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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.
The institute has its origins in department of Geology at University of Delhi, after being shifted to Dehradun it was initially named as the Institute of Himalayan Geology, renamed in 1976 as the Wadia Institute of Himalayan Geology in memory of its founder, late Prof. Darashaw Nosherwan Wadia (F.R.S. and National Professor), in honor to his contributions to the geology of the Himalayas.
Anil Kumar Gupta (born 1960) is a scientist and researcher from India who served as a Professor in the departments of geology and geophysics at the Indian Institute of Technology Kharagpur. [1] He was also the director of the Wadia Institute of Himalayan Geology, in Dehradun, India, from 2010 to 2017.
Himalaya is a type locality for the study of on-going continent-continent collision tectonics. The Himalayan arc extends about 2,400 km (1,500 mi) from Nanga Parbat (8,138 m (26,699 ft)) by the Indus River in northern Pakistan eastward to Namche Barwa (7,756 m (25,446 ft)) by the gorge of the Tsangpo-Brahmaputra in eastern Tibet. [1]
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 ...
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 ...
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 ...
Wadia Institute of Himalayan Geology This page was last edited on 8 November 2023, at 16:08 (UTC). Text is available under the Creative Commons Attribution ...