The Bottom Creek Suite is here named in the Pedlar massif in the Blue Ridge of VA. It is a charnockite suite and contains mesocharnockite, megaporphyry, and porphyroblastic gneiss rock types. Age is Middle Proterozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Bottom Creek is dominant unit of the Pedlar massif. Petrographically similar to the charnockites and jotunites of the Pedlar River Suite. Contains porphyroblastic charnockite and a few small bodies of mafic jotunite/norite. Foliation due to alignment of feldspar porphyroblasts and mafic minerals (pyroxene and garnet). Ultramafic rocks occur only as a few small dikes.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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