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Edward J. Petuch states that Orange Island was a dominant geomorphological feature of the Bainbridge Subsea on the Florida Platform [1] According to J. R. Bryan and the United States Geological Survey, a lack of deposition with reference to the eastern side of the Ocala Platform indicates this area as Orange Island. [2]
Group or Formation Period Notes Alachua Formation: Neogene: Chipola Formation: Neogene: Cypresshead Formation: Neogene: Oak Grove Formation: Neogene: Shoal River Formation
Location of the Hawthorn Group within Florida (in red). The Hawthorn Group (also Hawthorne Group, previously called Hawthorn(e) Formation) [a] is a stratigraphic unit of Miocene age in South Carolina, Georgia, and Florida, in the United States.
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The Bone Valley Formation is a geologic formation in Florida. It is sometimes classified as the upper member of the Peace River Formation of the Hawthorn Group . [ 2 ] It contains economically important phosphorite deposits that are mined in west-central Florida, as well as rich assemblages of vertebrate fossils .
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This article about a specific stratigraphic formation in Florida is a stub. You can help Wikipedia by expanding it.
The Ten Thousand Islands are located near the south end of the Florida peninsula on the Gulf Coast, west of the Everglades Indian Key Pass - Ten Thousand Islands. The Ten Thousand Islands are a chain of islands and mangrove islets off the coast of southwest Florida, between Cape Romano (at the south end of Marco Island) and the mouth of the Lostmans River.