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• <br />The coal seams and the Rollins and C-Sandstones are the only truly tabular sedimentarv <br />bodies in the section. The two Sandstone bodies are even more laterally continuous than <br />the thinner coal seams. Because of strength and lateral persistency. these two marine <br />sandstone bodies have by far the best characteristics for bearing and distributing loads. <br />The C-Sandstone is approximately 50-ft thick. <br />li nrmr Creek NN-l? X?Sectiorn <br /> <br /> L•n or C.vd <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> (- 4•a nu' <br /> <br /> t <br /> R-l'p µ•r Suarn <br /> <br />?"'? - - -- - - --' R- Lnwvr Smm <br /> <br /> Ro 111 nr San d,tu m. <br /> Ic nanu.%16 ill t'a II R GB,.J da v Cohh l n+Grar eI <br /> X "IM FIu,ial Sandmne('hannd <br /> Land nar to Nlaw i, r ?Ia ri uc Sandstmc <br /> In t•rlr ddal Sandi mna Y On Irmo %Iudstm c <br /> S km mr <br /> Mud k,n e <br /> -/. (IWl <br />Figure Geologic section after Ilunt 2004. <br />0 <br />Maleki Technologies. Inc. Pa.-'e 1 I