Search results
Results from the WOW.Com Content Network
Plateaus of Asia, areas of a highland consisting of flat terrain, that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified ...
The Tibetan Plateau, [a] also known as Qinghai–Tibet Plateau [b] and Qing–Zang Plateau, [c] is a vast elevated plateau located at the intersection of South, Central, and East Asia. [d] Geographically, it is located to the north of Himalayas and the Indian subcontinent, and to the south of Tarim Basin and Mongolian Plateau.
Category: Plateaus of Asia by country. 7 languages. ... Plateaus of Yemen (1 P) This page was last edited on 26 December 2016, at 21:37 (UTC). ...
Tibetan Plateau and surrounding areas above 1600 m – topography. [70] [71] Tibet is often called the "roof of the world". Himalayas, on the southern rim of the Tibetan plateau. All of modern China, including Tibet, is considered a part of East Asia. [72] Historically, some European sources also considered parts of Tibet to lie in Central Asia.
Satellite image of the Tibetan Plateau between the Himalayan mountains to the south and the Taklamakan Desert to the north. In geology and physical geography, a plateau (/ p l ə ˈ t oʊ, p l æ ˈ t oʊ, ˈ p l æ t oʊ /; French:; pl.: plateaus or plateaux), [1] [2] also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the ...
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 Tian Shan plateau, stretching 100 to 120 km wide, is located on the northern margin of the Tarim basin between the Kokshaal-Tau mountain chain to the south and the Terskey Alatau mountain chain to the north. The Kokshaal-Tau extends for 570 km from Pik Dankowa in the west to Pik Pobeda in the east-northeast.
The Deccan Plateau is one of the oldest and most stable land formations in the Indian subcontinent. [28] The plateau is marked by rocky terrain with an average of about 600 m (2,000 ft). [9] The Deccan Traps consist of multiple layers of igneous rocks, which are more than 2 km (1.2 mi) in thickness.