what type of rook formed the central part of the Hilalayas mountain
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metamorphic rocks
The Higher Himalaya, the backbone of the Himalayan mountains, is made up of 10-20 km-thick metamorphic rocks (schist and gneiss) and granites situated at altitudes of 3000 m to over 8000 m. These rocks are Proterozoic-Cambrian age (2,000-500 Ma) and belong to the continental crust of the Indian plate.
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