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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.
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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. The range has several peaks exceeding an elevation of 8,000 m (26,000 ft) including Mount Everest, the highest mountain on ...
Accordingly K2 is only in the table below for reference and not shown on the map on this page. The interactive map on this page ranks Himalayan peaks above 7,500 m (24,600 ft) and is more inclusive. A peak has a different definition to a mountain and different authorities may use different definitions of either.
The Great Himalayas (also known as Greater Himalayas or Himadri) is one of the four parallel sub-ranges of the Himalayas. [ 1 ] [ 2 ] It is the highest in altitude and extends for about 2,300 km (1,400 mi) from northern Pakistan to the Indian state of Arunachal Pradesh , passing through China , Nepal , and Bhutan .
The Great Himalayan National Park (GHNP) is a national park in India, located in Banjar sub-division of Kullu in the state of Himachal Pradesh. The park was established in 1984 and is spread over an area of 1171 km 2 ; elevations within the park range between 1500 and 6000 m.
The Himalaya orogenic belt the highest elevated mountain range on Earth. In summer, air mass across the South Asia is heated up in general. On the contrary, airmass above the Himalayas and Tibet experiences adiabatic cooling and sinks rapidly, forming an intense high pressure cell. This cell is therefore capable of facilitating landward airflow ...
A geological map of the Himalaya region. The Main Himalayan Thrust underlies the rock units. Diagram showing a décollement. The Main Himalayan Thrust (MHT) is a décollement under the Himalaya Range. This thrust fault follows a NW-SE strike, reminiscent of an arc, and gently dips about 10 degrees towards the north, beneath the region.