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Central Iranian Plateau : ウィキペディア英語版
Iranian Plateau

The Persian Plateau, or Iranian Plateau, is a geological formation in Western Asia and Central Asia. It is the part of the Eurasian Plate wedged between the Arabian and Indian plates, situated between the Zagros Mountains to the west, the Caspian Sea and the Kopet Dag to the north, the Armenian Highlands and the Caucasus mountains in the northwest, the Hormuz Strait and Persian gulf to the south and the Indus River to the east in Pakistan.
As a historical region, it includes Parthia, Media, Persis, the heartlands of Iran and some of its recently lost territories.〔(Old Iranian Online ), ''University of Texas College of Liberal Arts'' (retrieved 10 February 2007)〕
The Zagros Mountains form the plateau's western boundary, and its eastern slopes may be included in the term. The Encyclopædia Britannica excludes "lowland Khuzestan" explicitly〔(s.v. "ancient Iran" )〕 and characterizes Elam as spanning "the region from the Mesopotamian plain to the Iranian Plateau".〔(s.v. "Elamite language" )〕
From the Caspian in the northwest to Baluchistan in the south-east, the Iranian Plateau extends for close to 2,000 km. It encompasses the greater part of Iran, Afghanistan and Pakistan west of the Indus River on an area roughly outlined by the quadrangle formed by the cities of Tabriz, Shiraz, Peshawar and Quetta
containing some . In spite of being called a "plateau", it is far from flat but contains several mountain ranges, the highest peak being Damavand in the Alborz at 5610 m, and the Lut basin east of Kerman in Central Iran falling below 300 m.
== Geology ==
In geology, the plateau region of Iran primarily formed of the accretionary Gondwanan terranes between the Turan platform to the north and the Main Zagros Thrust, the suture zone between the northward moving Arabian plate and the Eurasian continent, is called 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 (although Iran's major petroleum reserves are not in the plateau).

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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