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    Geology of the Himalayas - Wikipedia

    The geology of the Himalayas is a record of the most dramatic and visible creations of the immense mountain range formed by plate tectonic forces and sculpted by weathering and erosion. The Himalayas, which stretch over 2400 km between the Namcha Barwa syntaxis at the eastern end of the mountain … See more

    During Late Precambrian and the Palaeozoic, the Indian subcontinent, bounded to the north by the Cimmerian Superterranes, was part of Gondwana and was separated from Eurasia by the Paleo-Tethys Ocean (Fig. … See more

    One of the most striking aspects of the Himalayan orogen is the lateral continuity of its major tectonic elements. The Himalaya is classically divided into four tectonic units … See more

    Localized geology and geomorphology topics for various parts of the Himalaya are discussed on other pages:
    Geology of Nepal
    Zanskar is a subdistrict of the Kargil district, which lies in the eastern half of the Indian union territory of See more

    Overview image

    The modern day rate of convergence between the Indian and Eurasian plates is measured to be approximately 17 mm/yr. This convergence is accommodated through seismic … See more

     
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  3. Himalayas | Definition, Location, History, Countries, Mountains, …

  4. Introduction to Himalayan tectonics: a modern …

    Geological map of the Himalaya. Fig. 2 . Photograph taken from the Space Shuttle looking west along the Himalaya with the outline of the major structural divisions and major faults of the Himalaya.

  5. Geological map of the Himalaya and distribution of main litho …

  6. Himalayas - Peaks, Glaciers, Rivers | Britannica

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