Pg. 295-296. Bradford schist. The noncalcareous member of Calciferous mica schist. Named from Bradford, [Mount Cube quadrangle], Orange Co., northeastern VT, where it predominates. The calcareous member is here named Washington limestone.
Source: US geologic names lexicon (USGS Bull. 896, p. 246-247).
Pg. 81. Bradford schist. Contains lower Trenton fossils. Was originally a sandstone, which is now represented by terranes of granular and micaceous quartzite and a foliated mica schist. Overlies black slate of Ordovician age. The Washington limestone is intimately interstratified with Bradford schist.
Source: US geologic names lexicon (USGS Bull. 896, p. 246-247).
Pg. 90, 115, footnote. Bradford schist. Includes all of the non-calcareous members of old "Calciferous Mica Schist." It therefore embraces the quartzite, staurolitic, actinolitic, amphibolitic, ottrelitic, graphitic, and garnetiferous phases lying between 2 large narrow belts of slate and shale, one on east near Connecticut River, the other on west passing through Newport and Montpelier to Barnard.
[USGS has adopted Vershire schist as substitute for Bradford schist (preoccupied). Washington limestone (preoccupied) is replaced with Waits River limestone.]
Source: US geologic names lexicon (USGS Bull. 896, p. 246-247).
Bradford schists, in Bradford Township, overlie Waits River limestone and are therefore younger than the phyllites here named Randolph phyllite.
Source: US geologic names lexicon (USGS Bull. 896, p. 246-247).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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