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The Lesser Himalaya (LH) tectonic plate is mainly formed by Upper Proterozoic to lower Cambrian detrital sediments from the passive Indian margin intercalated with some granites and acid volcanics (1840 ±70 Ma [17] ). These sediments are thrust over the Sub-himalayan range along the Main Boundary Thrust (MBT).
The Himalaya, located on the southern fringe of the Tibetan Plateau, form a mountain arc (convex toward the south) about 2400 km long and 250-300 km wide; they are bounded by two structural bends on the northwest (Nanga Parbat, the Indus gorge) and northeast (Namcha Barwa, the Tsangpo gorge). The Himalaya are the loftiest and still rising ...
The north-south width varies from 125-250 mi (200-400 km), and the range cover 229,500 sq mi (594,400 sq km) of Earth ’ s area. In height, the range rises to the top of Everest at 29,028 ft (8,848 m) and much of the area is at an elevation of 2.5 mi (4 km) above sea level. The Himalayas are part of a band of mountain ranges that cross the ...
Apr 22, 2024 · The metamorphic rocks of the Great Himalayan range were formed some 500 to 540 million years ago, and emplaced in approximately their current locations 19 to 21 million years ago. This zone is situated between two great thrusts – the Main Central in the south and the Tethyan in the north. The largest outcrops of Central Crystallines are ...
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Metamorphic. sedimentary. The Himalayas, or Himalaya ( / ˌhɪməˈleɪ.ə, hɪˈmɑːləjə / 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.
- 8,848.86 m (29,031.7 ft)
- Himālaya (Sanskrit)
- 2,400 km (1,500 mi)
2 days ago · Himalayan mountain ranges. Himalayas, great mountain system of Asia forming a barrier between the Plateau of Tibet to the north and the alluvial plains of the Indian subcontinent to the south. The Himalayas include the highest mountains in the world, with more than 110 peaks rising to elevations of 24,000 feet (7,300 metres) or more above sea ...
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 range and the Nanga Parbat syntaxis at the western end, are the result of an ongoing orogeny ...
