Littoral of the Northeastern United States: Late Quaternary Warping
- 7 June 1968
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 160 (3832) , 1110-1112
- https://doi.org/10.1126/science.160.3832.1110
Abstract
Isobases constructed from recently published data are strikingly parallel to both the edge of the continental shelf off the northeastern United States and the Fall Zone. Our analyses suggest that the downwarping recorded by these isobases may be explained by Daly's hypothesis of a collapsing peripheral or marginal "bulge."Keywords
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