Continental india is currently colliding north into continental asia at rate of ~ 2 inches/year producing The Himalayas
The steep Himalayas, which run 2,900 km along the boundary between India and Tibet, are among the most striking and obvious products of plate-tectonic forces. Between 40 and 50 million years ago, two massive landmasses, India and Eurasia, collided as a result of plate movement, giving rise to this enormous mountain range. One plate could not subduct beneath the other due to the roughly same rock density of these two continental landmasses. The only way for the colliding plates to release their pressure was to shove upward, bend the collision zone, and create the jagged Himalayan peaks.
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