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Map showing publication footprint
  • Usage in publication:
    • Thompson Valley limestone
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Limestone
  • AAPG geologic province:
    • Appalachian basin
Publication:

Prouty, C.E., 1946, Lower Middle Ordovician of southwest Virginia and northeast Tennessee: American Association of Petroleum Geologists Bulletin, v. 30, no. 7, p. 1140-1191. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Pg. 1146 (fig. 3), 1152-1156. Thompson Valley limestone of Cliffield group. Proposed for the thick-bedded, light-gray, commonly variegated coarse-grained limestone originally referred to as zone 6 of Tazewell County classification by Cooper and Prouty [1943, GSA Bull., v. 54, no. 6]. This zone was included by them in their Ward Cove limestone which is here restricted to NIDULITES beds (zone 7). Thickness 75 feet at type section; about 250 to 300 feet in Fountain City, northeastern Tennessee. Underlies Ward Cove limestone; overlies Lincolnshire formation. In Saltville belt, beds similar to Thompson Valley limestone are exposed in McNutt quarry, 1.5 miles southeast of Sharon Springs, Virginia; this was previously referred to as Effna limestone (Cooper, 1944, Virginia Geol. Survey Bull., no. 60). Age is Middle Ordovician.
Type locality: Thompson Valley, Tazewell Co., southwestern VA. Extends into northeastern TN.

Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 3871).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

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