The Hills Mountain Granulite Gneiss is here named in the Lovingston massif in the central Blue Ridge, VA. It consists of gray, medium-grained, hypersthene-bearing quartzo-feldspathic gneiss with granoblastic texture and poorly developed segregation layering. It forms most of the country rock around and roof-pendants in the Archer Mountain pluton. The contact zone between the gneiss and the pluton consists of a zone of migmatitic granulite gneiss. Age is Middle Proterozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Hills Mountain Granulite Gneiss was mapped by Bloomer and Werner (1955) as Lovingston Granite as opposed to surrounding Lovingston Gneiss, and by Bartholomew (1977) as poorly layered granulite gneiss.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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