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The Arabian plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: East, with the Indo-Australian plate, at the Owen fracture zone; South, with the African plate to the west and the Somali plate and the Indo-Australian plate to the east
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]
Indo-Australian plate – Major tectonic plate formed by the fusion of the Indian and Australian plates (sometimes considered to be two separate tectonic plates) – 58,900,000 km 2 (22,700,000 sq mi) Australian plate – Major tectonic plate separated from Indo-Australian plate about 3 million years ago – 47,000,000 km 2 (18,000,000 sq mi)
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 ...
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 principal tectonic plates of the Earth. The sixteen major pieces of crust and uppermost mantle of the Earth, called the lithosphere, and consisting of oceanic and continental crust.
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.
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