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In geologic terms, the Florida peninsula is relatively young and its soils generally are not as fertile as those in other older parts of the southeastern United States. Nor are the soils of south Florida enriched by river sediments as the soils are in parts of northern Florida.
Beneath the soil of south Florida is limestone, a type of rock formed over millions of years by deposits of shells and bones of sea creatures and chemicals evaporated from shallow sea water. In some places you can see bare limestone at the land surface.
Where water is present much of the year, richer soils develop as a result of decaying vegetation and plant litter. These soils are referred to as organic and are generally found in association with wetlands such as marshes and swamps. Peat is an example of an organic soil found in south Florida.
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