Mount Tom hornblende gneiss described here as the dark-green or green and white hornblende gneiss that forms Mount Tom, Little Mount Tom, and Mount Rat. Occurs as dikes in Hartland schist along northwest slope of Mount Rat.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Unit assigned to Mount Prospect complex (new).
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Mount Tom is dark-greenish-black or mottled black and white rock composed essentially of hornblende and plagioclase. Varies from coarse to fine grained, massive to foliated and lineated. Evidence in New Preston quad. for probable igneous origin.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Mount Tom hornblende gneiss is used in this report, as it applies primarily to hornblende gneisses in general area of Litchfield, New Preston, and Roxbury quads. Forms cluster of intrusive bodies in Hartland formation.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Mt. Tom Amphibolite included in Hartland Group in the Bantam Lake thrust sheet, along with Litchfield Schist. Hartland Group in the Cameron's Line thrust sheet includes the Mt. Prospect [Prospect] Formation, the Mt. Rat Schist [first used] and the Bee Brook Formation [first used]. Described as dark-green to black, fine- to coarse-grained, massive, lineated, or foliated, quartz-andesine-hornblende gneiss. Age shown as Cambrian(?) and Ordovician.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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