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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 .
The geology of Oklahoma is characterized by Carboniferous rocks in the east, Permian rocks in the center and towards the west, and a cover of Tertiary deposits in the panhandle to the west. The panhandle of Oklahoma is also noted for its Jurassic rocks as well.
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The Zayanderud or Zayandehrud (Persian: Zāyanderūd ,زایندهرود; from زاینده [zɑːjændɛ] "fertile" or "life-giver", and رود "river"), also spelled as Zayanderud or Zayanderood, ..., [2] is the largest river of the Iranian Plateau in central Iran.
Higher elevation mountain ridges of the Kuh Rud and Eastern Iran montane woodlands ecoregion, which intrude into the plateau. [4] In the north of the basin is the large Dasht-e Kavir (a salt desert), in the east and south is the Dasht-e Lut (a sand and gravel desert), and there are portions of the plateau covered in large sand dunes. The ...
Situated between the Great Plains and the Ozark Plateau in the Gulf of Mexico watershed, [6] Oklahoma tends to slope gradually downward from its western to eastern boundaries. [ 2 ] [ 7 ] Its highest and lowest points follow this trend, with its highest peak, Black Mesa , at 4,368 feet (1,516 m) above sea level, situated near the far northwest ...
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Central Iran in a broad sense, comprising the whole area between the North and South Iranian ranges. Within the Iranian plate the Central-East Iran microplate is bordered by the Great Kavir Fault in the north, by the Nain–Baft Fault in the west and southwest and by the Harirud Fault in the east. It is surrounded by the Upper Cretaceous to ...