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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Conway Cut siltstone member
  • Modifications:
    • Named
  • Dominant lithology:
    • Siltstone
  • AAPG geologic province:
    • Cincinnati arch
Publication:

Stockdale, P.B., 1939, Lower Mississippian rocks of the east-central interior [Indiana, Kentucky, Ohio]: Geological Society of America Special Paper, 22, 248 p.


Summary:

Named Conway Cut siltstone member of New Providence Formation. Composed of siltstone which is massive, gritty, and cliff-forming. Gray to light buff where fresh. Curly worm marks and TAONURUS abound. In places, large limestone or iron carbonate concretions are prominent. As much as 75 ft thick. Age is Early Mississippian.

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


Map showing publication footprint
  • Usage in publication:
    • Conway Cut Bed*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Cincinnati arch
Publication:

Weir, G.W., Gualtieri, J.L., and Schlanger, S.O., 1966, Borden Formation (Mississippian) in south- and southeast-central Kentucky, IN Contributions to stratigraphy, 1965: U.S. Geological Survey Bulletin, 1224-F, p. F1-F38.


Summary:

Conway Cut siltstone member of New Providence formation of Stockdale (1939) reduced in rank to Conway Cut Bed and assigned to Cowbell Member of Borden Formation. Upper Bed of two that extend southward from the main body of the Nancy Member of the Borden Formation. Crops out in south-central Kentucky. Age is Early Mississippian.

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

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).