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- Usage in publication:
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- Warix Run Member*
- Modifications:
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- Named
- Dominant lithology:
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- Limestone
- AAPG geologic province:
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- Cincinnati arch
Summary:
The Warix Run Member of the Slade Formation, used informally by Dever (1977) and here named, consists of light-olive-gray quartzose calcarenite and lesser calcilutite. Strata of the Warix Run were previously assigned to the Newman Limestone, which is here excluded from the Cumberland Escarpment area of east-central and northeastern KY. Disconformably overlies the Borden Formation or Renfro, St. Louis, or Ste. Genevieve Members of the Slade Formation; intertongues with or conformably underlies the Mill Knob Member of the Slade. Thickness ranges from 0 to 31 m. Age is Late 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 ([ ]).