Named the Durkee Hill greenstones for Durkee Hill, Strafford quadrangle, VT. Consists of a complex of gray to green to black basic and ultrabasic, massive and schistose, fine- to coarse-grained intrusives and volcanics and prominent chlorite schist. Light-gray feldspathic gneiss occurs irregularly among the greenstones. The Durkee Hill is of Late Devonian or post-Devonian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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