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Regional significance of pre-Wisconsinan till from Nantucket Island, Massachusetts

Quaternary Research

By:
and
https://doi.org/10.1016/0033-5894(83)90037-6

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Abstract

A major pre-Wisconsinan glacial event is the only possible source of the lower till on Nantucket Island, Massachusetts. The till occurs near the late Wisconsinan drift border and below fossiliferous marine beds of oxygen-isotope stage 5 (Sangamonian) age. It is considered to be Illinoian in age, but the evidence is tenuous. The till is correlated with the lower till of New England, and its presence supports the view that the New England upper and lower tills represent two glaciations. The pre-Wisconsinan (lower) till in New England may correlate with older tills elsewhere in the northeastern United States and in southeastern Canada that are considered to be early Wisconsinan or older in age. ?? 1983.

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Additional publication details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Regional significance of pre-Wisconsinan till from Nantucket Island, Massachusetts
Series title:
Quaternary Research
DOI:
10.1016/0033-5894(83)90037-6
Volume:
19
Issue:
3
Year Published:
1983
Language:
English
Publisher:
Elsevier
Publisher location:
Amsterdam, Netherlands
Contributing office(s):
Woods Hole Coastal and Marine Science Center
Description:
10 p.
First page:
302
Last page:
311
Country:
United States
State:
Massachusetts
Other Geospatial:
Nantucket Island