Named the Barton River formation for the Barton River, VT. Consists of mostly slates and phyllites intercalated with limestones and calcareous schists. Calcareous rocks are more abundant toward top; phyllites most common at top. Thickness is difficult to determine because of overturning; about 8800 feet. The Barton River underlies the Westmore formation and unconformably overlies the Ayers Cliff formation. Unit is considered of Silurian age based on stratigraphic position.
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 ([ ]).