the <br />interval referred to as the barren member in Section 2.04.6(2), <br />' consist of shales, siltstones, and sandstones with local thin <br />coals. Sandstones are predominantly massive and lenticular. <br />' Shale and siltstone intervals often occur as thin interbedded <br />sequences which show distorted bedding. Carbonaceous plant <br />fragments occur occasionally within all lithologies in the <br />' overburden. <br />' The stratum immediatley below the C seam consists of 5 to <br />12 feet of competent shales underlain by massive sandstone. <br />Refer to Figure 2.04.6(2)(a).Generalized Stratigraphic Column <br />for a graphical representation of available data. <br />(ii) Maps <br />' Refer to Figure 2.04.6(2)(a)-1, Drawings 2.04.6(2)(a)-1 and 2 <br />and to maps 2.04.6(2)(a)-3 and 2.04.6(2)(a)(i)-1, -2, and -3 <br />' for the Stratigraphic column, the geologic cross sections <br />the overburden isopach, and the strike and dip. <br /> <br /> <br />1 <br /> <br />1 <br /> <br />' <br /> 43 <br />