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  • It is mainly formed of the central crystallines (granites and gneisses) overlain by metamorphosed sediments [limestone]. {Rock System}
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    Himalayan Ranges: Shiwaliks, Middle Himalayas, Greater Himalayas, Trans-Himalayas & Purvanchal | PMF IAS
    lel to the slope (along the dip). 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. <span>It is mainly formed of the central crystallines (granites and gneisses) overlain by metamorphosed sediments [limestone]. {Rock System} The folds in this range are asymmetrical with steep south slope and gentle north slope giving ‘hog back (a long, steep hill or mountain ridge)’ topography. This mountain arc convexes to


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