Title: A post-Harbor Hill-Charlestown moraine in southeastern Connecticut
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...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.Read More