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The AAPG/Datapages Combined Publications Database
GCAGS Transactions
Abstract
The Ancient Mississippi River
C. John Mann, William A. Thomas
ABSTRACT
Stratigraphic evidence in the central Mississippi Embayment indicates that apparently a stream of major size has continuously occupied approximately the same location as the existing Mississippi River since at least Late Jurassic. Significant deltaic sediments occur in the Smackover Limestone (Late Jurassic) and in most younger units. The stream which has persisted from the Jurassic to the present is referred to here as the Ancient Mississippi River.
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