Pg. 49-50, and under county descriptions. Herbert conglomerate. Basal member of Bonair sandstone. Consists of 40 to 150 feet of soft, light-yellow sandstone, coarse grained and in places conglomeratic. Underlies Eastland shale lentil of Bonair sandstone, and rests on Whitwell shale. [Age is Early Pennsylvanian (early Pottsville).]
Recognized in Bledsoe, White, Van Buren, Hamilton, and Cumberland Cos., southeastern TN. Best measurement was taken on Glade Creek just north of old road from [Herbert Domain], Bledsoe Co., to Sparta crosses this stream, [Pikeville quadrangle, scale 1:125,000], southeastern TN.
Source: US geologic names lexicon (USGS Bull. 896, p. 943).
Listed as Herbert member of Lee formation. [Age is Early Pennsylvanian (Pottsville).]
Source: US geologic names lexicon (USGS Bull. 1200, p. 1737-1738).
Chart 6 (column 17). Herbert sandstone. Correlation chart shows Herbert sandstone underlying Eastland formation and overlying Whitwell [shale]. [Age is Early Pennsylvanian (Pottsville).]
Source: US geologic names lexicon (USGS Bull. 1200, p. 1737-1738).
Pg. 4. Herbert conglomerate member of Bon Air sandstone. The conglomeratic phase of Newton sandstone in southern Cumberland and northern Bledsoe Counties was the type "Herbert conglomerate" erroneously considered by Nelson (1925) to be older than Newton. Shale thought to be between sandstones and named "Eastland shale" by Nelson is actually Whitwell shale; therefore, names "Herbert" and "Eastland" are discarded [abandoned].
Source: US geologic names lexicon (USGS Bull. 1200, p. 1737-1738).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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