btw. p. 61 and 98. Of the eruptives in Washington limestone [Waits River limestone of current literature] the Barre granite plays most important part. The area is about 8 miles long and 4 miles wide, mostly in Barre Township, Washington County, Vermont, but with a small area in Williamstown Township, Orange County, Vermont. It is a fine granite, composed of quartz, feldspar, and mica, and of lower Trenton age.
Source: US geologic names lexicons (USGS Bull. 896, p. 117; USGS Bull. 1200, p. 221).
Barre granite, Devonian, intrudes Waits River limestone.
Source: US geologic names lexicon (USGS Bull. 896, p. 117).
Table opp. p. 288. Assigned Barre granite to Devonian.
Source: US geologic names lexicon (USGS Bull. 896, p. 117).
Pg. 70-73. Barre granite. Is an elongated, oval-shaped body that crops out in northwestern and west-central parts of East Barre quadrangle. Outcrop is confined to Westmore formation except at eastern margin, near East Barre village, where it extends a short distance in Waits River formation. Age is Devonian.
Source: US geologic names lexicon (USGS Bull. 1200, p. 221).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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