India meets Asia — the Himalaya rise
Racing north, India began to collide with Asia about 50 million years ago, raising the Himalaya and the Tibetan Plateau. India is still pushing north today.

NASA · Public domain · Source
Broken away from Gondwana, India crossed the Tethys Sea northward and began to collide with Asia some 55–50 million years ago (estimates of the timing vary). The sea floor between them was thrust upward and the crust folded layer upon layer, raising the Himalaya and the Tibetan Plateau — which is why the limestone at the summit of Everest holds fossils of sea creatures.
India still pushes into Asia by 4–5 cm a year, so the Himalaya are still slowly rising and great earthquakes are frequent in the region; the 2015 Nepal earthquake came from this movement.