Delaware River: Evidence for its former extension to Wilmington Submarine Canyon

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Abstract

Seismic-reflection profiles indicate that during the Pleistocene the Delaware River flowed across the continental shelf east of Delaware Bay and emptied into Wilmington Submarine Canyon. The ancestral valley (width, 3 to 8 kilometers; relief, 10 to 30 meters) is buried, is not reflected in the surface topography, and probably predates the formation of the present canyon head.

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Publication type Article
Publication Subtype Journal Article
Title Delaware River: Evidence for its former extension to Wilmington Submarine Canyon
Series title Science
DOI 10.1126/science.195.4277.483
Volume 195
Issue 4277
Year Published 1977
Language English
Publisher American Association for the Advancement of Science
Description 3 p.
First page 483
Last page 485
Country United States
State Delaware
Other Geospatial Delaware Bay
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