In West Canada Valley, east-central NY, Valley Heads Drift unconformably overlies West Canada Diamicton (new name), uppermost member of newly named Middleville Formation. Boundary between the two units is called the Shed Brook discontinuity (Ridge, 1985). Unit has been dated at 15.5-12.9 ka and tentatively assigned to the Port Bruce and Port Huron stadials by previous authors.
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 ([ ]).