Smith Mountain introduced as one of two large mafic-ultramafic complexes mapped in the Dadeville Complex. Rock assemblage includes enstatite-hypersthene-pyroxenite masses, metagabbro, metanorite, massive amphibolites, and soapstone. Massive hornblende-amphibolite has been found near Smith Mountain. Pyroxenite bodies range in diameter from a few inches to several hundred ft. Complex appears to underlie the Agricola Schist-gneiss, but contact relationships between the two have not been ascertained. Smith Mountain may represent an ancient volcanic plug.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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