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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.
Indian rhinoceros in the Terai. Above the alluvial plain lies the Terai strip, a seasonally marshy zone of sand and clay soils. The Terai has higher rainfall than the plains, and the downward-rushing rivers of the Himalaya slow down and spread out in the flatter Terai zone, depositing fertile silt during the monsoon season and receding in the dry season.
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 some of the Earth's highest peaks, including the highest, Mount Everest.
The Himalayas have three biogeographical provinces – Northwest Himalayas, West Himalayas, Central Himalayas and East Himalayas, which together constitute about 6.4% of the country's area. [2] [13] Tropical rainforests predominate in the Eastern Himalayas while dense subtropical and alpine forests are typical in the Central and Western Himalayas.
The Eastern Himalayas sustain a diverse array of wildlife, including many rare species of fauna and flora. [3] Wildlife in Nepal includes snow leopard in its Himalayan region, and Indian rhinoceros, Asian elephant and water buffalo in the foothills of the Himalayas, making the country one of the world's greatest biodiversity hotspots.
Enayat Ahmad (1 August 1923 – 10 December 1999) was an Indian geographer known for his contribution to the study of the geography of India, especially his interpretation of the evolution of drainage systems in the Himalayas and his writings on tropical coastal geomorphology.
The Main Frontal Thrust (MFT), also known as the Himalayan Frontal Thrust (HFT), is a geological fault in the Himalayas that defines the boundary between the Himalayan foothills and Indo-Gangetic Plain. [1] The fault is well expressed on the surface thus could be seen via satellite imagery.
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 ...