Named Toxaway Gneiss for the Toxaway River, Transylvania Co., NC. Unit is a granitic to quartz monzonitic gneiss. It is banded and forms the core of the Toxaway structural dome and shows repeating folding events. The Toxaway was previously called the Whiteside Granite. The base is not exposed; unconformably underlies the Tallulah Falls Formation.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Toxaway Gneiss of Hatcher (1974) has Rb-Sr whole-rock isochron age of 1109 +/-59 Ma (Fullagar and others, 1979).
Source: GNU records (USGS DDS-6; Reston GNULEX).
Toxaway Gneiss extended to GA. Described as light- to medium-gray, massive to well-layered, equigranular to inequigranular gneiss, characterized by coarse eyes or knots of quartz and feldspar enclosed by folia of medium-grained biotite; microcline commonly occurs as coarse, blocky porphyroblasts. Fullagar and others (1979) report a whole-rock age of 1203 +/-54 m.y. Age is Middle Proterozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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