explain the formation of the Tibetan plateau
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Explanation:
As the crust was mashed, the towering peaks that make up the Himalayas and the Karakoram were gradually pushed up to their dizzying heights. As the collision progressed, material from the lithosphere (the solid outer shell of the planet) below the surface crust was "shoved out" toward the east, as Royden put it.
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The Himalayan mountain range and Tibetan plateau have formed as a result of the collision between the Indian Plate and Eurasian Plate which began 50 million years ago and continues today. ... From about 50-40 Ma the rate of northward drift of the Indian continental plate slowed to around 4-6 cm per year.
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