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The Eurasian plate is a tectonic plate that includes most of Eurasia (a landmass consisting of the traditional continents of Asia and Europe), with the notable exceptions of the Arabian Peninsula, the Indian subcontinent, and the area east of the Chersky Range in eastern Siberia.
Eurasian plate – Tectonic plate which includes most of Eurasia – 67,800,000 km 2 (26,200,000 sq mi) 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)
Plate tectonics map. The East African Rift (Great Rift Valley) in eastern Africa; The Mid-Atlantic Ridge system separates the North American plate and the South American plate in the west from the African plate and the Eurasian plate in the east; The Gakkel Ridge is a slow spreading ridge located in the Arctic Ocean
The Amurian microplate is a division within the Eurasian plate, with an unknown western boundary, defined on the south by the Qinling suture zone [additional citation(s) needed] in central China and the Baikal Rift Zone and Stanovoy Mountains on the north. [2] The Baikal Rift Zone is considered a boundary between the Amurian Plate and the ...
It is widely accepted that the Indian plate began to approach the Eurasian plate during the Mesozoic times as a result of the break up of Gondwana supercontinent. [ 31 ] In the Mesozoic time, there was an oceanic basin in between the Lhasa block and the North Tibet continental block.
The Iranian plateau [1] or Persian plateau [2] [3] is a geological feature spanning parts of the Caucasus, Central Asia, South Asia, and West Asia.It makes up part of the Eurasian plate, and is wedged between the Arabian plate and the Indian plate.
In plate tectonics, the Eurasian Plate includes Europe and most of Asia but not the Indian subcontinent, the Arabian Peninsula or the area of the Russian Far East east of the Chersky Range. From the point of view of history and culture, Eurasia can be loosely subdivided into Western Eurasia and Eastern Eurasia. [8]
Taiwan has a history of strong earthquakes. [2] The island is located within a complex zone of convergence between the Philippine Sea plate and Eurasian plate.At the location of the earthquake, these plates converge at a rate of 75 millimetres (3.0 in) per year.