
Florida is characterized by a series of ridges, like the Trail Ridge, that run from north to south down the peninsula. These ridges bear abundant marine fossils in their sandy deposits. A new study out of Gainesville indicates that the marine nature of these elevated ridges results from isostatic rise of the land, rather than elevated sea levels. The peninsula, and its ridges, have risen as the result of the lowered density of crust deposits as acidic waters dissolve some of the limestone making them up. As the crust lightens, it's lifted by the mantle beneath. That's till going on, at a rate of about .05 mm per year. Unfortunately, that's not enough of an increase to keep up with rising sea levels, estimated at about 3 mm per year. Enjoy your waterfront property while you can.
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