- The Great Himalaya:
- Also known as Inner Himalaya, Central Himalaya or Himadri.
- Average elevation of 6,100 m above sea level and an average width of about 25 km.
- It is mainly formed of the central crystallines (granites and gneisses) overlain by metamorphosed sediments [limestone].
- The folds in this range are asymmetrical with a steep south slope and a gentle north slope, giving ‘hog back (a long, steep hill or mountain ridge)’ topography.
- This mountain arc convexes to the south just like the other two.
- Terminates abruptly at the syntaxial bends. One in the Nanga Parbat in north-west and the other in the Namcha Barwa in the north-east.
- This mountain range boasts the tallest peaks in the world, most of which remain under perpetual snow.
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