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The Floridian Peninsula is a porous plateau of karst limestone sitting atop bedrock known as the Florida Platform.The emergent portion of the platform was created during the Eocene to Oligocene as the Gulf Trough filled with silts, clays, and sands.
From 1513 onward, the land became known as La Florida. After 1630, and throughout the 18th century, Tegesta (after the Tequesta tribe) was an alternate name of choice for the Florida peninsula following publication of a map by the Dutch cartographer Hessel Gerritsz in Joannes de Laet's History of the New World. [22] [23] [24]
The Florida peninsula is located on the eastern side of the platform, where in places it lies only 3 to 4 miles (4.8 to 6.4 km) from the platform's edge. On the gulf side the platform ends over 100 miles (160 km) to the west of the modern shoreline, where a massive cliff rises over 6,000 feet (1,800 m) from the 10,600 feet (3,200 m) depth of ...
The Florida peninsula is a porous plateau of karst limestone sitting atop bedrock known as the Florida Platform. The emergent portion of the platform was created during the Eocene to Oligocene as the Gulf Trough filled with silts, clays, and sands.
Florida (/ ˈ f l ɒr ɪ d ə / ⓘ FLORR-ih-də; Spanish: [floˈɾiða]) is a state in the Southeastern region of the United States.It borders the Gulf of Mexico to the west, Alabama to the northwest, Georgia to the north, the Atlantic Ocean to the east, and the Straits of Florida and Cuba to the south.
The Lake Wales Ridge, sometimes referred to as the Mid-Florida Ridge, [1] is a sand ridge running for about 100 miles (160 km) south to north in Central Florida. Clearly viewable from satellite, the white sands of the ridge are located in Highlands County and Polk County , and also extend north into Osceola , Orange , and Lake Counties .
Satellite images illustrate the scope of the damage in coastal communities along the western part of the Florida peninsula, near the Sarasota barrier island of Siesta Key where Milton made ...
The Dade Subsea was named for Dade County, Florida fossil reefs and is contemporary with the Bainbridge Subsea of North Florida. It is the last platform created from carbonate deposits and the predecessor of the recent Florida peninsula. It was formed out of the meteor impacts and tsunamis of the colder Eocene.