You are not currently logged in.
Access JSTOR through your library or other institution:
If You Use a Screen ReaderThis content is available through Read Online (Free) program, which relies on page scans. Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Extent and Formation of Deeply Buried Channels on the Continental Shelf off Southern New England
Robert L. McMaster and Asaf Ashraf
The Journal of Geology
Vol. 81, No. 3 (May, 1973), pp. 374-379
Published by: The University of Chicago Press
Stable URL: http://www.jstor.org/stable/30084831
Page Count: 6
You can always find the topics here!Topics: Ice, Valleys, Geology, Vineyards, Moraines, Glacial landforms, Flint, Glacial drift, Coastal plains, Coasts
Were these topics helpful?See somethings inaccurate? Let us know!
Select the topics that are inaccurate.
Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Preview not available
Seismic reflection profiles reveal a network of deeply buried channels that extends from coastline buried bedrock valleys to some 50 km off Rhode Island. Thalwegs below sea level reach 100-286 m in Coastal Plain deposits. The limited extent, depth, and longitudinal profiles of these channels together with the seaward lobate boundary of the channel pattern suggest severe ice scour modifications of late Tertiary-early Pleistocene preglacial river valleys. Maximum ice advance is correlated with a pre-Woodfordian ice margin of the Wisconsin stage.
The Journal of Geology © 1973 The University of Chicago Press