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Updated: Jul 12, 2026

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Morris Water Maze Experiment
Published on: September 24, 2008
Delaware river: evidence for its former extension to wilmington submarine canyon
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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