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The geology of the Florida Keys

Oceanus

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Abstract

The Florida reefs have evolved over the last 7000 years during rising sea level. An ancient reef existed from sand shoals on which Miami and Key West are now sited before the last glaciation (100 000 to 125 000 years ago). During the glacial period sea level fell to >300 feet below its present level. Since sea level rose again invading the south Florida shelf again, corals have returned. The bulk of the Florida reef tract is composed of carbonate sand, some coming from corals but most from calcified algae. Future scenarios are considered for the Florida reefs assuming sea level to remain stable or to continue to rise. -J.G.Harvey

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
The geology of the Florida Keys
Series title:
Oceanus
Volume
31
Issue:
1
Year Published:
1988
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Oceanus
First page:
46
Last page:
53
Number of Pages:
8