A post-Harbor Hill-Charlestown moraine in southeastern Connecticut

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ID: 302838
1960
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Abstract
A discontinuous, NE.-trending belt, at least 13 mi. long, of linear accumulations of boulders and patches of hummocky till at which outwash deposits head, lies about 8 mi. N. of Long Island Sound near New London, Connecticut. This feature, here named the Ledyard moraine, marks a temporary halt during ice retreat from the moraines of Wisconsin age of Long Island and southern Rhode Island. It lies S. of the postulated line of the Middletown readvance.
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openalex_W2318715951 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Richard Goldsmith
Journal american journal of science
Year 1960
DOI
10.2475/ajs.258.10.740
URL
https://ajs.scholasticahq.com/article/58794.pdf
Keywords Keywords not found

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