The Ocala Limestone is a late Eocene geologic formation of exposed limestones near Ocala, Marion County, Florida.
Age Period: Paleogene Epoch: Late Eocene Faunal stage: Late Clarkforkian through early Orellan Absolute Age: ~55.8 to ~33.9 mya, calculates to a period of approximately
Location The Ocala Limestone is at or near the surface within the Ocala Karst District located in west-central to the northwestern part of the peninsula. It is also within the Dougherty Plain District in the north-central panhandle where it easily forms karsts. These karsts often have several feet (meters) of relief which dramatically influence the topography of the Ocala Karst District and the Dougherty Plain District. The area is abundant with disappearing streams and springs.
Composition Formerly a geologic group, Ocala Limestone was downgraded to formation status by T.M. Scott in 1991.Scott, T.M, Lloyd, J.M, and Maddox, G., A Geological overview of Florida: Florida's Ground Water Quality Monitoring Program- Hydrogeological Framework: Florida Geological Survey Special Publication 32, p. 5-14. The Ocala Limestone consists of almost pure limestones with occasional dolomites. It can be subdivided into both lower and upper facies with the lower facies composed of a whitish to cream-colored, fine to medium grained, poorly to moderately hard, fossil rich grainstone and packstone. The upper Ocala is white and somewhat weak and poorly sorted. Its extremely fossil rich grainstone, packstone and wackestone and some chert is common in the upper facies. Its permeable and transmissive properties allow it to form a vital portion of the Floridan Aquifer.
Overlay The Ocala Limestone overlies the Avon Park Formation and forms part of the Floridan Aquifer System. (USGS)
Fossils Foraminifers, Lepidocyclina Echinoids Bryozoans Mollusks Rare vertebrates
References
External links SOFIA, United States Geological Survey: Florida geology maps