Pg. 3. Armuchee chert. Rusty, sandy, bedded chert, at places grading into ferruginous sandstone. Thickness 0 to 50 feet. Underlies Chattanooga shale and overlies Rockwood formation on north side of Coosa Valley, northwest of Coosa fault, northwestern Georgia. Probably contemporary with Frog Mountain sandstone, of Oriskany age, which is present only in the southwest corner of Rome quadrangle. [Age is Early and Middle Devonian.]
[Named from exposures around Armuchee, Floyd Co., northwestern GA.]
Source: US geologic names lexicon (USGS Bull. 896, p. 75).
Pg. 10. Typical Frog Mountain sandstone is all of Onondaga age. It extends northeast into Georgia, where it is present in Lavender Mountain and in Horseley Mountain, about 1 mile west of Rome, and was mapped by Hayes in Armuchee chert. In both of these mountains this sandstone is immediately underlain by fossiliferous chert which belongs to Armuchee chert of Hayes as described in Rome folio.
Source: US geologic names lexicon (USGS Bull. 896, p. 75).
Armuchee chert. Underlies Frog Mountain sandstone. [Age is Early and Middle Devonian.]
Source: US geologic names lexicon (USGS Bull. 1200, p. 137).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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