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The Arabian plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and Indian plates) that have been moving northward in geological history and colliding with the Eurasian 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]
Philippine Sea plate – Oceanic tectonic plate to the east of the Philippines – 5,500,000 km 2 (2,100,000 sq mi) Scotia plate – Minor oceanic tectonic plate between the Antarctic and South American plates – 1,600,000 km 2 (620,000 sq mi)
Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
Map of the Dead Sea Transform showing the main fault segments and motion of the Arabian plate relative to the African plate, [1] from GPS data The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run for about 1,000 km from the Marash triple junction (a junction with the East Anatolian Fault in southeastern Turkey) to the ...
Tectonic plates in Turkey; the Anatolian sub-plate, the African plate, the Arabian plate, and the Eurasian plate. Except for a relatively small portion of its territory along the Syrian border that is a continuation of the Arabian plate , Turkey geologically is part of the great Alpide belt that extends from the Atlantic Ocean to the Himalaya ...
The Persian Gulf Basin (Persian: آبخیز شاخاب پارس, Arabic: حوض الخليج الفارسی) is found between the Eurasian and the Arabian Plate.The Persian Gulf is described as a shallow marginal sea of the Indian Ocean that is located between the south western side of Zagros Mountains and the Arabian Peninsula and south and southeastern side of Oman and the United Arab Emirates.
Lebanon's tectonic history is closely related to the Levant Fracture System, a left-lateral strike-slip fault zone, separating the Arabian Plate from the African Plate.The intracontinental Palmyride fold belt, with a maximum elevation of 1,385 metres (4,544 ft) above sea level, is an important structural feature that dominates much of Lebanon and Syria, extending northeast towards the ...
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