Now showing items 1-3 of 3
Relative sea-level rise and the development of channel-fill and shallow-water sequences on Cape Cod, Massachusetts
(Massachusetts Institute of Technology, 1999)
Channel-fill sediments located in shallow-water off the south shore of Cape Cod, Massachusetts, provide a record of the late-Pleistocene and Holocene geological evolution in a post-glacial setting. Though conventionally ...
Recent relative sea-level change in Eastern North America
(Massachusetts Institute of Technology, 1987)