Pocahontas group divided into (descending) Flattop Mountain sandstone; Pocahontas coals Nos. 6, 5, 4, 3, 2, and 1 with intervening sandstones and shales; and Pocahontas sandstone.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Named as top member of Pocahontas group in Lower Pottsville series. Named for Flattop Mountain, 2 mi northwest of Pocahontas, southwestern VA. Consists of bluish-gray to brown, medium- to coarse-grained, micaceous, massive to current-bedded sandstone. Thickness is 22 to 50 ft. Overlies Rift shale. [Age is Pennsylvanian.]
Source: GNU records (USGS DDS-6; Reston GNULEX).
Unit is subtly distinct from other sandstones of the upper Pocahontas Formation. Flattop Mountain is a medium-grained, moderately sorted, texturally submature lithic arenite to sublitharenite, quartz grains composing 65 percent of the sandstone, while the lower sandstones are finer-grained and enriched in twinned plagioclase feldspar. Unit attains a maximum thickness of 13.7 m in the Crumpler quad, Mercer, McDowell, and Wyoming Cos. Consists entirely of channel-form sandstones with thin mudstone and siltstone partings. Locally massive in appearance but characteristically trough cross-bedded and contains internal erosional scours with claystone rip-up clasts, bark and tree molds, plant fragments, and carbonaceous debris. Forms a prominent bench or cliff where exposed.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Flattop Mountain Sandstone Member, uppermost part of Pocahontas Formation, is a massive sandstone present in VA and WV.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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