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The Iranian plateau The Iranian Plateau from Paleolithic Times to the Rise of the Achaemenid Empire or Persian plateau

(1968). 9780521070980, Cambridge University Press. .
is a spanning parts of the , , , and . It makes up part of the , and is wedged between the and the . The plateau is situated between the to the west, the and the to the north, the Armenian Highlands and the Caucasus Mountains to the northwest, the Strait of Hormuz and the to the south, and the Indian subcontinent to the southeast.

As a historical region, it includes , Media, , and some of the previous territories of . "Old Iranian Online" , University of Texas College of Liberal Arts (retrieved 10 February 2007) 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 as spanning "the region from the to the Iranian Plateau".

Stretching from the Caspian Sea in the northwest to the Sulaiman Mountains in the southeast, the Iranian Plateau extends nearly . It encompasses the majority of , all of , and the parts of that are situated to the west of the , covering an area of some In spite of being called a , it is far from flat, and contains several mountain ranges; its highest point is in the at , and its lowest point is the to the east of , Iran, at below .


Geology
In geology, the plateau region of primarily formed from the accretionary between the Turan platform to the north and the Zagros fold and thrust belt; the suture zone between the northward moving Arabian 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 , particularly in .


Geography
The Iranian plateau in geology refers to a geographical area north of the great belts resulting from the collision of the with the . In this definition, the Iranian plateau does not cover southwestern Iran.

The plateau extends from East Azerbaijan province in northwestern all the way to and west of the . It also includes smaller parts of the , , and .

The northwestern Iranian plateau, where the and converge, is rugged country with higher elevations, a more severe climate, and greater precipitation than are found on the Anatolian plateau. The region is known as the , and the average elevation of its peaks exceeds . , at 5,137 meters (16,854 ft) the highest point in , is located in the Anti-Taurus. is situated in the mountains at an elevation of 1,546 meters (5,072 ft).

The headwaters of major rivers arise in the Anti-Taurus: the east-flowing flows into the , and the south-flowing and join in before flowing into the . Several small streams that flow into the or landlocked Lake Van also originate in these mountains. The begins in the highlands of and flows the length of Pakistan almost tracing the eastern edge of the Iranian plateau.

Southeast Anatolia lies south of the Anti-Taurus Mountains. It is a region of rolling hills and a broad plateau surface that extends into Syria. Elevations decrease gradually, from about 800 meters (2,600 ft) in the north to about 500 meters (1,600 ft) in the south. Traditionally, and are the main crops of the region.


Mountain ranges
The plateau's mountain ranges can be divided into five major :


Northwest Iranian Ranges


Southwest Iranian Ranges


Central Iranian plateau
    • Kūh-e Hazār
    • Kuh-e Jebal Barez


Eastern Iranian Ranges


Balochistan


Rivers and plains


History
The Iranian plateau may have played a major role in the expansion of after the Out of Africa migration, serving as 'population hub' for 'Common Eurasians', where they subsequently diverged into 'Ancient East Eurasians' and 'Ancient West Eurasians' at c. 50,000 years ago, and from where they expanded in two waves during the Initial Upper Paleolithic (c. 45kya) and Upper Paleolithic (c. 38kya) periods respectively. Ancient and modern populations in the Iranian plateau have a similar genetic component to the Ancient West Eurasian lineage which stayed in the 'population hub' (WEC2), but also display some ancestry from and Ancient East Eurasians via contact events starting in the .

In the Bronze Age, stretched across the Zagros mountains, connecting and the Iranian plateau. The kingdoms of , known from sources, may have been located in the central Iranian plateau. In classical antiquity the region was known as , due to the Persian Achaemenid dynasty originating in . The Middle Persian Erān (whence Modern Persian ) began to be used in reference to the state (rather than as an ethnic designator) from the (see Etymology of Iran).


Archaeology
Archaeological sites and cultures of the Iranian plateau include:Y. Majidzadeh, Sialk III and the Pottery Sequence at Tepe Ghabristan. The Coherence of the Cultures of the Central Iranian Plateau, Iran 19, 1981, 141–46.


Flora
The plateau has historical and forests. Oak forests are found around . , , , , , , and are also found, though the latter two are rare. As of 1920, poplar was harvested for making . Elm was used for . Other trees like , cypress, and were used for decorative purposes. Flower wise, the plateau can grow , , and . and Cercis siliquastrum are common, which are both used for .


Fauna
The plateau is abundant with including , , , , , , and . These animals are mostly found in the wooded mountains of the plateau. The shores of the and the house aquatic birds such as , , and . Deer, hedgehogs, foxes, and 22 species of rodents are found in semidesert, and palm squirrels and Asiatic black bears live in Baluchistan.

Wide variety of and such as toads, , , , , racers, rat snakes ( Ptyas), cat snakes ( Tarbophis fallax), and vipers live the region and along the slopes of the Elburz and Zagros mountains. 200 varieties of fish live in the Persian Gulf. Thirty species of the most important commercial fish Sturgeon is found in the Caspian Sea.Zarubezhnaia Aziia: Fizicheskaia geografiia. Moscow, 1956.Petrov, M. P. Iran: Fiziko-geograficheskii ocherk. Moscow, 1955.


Economy
The Iranian plateau harvests trees for making doors, ploughs, and baskets. is grown also. , , , , , , , , and were commonly seen in the 20th century. and are common in warmer areas. Dates, oranges, , , and limes are also grown. Other edibles include and , which were hard to grow until European settlement brought irrigation improvements. Other vegetables include , , , , , , , and .

The plateau also produces , , , , , , , and . The barley is fed mainly to . is grown and made into . and were also seen in the plateau area as of 1920. is grown in the .


See also
  • Biosphere reserves of Iran
  • Geography of Iran
  • List of Iranian four-thousanders


Notes

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