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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 .
Stuart Range from Cashmere Peak. There are at least 64 named mountain ranges in the U.S. state of Washington.Names, elevations and coordinates from the U.S. Geological Survey, Geographic Names Information System and trail guides published by The Mountaineers.
The day before its 1980 eruption, Mount St. Helens was the fifth highest major summit of Washington. Today, Mount St. Helens is the 35th highest major summit of the state. This article comprises three sortable tables of major mountain peaks [1] of the U.S. State of Washington. The summit of a mountain or hill may be measured in three principal ...
The mountains are divided into many parallel sub-ranges (up to 10 or 250 km (6.2 or 155.3 miles) wide), and orogenically have the same age as the Alps. [12] Iran's main oilfields lie in the western central foothills of the Zagros mountain range. The southern ranges of the Fars province have somewhat lower summits, reaching 4,000 metres (13,000 ...
Takht-e Suleyman Mountains Siahsang: 4,604 Takht-e Suleyman Mountains Haft Khan: 4,537 Takht-e Suleyman Mountains Chaloon: 4,516 Takht-e Suleyman Mountains South Siahgook: 4,500 Takht-e Suleyman Mountains Hazaran: 4,501 Central Iranian plateau: Siah-Kaman: 4,472 Takht-e Suleyman Mountains Shaneh-Kuh: 4,465 Takht-e Suleyman Mountains North ...
The mountains also impeded easy access to the Persian Gulf and the Caspian Sea. With an area of 1,648,195 square kilometres (636,372 sq mi), Iran ranks seventeenth in size among the countries of the world. Iran shares its northern borders with several post-Soviet states: Armenia, Azerbaijan, [a] and Turkmenistan. These borders extend for more ...
The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as many of those in the North Cascades , and the notable volcanoes known as the High Cascades .
The Alborz mountain range forms a barrier between the south Caspian and the Iranian plateau. This range is located in northern Iran, parallel to the southern margin of Caspian Sea. Alborz is characterized by the dominance of platform-type sediments, including limestone, dolomite, and clastic rocks.