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The unit outcrops in the central part of the Deep River coal field, and gradationally overlies the Pekin and underlies the Sanford formations. The Cumnock formation of the Newark group is here adopted by the USGS. R., 1993, Revision of the biostratigraphy of the Chatham Group (Upper Triassic), Deep River basin, North Carolina, U. Although the Sanford Formation has not been dated paleontologically, it must extend into the lower Norian on the basis of lithologic correlation with the Stoneville Formation of the Danville-Dan River basin 100 km to the northeast. "No current usage" (†) implies that a name has been abandoned or has fallen into disuse.
The contact with the gradationally underlying Pekin formation is drawn at the top of the highest persistent red or brown beds below the Cumnock coal beds, and the contact with the gradationally overlying Sanford Formation is drawn at the base of the lowest persistent red or brown beds above the coal beds. The upper part of the Stoneville contains early Norian palynomorphs. Former usage and, if known, replacement name given in parentheses ( ).
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The Cumnock crops out in a narrow belt along the northwest side of the Sanford basin and at the southern end of the Durham basin. This evidence indicates that Chatham Group sediments were deposited from the early(? Slash (/) indicates name does not conform with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005).
Late Carnian palynomorphs were also identified in the Cumnock Formation in the Sanford subbasin, thus confirming the age of the Cumnock.
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