- Caribbean Plate
The Caribbean Plate is a mostly oceanic
tectonic plate underlyingCentral America and theCaribbean Sea off the north coast ofSouth America .Roughly 3.2 million square kilometers (1.2 million square miles) in area, the Caribbean Plate borders the
North American Plate , theSouth American Plate , theNazca Plate and theCocos Plate . These borders are regions of intense seismic activity, including frequentearthquake s, occasionaltsunami s, [cite journal
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author =Fernández-Arce, Mario & Guillermo Alvarado-Delgado
coauthors =
date =
year = 2005
month = December
title =Tsunamis and Tsunami Preparedness in Costa Rica, Central America
journal =ISET Journal of Earthquake Technology. Paper No. 466.
volume =42
issue =4
pages =203-212
publisher =Indian Society of Earthquake Technology
location =
issn =0972-0405
pmid =
pmc =
doi =
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oclc =
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url =http://home.iitk.ac.in/~vinaykg/Iset466.pdf
language =English
format =pdf
accessdate =2008-08-04
laysummary =
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quote = ] and volcanic eruptions.Boundary types
The northern boundary with the North American plate is a transform or strike-slip boundary which runs from the border area of
Belize ,Guatemala , andHonduras in Central America, eastward through the Cayman trough on south of the southeast coast ofCuba , and just north ofHispaniola ,Puerto Rico , and theVirgin Islands . Part of thePuerto Rico Trench , the deepest part of theAtlantic Ocean (roughly 8,400 meters), lies along this border. The Puerto Rico trench is at a complex transition from the subduction boundary to the south and the transform boundary to the west.The eastern boundary is a
subduction zone , but since the boundary between the North and South American Plates in the Atlantic is as yet undefined, it is unclear which one, or possibly both, is descending under the Caribbean Plate. Subduction forms the volcanic islands of theLesser Antilles island arc from the Virgin Islands in the north to the islands off the coast ofVenezuela in the south. This boundary contains seventeen active volcanoes, most notably Soufriere Hills onMontserrat ,Mount Pelée onMartinique ,La Grande Soufrière onGuadeloupe , Soufrière Saint Vincent on Saint Vincent, and the submarine volcanoKick-'em-Jenny which lies about 10 km north ofGrenada .Along the geologically complex southern boundary the Caribbean Plate interacts with the South American Plate forming
Barbados ,Trinidad (both on the South American Plate) andTobago (on the Caribbean Plate), and islands off the coast of Venezuela (including theLeeward Antilles ) andColombia . This boundary is in part the result of transform faulting along withthrust fault ing and some subduction. The rich Venezuelanpetroleum fields possibly result from this complex plate interaction.The western portion of the plate is occupied by Central America. The Cocos Plate in the
Pacific Ocean is subducted beneath the Caribbean Plate, just off the western coast of Central America. This subduction forms the volcanoes ofGuatemala ,El Salvador ,Nicaragua , andCosta Rica , also known as theCentral America Volcanic Arc .Origin
There are two contending theories as to the origin of the Caribbean Plate.
One holds that it is a
large igneous province that formed in the Pacific Ocean tens of millions of years ago. As the Atlantic ocean widened, North America and South America were pushed westward, separated for a time by oceanic crust. The Pacific Ocean floor subducted under this oceanic crust between the continents. The Caribbean Plate drifted into the same area, but as it was less dense (although thicker) than the surrounding oceanic crust, it did not subduct, but rather overrode the ocean floor, continuing to move eastward relative to North America and South America. With the formation of theIsthmus of Panama 3 million years ago, it ultimately lost its connection to the Pacific.A more recent theory asserts that the Caribbean Plate came into being from an Atlantic hotspot which no longer exists. This theory points to evidence of the absolute motion of the Caribbean Plate which indicates that it moves westward, not east, and that its apparent eastward motion is only relative to the motions of the
North American Plate and theSouth American Plate . [ [http://books.google.com/books?id=RZbjcQEvfN4C&pg=PA7&lpg=PA7&dq=%22plate+boundary%22+north+american+plate+south+american+plate&source=web&ots=Xdfg44f15E&sig=59KVPL0hQLpBDUx9FaCzpg1ko_Q&hl=en "Caribbean Geology Into the Third Millennium: Transactions of the Fifteenth Caribbean Geological Conference", ed. Tervor A Jackson, University of the West Indies Press, 2002] ]ee also
*
List of tectonic plates
*Central America Volcanic Arc
*Earthquakes in Guatemala References
External links
* [http://oceanexplorer.noaa.gov/explorations/03trench/welcome.html NOAA Ocean Explorer]
* [http://www.geo.tu-freiberg.de/~merkel/vorlesung/OS2001/bachmann_raik.pdf Caribbean Plate formation PDF file]
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