Florida Geological Survey - Geology Topics
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The Avon Park Formation is composed of cream to light-brown
or tan, Middle Eocene (see time
scale), fossiliferous marine limestone interbedded with
dolostone. In a few areas of west-central Florida, molds of
evaporites may be present in the dolostone. The Avon Park
Formation occurs throughout the Florida peninsula and the
eastern panhandle. It comprises the oldest rock cropping out
in Florida. These sediments are locally exposed in sinks and
quarries near the crest of the Ocala Platform in Citrus and
Levy Counties. Avon Park fossils include mollusks,
foraminifera, echinoids, algae, and carbonized plant
remains.
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