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2.2.1 (Continued) <br />Coal and other strata outcrops on the north-facing slopes within <br />•- the Sulfur Creek syncline and on the Meeker project area are rare, <br />being obscured by colluvial and local "alluvial" deposits originated <br />from parent Williams Fork Formation strata. In addition, the thin <br />topsoil layers and live and decaying vegetation contribute to <br />masking rock exposures. Only the FF coal seam, rather the <br />clinkered outcrop of the coal; and approximately the 100 feet of <br />sandstone, sandy shale and siltstone encorrrpassing the bed are <br />exposed in the south slope of an east-west trending ridge near <br />the center of Sections 21 and 22, Tavnship 2 North, Range 93 West. <br />Across Highway 13/789 from the active Rienau No. 2 P.1ine, the <br />G coal bed is locally exposed at the buried mine portals of <br />the abandoned Rienau No. 1 underground coal mine. <br /> <br /> <br />F-5a <br />