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The AAPG/Datapages Combined Publications Database

GCAGS Transactions

Abstract


Gulf Coast Association of Geological Societies Transactions
Vol. 27 (1977), Pages 409-420

Plio-Pleistocene Paleogeography of the Florida Gulf Coast Interpreted from Relict Shorelines (1)

Charles D. Winker, James D. Howard (2)

ABSTRACT

Detailed analyses of large-scale topographic maps permit the interpretation of relict coastal features and the compilation of a shoreline record which can be differentiated into relative age groups. Each shoreline sequence is mapped on the basis of lateral continuity and alignment, state of topographic preservation, and elevation. taking into account the possibility of regional warping. This method indicates, for each period of high sea level, not only paleogeography but regional variations in erosion and deposition as well.

In Florida, three sequences of relict Gulf shorelines are recognized, none of which has previously been mapped, as either a terrace or a stratigraphic unit. The Escambia Sequence is well preserved from Mobile Bay to south of Tampa Bay, at elevations below 10 m, primarily as erosional scarps, but in Escambia and Gulf Counties as beach ridge plains. These shorelines have sometimes been described as Sangamon (late Pleistocene) in age. The Wakulla Sequence consists primarily of a discontinuous scarp between 20 and 30 m above present sea level, which forms a broad arc between the Apalachicola River and Tampa Bay. Beach ridges in Wakulla and Leon Counties and some scarps around Tampa Bay may be part of the sequence. The Gadsden Sequence consists of an extensive beach ridge plain occupying a warped, dissected upland surface between Tallahassee and the Escambia River. This surface reaches a maximum elevation of 100 m. Original ridge-and-swale trends are preserved as, and accentuated by, a deeply incised network of trellis drainage. On the Florida peninsula, the Brooksville, Lakeland. and Bartow Ridges probably represent contemporaneous deposition.

During formation of the Gadsden Sequence, the Apalachicola River built a large cuspate delta into the Gulf. At the same time, beach ridges were built on the peninsula by sand brought from the delta by longshore transport. Later, during formation of the Wakulla and Escambia Sequences, clastic deposition was localized near the mouths of the Apalachicola and Escambia Rivers. Little sand was introduced to the Gulf side of the peninsula, in striking contrast to the Atlantic side during the same period.


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