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  2. Geology of the Himalayas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Himalayas

    The Tethys Himalaya is an approximately 100-km-wide synclinorium formed by strongly folded and imbricated, weakly metamorphosed sedimentary series. Several nappes, termed the "North Himalayan Nappes", [18] have also been described within this unit.

  3. Geology of Himachal Pradesh - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Himachal_Pradesh

    The geology of Himachal Pradesh is dominated by Precambrian rocks that were assembled and deformed during the India-Asia collision and the subsequent Himalayan orogeny. The Northern Indian State Himachal Pradesh is located in the Western Himalaya (Fig. 1).

  4. Himalayas - Wikipedia

    en.wikipedia.org/wiki/Himalayas

    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. The range has several peaks exceeding an elevation of 8,000 m (26,000 ft) including Mount Everest, the highest mountain on ...

  5. Geology of Nepal - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Nepal

    The Lesser Himalayas is made up mostly of unfossiliferous sedimentary and metasedimentary rocks; such as shale, sandstone, conglomerate, slate, phyllite, schist, quartzite, limestone and dolomite. The rocks range in age from Precambrian to Miocene. The geology is complicated due to folding, faulting, and thrusting and are largely unfossiliferous.

  6. Tibetan Plateau - Wikipedia

    en.wikipedia.org/wiki/Tibetan_Plateau

    The Himalayas as seen from space looking south from over the Tibetan Plateau. In winter, the land cools off quickly, but the ocean maintains the heat longer. The hot air over the ocean rises, creating a low-pressure area and a breeze from land to ocean while a large area of drying high pressure is formed over the land, increased by wintertime ...

  7. South Tibetan Detachment - Wikipedia

    en.wikipedia.org/wiki/South_Tibetan_Detachment

    The Himalaya offers many opportunities to study all factors that go into mountain building such as continental collisions, erosion, and even climatic changes. In order to understand the structural complexity of the Himalaya orogen, understanding the South Tibet detachment is critical to figuring out the exact time and processes involved in the ...

  8. Siachen Glacier - Wikipedia

    en.wikipedia.org/wiki/Siachen_Glacier

    The Siachen Glacier is a glacier located in the eastern Karakoram range in the Himalayas at about , just northeast of the point NJ9842 where the Line of Control between India and Pakistan [ 3 ] [ 4 ] At 76 km (47 mi) long, it is the longest glacier in the Karakoram and second-longest in the world's non-polar areas . [ 5 ]

  9. Lower Himalayan Range - Wikipedia

    en.wikipedia.org/wiki/Lower_Himalayan_Range

    Lower Himalayan Range in Tansen, Nepal with the Great Himalayas in the background. The Lower Himalayan Range, also called the Lesser Himalayas or Himachal, is one of the four parallel sub-ranges of the Himalayas. [1] [2] It has the Great Himalayas to the north and the Sivalik Hills to the south.