Bahama Banks
The Bahama Banks are the submerged
Turks Islands, and wholly submerged Mouchoir Bank. Farther southeast are the equally wholly submerged Silver Bank and Navidad Bank north of the Dominican Republic
.
Geologic history and structure
The limestone that comprises the Banks has been accumulating since at least the Cretaceous period, and perhaps as early as the Jurassic; today the total thickness under the Great Bahama Bank is over 4.5 kilometres (2.8 miles).[1] As the limestone was deposited in shallow water, the only way to explain this massive column is to estimate that the entire platform has subsided under its own weight at a rate of roughly 3.6 centimetres (2 inches) per 1,000 years.[1]
The waters of the Bahama Banks are very shallow; on the Great Bahama Bank they are generally no deeper than 25 meters (80 feet).[2] The slopes around them however, such as the border of the
See also
- Oolitic Aragonite Sand - largest deposit of oolitic aragonite sand is found on the Bahamas Banks
- Dean's Blue Hole – Deep water-filled sinkhole in the Bahamas
- Geography of the Bahamas
- Ocean bank – A part of the sea which is shallow compared to its surrounding area
References
- ^ a b c d "Geomorphology from Space, Chapter 6: Coastal Landforms. Plate C-16, 'Great Bahama Bank'". geoinfo.amu.edu.pl. Retrieved March 9, 2006.
- ^ a b Stephen K. Boss, "Geological Research on the Great Bahama Bank" (Accessed 3/9/06) Archived 2006-02-05 at the Wayback Machine
Further reading
- Agassiz, Alexander (1894). A Reconnoissance of the Bahamas and of the Elevated Reefs of Cuba in the Steam Yacht "Wild Duck", January to April 1893. pp. 17–18. OCLC 8310508.
- Harris, Paul (Mitch); Diaz, Mara R.; Eberli, Gregor P. (2019). "The Formation and Distribution of Modern Ooids on Great Bahama Bank". PMID 30089226.