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Iranian plateau

Geological feature in Asia

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Carte des chaînes du plateau d’Iran
Élisée Reclus · Public domain

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Through Geology, Central Asia and South Asia

As a historical region, it includes Parthia, Media, Persis, and some of the previous territories of Greater Iran. The Zagros form the plateau's western boundary, and its eastern slopes may also be included in the term. The Encyclopædia Britannica excludes "lowland Khuzestan" explicitly and characterizes Elam as spanning "the region from the Mesopotamian plain to the Iranian Plateau".

Stretching from the Caspian Sea in the northwest to the Sulaiman Mountains in the southeast, the Iranian Plateau extends nearly 2,000 kilometres (1,200 mi). It encompasses the majority of Iran, all of Afghanistan, and the parts of Pakistan that are situated to the west of the Indus River, covering an area of some 3,700,000 square kilometres (1,400,000 sq mi). In spite of being called a plateau, it is far from flat, and contains several mountain ranges; its highest point is Noshaq in the Hindu Kush at 7,492 metres (24,580 ft), and its lowest point is the Lut Desert to the east of Kerman, Iran, at below 300 metres (980 ft).

Geology

In geology, the plateau region of Iran primarily formed from the accretionary Gondwanan terranes between the Turan platform to the north and the Zagros fold and thrust belt; the suture zone between the northward moving Arabian plate and the Eurasian continent is the Iranian plateau. It is a geologically well-studied area because of general interest in continental collision zones, and because of Iran's long history of research in geology, particularly in economic geology.

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