Named the Gratton limestone for Gratton, 5 miles east of Tazewell, Tazewell Co., VA. Consists of laminated limestone and calcilutite that ranges from 0 to 120 feet thick (averages 60 feet). The Gratton corresponds to the lower part of Butts' (1940) Lowville-Moccasin interval east of Tazewell. Unit overlies the Burkes Garden member of the Benbolt limestone, the Shannondale member of the Benbolt limestone, or the Cliffield formation, and underlies the Wardell formation. The Gratton is of Middle Ordovician age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Pg. 1165-1166. Gratton limestone. Geographically extended into northeastern Tennessee. Formation thins toward southwest as underlying Benbolt limestone and overlying Wardell formation thicken. Between Tazewell and Sharps Chapel, the Gratton rests directly on dolomites of the Beekmantown and locally has thickness of several hundred feet. [Age is Middle Ordovician.]
Source: US geologic names lexicon (USGS Bull. 1200, p. 1581).
The Gratton Limestone occurs in the subsurface of southwestern VA between the St. Clair and Pulaski thrust faults as shown in section G-G'. Overlies the Wardell Formation and underlies the Moccasin Formation. The Gratton is of Middle Ordovician (Mohawkian) age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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