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  • Usage in publication:
    • Lake Ardmore sandstone [member]
  • Modifications:
    • Named
  • Dominant lithology:
    • Sandstone
  • AAPG geologic province:
    • South Oklahoma folded belt
Publication:

Tomlinson, C.W., 1929, The Pennsylvanian system in the Ardmore basin: Oklahoma Geological Survey Bulletin, no. 46, 79 p.


Summary:

Named as a member of Springer formation in the Ardmore basin in southern OK in the S. Oklahoma folded belt province. Name derived from a sportsman's lake of that name in sec 2, T4S, R1E, Carter Co, OK, where ledge forms narrow peninsulas and islets. No type locality given. Is a persistent sandstone quite similar in character to the Overbrook sandstone member (new) of the Springer formation. Is 15 to 20 ft thick. Lies 500 ft or less above the Overbrook; overlies and underlies unnamed black shale of Springer. Is 250 to 500 ft below Primrose member (new) of Springer formation. A few casts of coiled cephalopods, not specifically identifiable, found near southwest corner sec 6, T6S, R2E, just north of Springer. Fossil list; geologic map; columnar section. Of Pennsylvanian age.

Source: GNU records (USGS DDS-6; Denver GNULEX).


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

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

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