Virtual Field Trip to the Carbonate Sediments of the Florida Keys

The Lower Keys

Big Pine shuttle image

Space shuttle image of part of the Lower Keys, courtesy of NASA.

  • Move cursor over the image to see labelled features
  • Note the strong development of NNW-SSE oriented tidal channels through this part of the Lower Florida Keys
  • These are believed to reflect the pattern of channels between oolite banks, developed in the Pleistocene Miami Oolite, which now forms the solid bedrock
  • There are no oolites forming in the Florida Keys at the present time

Go to:

The Upper Keys

The Middle Keys

The Lower Keys

Florida Bay

The Everglades

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