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
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