Passagassawakeag Formation is here proposed to replace term Knox Gneiss of Perkins and Smith (1925). Unit is subdivided into a basal calc-silicate member (30-150 m) and the upper Mixer Pond Member (new name) (300 m). Mixer Pond described as light-gray to white, fine-grained, massive, and compositionally layered feldspathic gneiss composed of hornblende, biotite, ferrosalite, and magnetite. Isotopic dating of Passagassawakeag by Zartman (oral commun., 1974) and Brookins (1975, written commun.) ranges from 430+/-10 m.y. (Pb206-Pb207, zircons) to 600+/-80 m.y. (Rb-Sr).
Source: GNU records (USGS DDS-6; Reston GNULEX).
Age of the Passagassawakeag Gneiss and its Mixer Pond Member of Bickel (1976) is Proterozoic(?) to Ordovician(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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