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All of the Asian ranges above have been formed in part over the past 35 to 55 million years by the collision between the Indian Plate and Eurasian Plate. The Indian Plate is still particularly mobile and these mountain ranges continue to rise in elevation every year and this page may need to be updated in a few years; of these the Himalayas are rising most quickly; the Kashmir and Pamirs region to the north of the Indian subcontinent is the point of confluence of these mountains which encircle the Tibetan Plateau.ļ