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The Caribbean plate is a mostly oceanic tectonic plate underlying Central America and the Caribbean Sea off the northern coast of South America. Roughly 3.2 million square kilometres (1.2 million square miles) in area, the Caribbean plate borders the North American plate, the South American plate, the Nazca plate and the Cocos plate.
Burma plate – Minor tectonic plate in Southeast Asia – 1,100,000 km 2 (420,000 sq mi) Caribbean plate – A mostly oceanic tectonic plate including part of Central America and the Caribbean Sea – 3,300,000 km 2 (1,300,000 sq mi) Caroline plate – Minor oceanic tectonic plate north of New Guinea – 1,700,000 km 2 (660,000 sq mi)
The Panama plate is a south-western extension of the Caribbean plate surrounded by five tectonic plates: the South American plate, Caribbean plate, Cocos plate, and Nazca plate, and by the Chortis tectonic block. [2] The plate had once been a piece of volcanic arc that split off from the rest of the Caribbean plate between the late Tertiary and ...
Burma plate – Minor tectonic plate in Southeast Asia; Cocos plate – Young oceanic tectonic plate beneath the Pacific Ocean off the west coast of Central America; Eurasian plate – Tectonic plate which includes most of Eurasia; Explorer plate – Oceanic tectonic plate beneath the Pacific Ocean off the west coast of Vancouver Island, Canada
Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
The Cocos tectonic plate is located along the western edge of Central America. The latter is along the western edge of the Caribbean tectonic plate and can be split into two distinct regimes. [ 3 ] These regimes are demarcated roughly by the Costa Rican - Nicaraguan border and can be differentiated by the different tectonic histories of each ...
The Cocos plate is a young oceanic tectonic plate beneath the Pacific Ocean off the west coast of Central America, named for Cocos Island, which rides upon it. The Cocos plate was created approximately 23 million years ago when the Farallon plate broke into two pieces, which also created the Nazca plate .
It forms part of the tectonic boundary between the North American plate and the Caribbean plate. It is considered the onshore continuation of the Swan Islands Transform Fault and Cayman trench, which run under the Caribbean Sea. [1] Its western end appears not to continue further than its surface trace, [2] where it is covered by Cenozoic ...
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