Named the Hall Stream member of the Gile Mountain formation for Hall Stream, Essex Co., eastern VT. Consists of highly feldspathic grit, probably of volcanic origin and feldspathic chlorite-ankerite schist and amphibolite. Unit is uppermost member of Gile Mountain. The Hall Stream is of Early Devonian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
Asterisk (*) indicates published by U.S. Geological Survey authors.
"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).
Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).