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The Himalayas, or Himalaya (/ ˌ h ɪ m ə ˈ l eɪ. ə, h ɪ ˈ m ɑː l ə j ə / HIM-ə-LAY-ə, hih-MAH-lə-yə) [b] is a mountain range in Asia, separating the plains of the Indian subcontinent from the Tibetan Plateau.
Diamir, "Naked Mountain" 8,126 26,660 4,608 188.5 Gilgit-Baltistan (GB) region Pakistan [6] [dp 2] 1953: Westernmost peak of Himalayas, rises 7000m above Indus River. 10 Annapurna I "Goddess of the Harvests" 8,100 26,568 2,984 33.9 Central
The Himalayas border the Indo-Gangetic Plain to the south, Pamir Mountains to the west in Central Asia, and the Hengduan Mountains to the east on the China–Myanmar border. From east to west the Himalayas are divided into 3 regions, Eastern Himalaya, Central Himalaya, and Western Himalaya, which collectively house several nations and states.
The Indian Plate is still particularly mobile and these mountain ranges continue to rise in elevation every year and this page may need to be updated in a few years; of these the Himalayas are rising most quickly; the Kashmir and Pamirs region to the north of the Indian subcontinent is the point of confluence of these mountains which encircle ...
The Aravalli-Delhi Orogen is an orogen event that led to a large structural deformation of the Earth's lithosphere (crust and uppermost mantle, such as Aravalli and Himalayas fold mountains) due to the interaction between tectonic plates when a continental plate is crumpled and is pushed upwards to form mountain ranges, and involve a great ...
Illustration of mountains that developed on a fold that thrusted. Mountain formation occurs due to a variety of geological processes associated with large-scale movements of the Earth's crust (tectonic plates). [1] Folding, faulting, volcanic activity, igneous intrusion and metamorphism can all be parts of the orogenic process of mountain ...
The Sub-Himalayan Range (also known as the Cis-Himalaya) is the southernmost mountains in the Himalayas, located on the Indian subcontinent.Their average height varies between 600 and 1,200 meters, and are not so high in altitude as compared to other mountain ranges in the Himalaya range.
Fold mountains form in areas of thrust tectonics, such as where two tectonic plates move towards each other at convergent plate boundary.When plates and the continents riding on them collide or undergo subduction (that is – ride one over another), the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak ...