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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 ...
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)
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.
Plate tectonics within Colombia.. Geology of Colombia refers to the geological composition of the Republic of Colombia that determines its geography.Most of the emerged territory of Colombia covers vast areas within the South American Plate, whereas much submerged territory lies within the Caribbean Plate and the Nazca Plate.
Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]
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 ...
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