The Nellysford Granulite Gneiss is here named in the Pedlar massif in the central Blue Ridge, Virginia. It consists of well layered, dark grayish-green to dark-green, fine- to medium-grained, granoblastic, garnet-hypersthene-quartz-feldspar gneiss. It is found along the eastern margin of and as roof-pendants in the Pedlar River pluton. Contacts with the pluton are concordant and gradational. 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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