Coweeta Group formally named in Macon Co., west-central NC, where it occupies syncline resulting from polyphase deformation. Composed of feldspar-quartz-biotite gneiss, metasandstone, quartzite, and schist. Thickness ranges from 2,000 to 4,000 m. Includes Persimmon Creek Gneiss, Coleman River Formation, and Ridgepole Mountain Formation (all formally named in this report). Overlies Tallulah Falls Formation; upper contact not observed. Age is late Precambrian(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Coweeta Group of Hatcher (1979), and informally named units assigned to it, the Persimmon Creek gneiss, Coleman River formation, and Ridgepole Mountain formation, are here abandoned. Mapping for this study shows that the Coweeta Group belongs partly to the Sandy Springs Group and partly to the Richard Russell Formation in the Bill Arp thrust sheet.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Composes part of Toe terrane, which also includes Ashe Metamorphic Suite, Alligator Back Metamorphic Suite, and Tallulah Falls Metamorphic Suite. Age is Late Proterozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Coweeta Group and its Persimmon Creek Gneiss, Coleman River Formation, and Ridgepole Mountain Formation are used informally in this report (local usage of Hatcher, 1979). Age changed from Late Proterozoic to Late Proterozoic and early Paleozoic. All formations are found in Richard Russell thrust sheet, east of Shope Fork fault.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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