Suwannee Limestone Stratigraphic range: Oligocene |
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Type | Geological formation |
Underlies | Hawthorn Group-Arcadia Formation |
Overlies | Ocala Limestone |
Thickness | 160 feet |
Lithology | |
Primary | Limestone |
Location | |
Region | North Florida |
Country | United States |
Extent | Leon to Hamilton to Taylor counties |
Type section | |
Named for | Suwannee River |
Named by | C.W. Cooke and W.C. Mansfield |
The Suwannee Limestone is an Early Oligocene geologic formation of exposed limestones in North Florida, United States.
Period: Paleogene
Epoch: Early Oligocene
Faunal stage: Rupelian ~33.9 to ~23 mya, calculates to a period of approximately 16.9 million years
Suwannee Limestone is found in the peninsula carbonate outcroppings on the northwestern, northeastern and southwestern flanks of the Ocala Platform. However, Suwannee Limestone is not present on an area known as Orange Island on the eastern side of the Ocala Platform due to erosion, nondeposition or both. This limestone is present in southeastern Leon, Jefferson, Madison, Taylor, Lafayette counties as well as Hamilton along the upper Suwannee River basin, and southward into Suwannee County, Florida.
Early Oligocene Suwannee Limestone was recognized in the northwestern peninsula by P. F. Huddleston in 1993 as a triple subdivision of Suwannee Limestone, Ellaville Limestone, and Suwannacoochee Dolostone.