It is considered the basal member of the Chilhowee Group.
[1] The Weverton Formation dates back to the Cambrian period.
[2] The Buzzard Knob member is a coarse-grained quartzite with pervasive cross-beds.
The Owens Creek Member is a coarse-grained to conglomeratic metamorphosed greywacke.
This article about a specific stratigraphic formation in West Virginia is a stub.