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The collision of India into Asia 50 million years ago caused the Eurasian Plate to crumple up and override the Indian Plate. After the collision, the slow continuous convergence of the two plates over millions of years pushed up the Himalayas and the Tibetan Plateau to their present heights. Convergent plate boundaries.
There are a few tertiary plates that are considered major and are rifting apart. These are the Capricorn and Indian Plates of the Indo-Australian and the Nubian and Somali Plates associated with the African. Most of the 14 major plates, have 1-5 tertiary plates associated with them. The largest groupings are the Eurasian Plate, which has 17 of these microplates; the Pacific Plate, with 14 tertiary plates, and the Indo-Australian Plate, which has 10 tertiary plates.