enow.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

    From south to north the Himalaya (Himalaya orogen) is divided into 4 parallel tectonostratigraphic zones and 5 thrust faults which extend across the length of Himalaya orogen. Each zone, flanked by the thrust faults on its north and south, has stratigraphy (type of rocks and their layering) different from the adjacent zones.

  3. 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.

  4. Geology of India - Wikipedia

    en.wikipedia.org/wiki/Geology_of_India

    Due to continental drift, the India Plate split from Madagascar and collided with the Eurasian Plate resulting in the formation of the Himalayas.. The earliest phase of tectonic evolution was marked by the cooling and solidification of the upper crust of the earth's surface in the Archaean Era (prior to 2.5 billion years) which is represented by the exposure of gneisses and granites especially ...

  5. Great Trigonometrical Survey - Wikipedia

    en.wikipedia.org/wiki/Great_Trigonometrical_Survey

    Deb Roy, Rama (1986), "The Great Trigonometrical Survey of India in a Historical Perspective" (PDF), Indian Journal of History of Science, 21 (1): 22– 32, archived from the original (PDF) on 25 January 2014; Reginald Henry Phillimore, Historical Records of the Survey of India, 5 vols. Dehra Dun, Survey of India (1945–1968)

  6. Main Central Thrust - Wikipedia

    en.wikipedia.org/wiki/Main_Central_Thrust

    the Greater Himalayan Crystalline complex, which is mainly composed by high-grade gneiss and migmatite, fringed below by the Main Central Thrust and the South Tibetan Detachment; and; the Tethyan Himalayan Sequence, mainly composed by Proterozoic to Eocene sediments, deformed in a Paleogene fold-thrust belt, fringed below by the South Tibetan ...

  7. Āryāvarta - Wikipedia

    en.wikipedia.org/wiki/Āryāvarta

    Course of the Ganges river; Ganges-Yamuna doab western part of the green area. The Ganges-Yamuna doab. The Baudhayana Dharmasutra (BDS) 1.1.2.10 (perhaps compiled in the 8th to 6th centuries BCE) declares that Āryāvarta is the land that lies west of Kālakavana, east of Adarsana, south of the Himalayas and north of the Vindhyas, but in BDS 1.1.2.11 Āryāvarta is confined to the doab of the ...

  8. Enayat Ahmad - Wikipedia

    en.wikipedia.org/wiki/Enayat_Ahmad

    The fact that the Himalayan rivers seem to have a longer history as compared to the mountains themselves has been a subject of enduring curiosity. Himalayan rivers like the Indus, Sutlej, and the Brahmaputra have created deep gorges across the mountain range to reach the plains of northern India. They have first flowed parallel to the main axis ...

  9. Indian plate - Wikipedia

    en.wikipedia.org/wiki/Indian_Plate

    The Indian plate (or India plate) is a minor tectonic plate straddling the equator in the Eastern Hemisphere.Originally a part of the ancient continent of Gondwana, the Indian plate broke away from the other fragments of Gondwana and began moving north, carrying Insular India with it. [2]