When.com Web Search

Search results

  1. Results From The WOW.Com Content Network
  2. Geology of the Himalayas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Himalayas

    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.

  3. Himalayas - Wikipedia

    en.wikipedia.org/wiki/Himalayas

    Despite its greater size, the Himalayas does not form a water divide across its span because of the multiple river systems that cut across the range. While the mountains were formed gradually, the rivers concurrently cut across deeper gorges ranging from 1,500–5,000 m (4,900–16,400 ft) in depth and 10–50 km (6.2–31.1 mi) in width.

  4. Mountain range - Wikipedia

    en.wikipedia.org/wiki/Mountain_range

    The Himalayas contain the highest mountains in the world, including Mount Everest, which is 8,848 metres (29,029 ft) high. [6] Mountain ranges outside these two systems include the Arctic Cordillera, Appalachians, Great Dividing Range, East Siberians, Altais, Scandinavians, Qinling, Western Ghats, Vindhyas, Byrrangas, and the Annamite Range.

  5. The Earth's tectonic plates made the Himalayas — and could ...

    www.aol.com/news/earth-tectonic-plates-made...

    But the ongoing tectonic collision that formed the highest mountains in the world may also be cleaving Tibet in two, according to new research. ... now recognize as the Himalayas. But precisely ...

  6. Himalaya: A Human History - Wikipedia

    en.wikipedia.org/wiki/Himalaya:_A_Human_History

    The book is divided into 20 chapters that cover the emergence of the mountains from the Tethys Sea, the role of the Himalayas in the Puranas, the exploits of British explorers, the Sino-Indian War, and the recent tensions surrounding Sherpa labor and mountaineering on Mount Everest. [1]

  7. Geological history of Earth - Wikipedia

    en.wikipedia.org/wiki/Geological_history_of_Earth

    This took the form of a giant "Pac-Man" with an east-facing "mouth" constituting the Tethys sea, a vast gulf that opened farther westward in the mid-Triassic, at the expense of the shrinking Paleo-Tethys Ocean, an ocean that existed during the Paleozoic. The remainder was the world-ocean known as Panthalassa ("all the sea").

  8. Alpine orogeny - Wikipedia

    en.wikipedia.org/wiki/Alpine_orogeny

    The Alpine orogeny is caused by the continents Africa, Arabia and India and the small Cimmerian Plate colliding (from the south) with Eurasia in the north. Convergent movements between the tectonic plates (the African Plate, the Arabian Plate and the Indian Plate from the south, the Eurasian Plate and the Anatolian Sub-Plate from the north, and many smaller plates and microplates) had already ...

  9. Pre-collisional Himalaya - Wikipedia

    en.wikipedia.org/wiki/Pre-collisional_Himalaya

    Satellite image of the Himalayas Spatial arrangement of the Himalayan tectonostratigraphic zones. Modified from N.R. McKenzie et al 2011 [1]. Pre-collisional Himalaya is the arrangement of the Himalayan rock units before mountain-building processes resulted in the collision of Asia and India.