Summary
The Key Largo Limestone is a geologic formation in Florida. It is a fossilized coral reef. The formation is exposed along the upper and middle Florida Keys from Soldier Key (at the north end of the Florida Keys) to the Bahia Honda Channel (at the west end of Bahia Honda Key). The islands form a long narrow arc concentric with the inner edge of the Florida Straits and with the Florida Reef. The limestone includes fossils of corals, mollusks and bryozoans. Fossilized coral head formations are visible in some exposures.[1][2] The Key Largo Limestone continues in a narrow band underwater just offshore of the coast of Florida north of Soldier Key to the middle of the Palm Beach County coast, and southward just offshore of the lower Florida Keys to the Dry Tortugas.[3]
| Key Largo Limestone | |
|---|---|
| Type | Formation |
| Location | |
| Region |  Florida |
| Country |  United States |
See also edit
Citations edit
- ^ "Key Largo Limestone". USGS. Archived from the original on November 28, 2021. Retrieved May 8, 2019.
- ^ "Pleistocene geology". USGS South Florida Information Access. September 4, 2013. Archived from the original on July 31, 2020. Retrieved May 8, 2019.
- ^ Mitchell-Tapping 1980, p. 118.
References edit
- Mitchell-Tapping, Hugh J. (Spring 1980). "Depositional History of the Oolite of the Miami Limestone Formation". Florida Scientist. 43 (2): 116–125. JSTOR 24319647.