| Suwannee Limestone | |
|---|---|
| Stratigraphic range: Oligocene | |
| Type | Geological formation |
| Underlies | Hawthorn Group- Arcadia Formation |
| Overlies | Ocala Limestone |
| Thickness | 160 ft (49 m) |
| 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.
Description
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. [1] 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. [2] The Suwannacoochee Dolostone was later officially renamed as the Suwannacoochee Dolomite. [3]
Sedimentology
Suwannee Limestone consists of a white to cream, poorly to well hardened, fossil rich, vuggy to moldic grainstone and packstone. The dolomitized parts of the Suwannee Limestone are gray, tan, light brown to moderate brown, moderately to well indurated (hard), finely to coarsely crystalline, dolomite with limited occurrences of fossil-bearing beds. Limestone in silicate form is common in Suwannee Limestone. [4] [5]
Stratigraphy
The Suwannee Limestone overlies the Ocala Limestone and forms part of the intermediate confining unit/aquifer system. (USGS)
Fossil content
References
- ^ Bryan, J.R., 1991, Stratigraphic and paleontologic studies of Paleocene and Oligocene carbonate facies of the eastern Gulf Coastal Plain: unpublished Ph.D. dissertation, University of Tennessee, Knoxville, TN, 324 p.
- ^ Huddleston, P.F., A revision of the lithostratigraphic units of the Coastal Plain of Georgia - The Oligocene: Georgia Geological Survey Bulletin 105, 152 p.
- ^ Stamm, N., 2018, Geologic Unit: Suwannacoochee. National Geologic Map Database Geolex — Unit Summary, U.S. Department of the Interior, U.S. Geological Survey, Reston Virginia.
- ^ Cooke, C. W., and Mansfield, W. C., 1936, Suwanne Limestone of Florida (abstract): Geological Society of America Proceedings, 1935, p. 71–72.
- ^ USGS: Geology of Florida
| Suwannee Limestone | |
|---|---|
| Stratigraphic range: Oligocene | |
| Type | Geological formation |
| Underlies | Hawthorn Group- Arcadia Formation |
| Overlies | Ocala Limestone |
| Thickness | 160 ft (49 m) |
| 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.
Description
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. [1] 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. [2] The Suwannacoochee Dolostone was later officially renamed as the Suwannacoochee Dolomite. [3]
Sedimentology
Suwannee Limestone consists of a white to cream, poorly to well hardened, fossil rich, vuggy to moldic grainstone and packstone. The dolomitized parts of the Suwannee Limestone are gray, tan, light brown to moderate brown, moderately to well indurated (hard), finely to coarsely crystalline, dolomite with limited occurrences of fossil-bearing beds. Limestone in silicate form is common in Suwannee Limestone. [4] [5]
Stratigraphy
The Suwannee Limestone overlies the Ocala Limestone and forms part of the intermediate confining unit/aquifer system. (USGS)
Fossil content
References
- ^ Bryan, J.R., 1991, Stratigraphic and paleontologic studies of Paleocene and Oligocene carbonate facies of the eastern Gulf Coastal Plain: unpublished Ph.D. dissertation, University of Tennessee, Knoxville, TN, 324 p.
- ^ Huddleston, P.F., A revision of the lithostratigraphic units of the Coastal Plain of Georgia - The Oligocene: Georgia Geological Survey Bulletin 105, 152 p.
- ^ Stamm, N., 2018, Geologic Unit: Suwannacoochee. National Geologic Map Database Geolex — Unit Summary, U.S. Department of the Interior, U.S. Geological Survey, Reston Virginia.
- ^ Cooke, C. W., and Mansfield, W. C., 1936, Suwanne Limestone of Florida (abstract): Geological Society of America Proceedings, 1935, p. 71–72.
- ^ USGS: Geology of Florida