The Biscayne Aquifer, named after Biscayne Bay, is a surficial aquifer. It is a shallow layer of highly permeable limestone under a portion of South Florida. The area it underlies includes Broward County, Miami-Dade County, Monroe County, and Palm Beach County, a total of about .
Because the top part of the Biscayne aquifer is the water table, this aquifer is known as an unconfined aquifer. Since it merges with the floor of Biscayne Bay and with the Atlantic Ocean, it is also a coastal aquifer. Both of these factors contribute to its potential contamination. Lowered water tables, primarily from over-pumping, could allow Seawater intrusion without man-made interventions such as dam-like structures that control fresh and salt water levels in canals. Because the aquifer is so close to the surface, it is extremely vulnerable to surface contaminants. A massive saltwater plume is radiating from the Turkey Point Nuclear Generating Station toward wellfields in the aquifer.
The Biscayne Aquifer supplies South Florida metropolitan area with its primary source of fresh water. This area includes most of south Florida (Miami-Dade, Monroe, and parts of Broward Counties) as well was other urban areas stretching from Homestead, Florida to Delray Beach, Florida. Further, water from the Biscayne Aquifer is piped to the Florida Keys.
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