Sunny Priyan
Earth's crust is made of large tectonic plates that constantly shift and move, leading to collisions.
In certain regions, one plate is forced beneath another, creating intense pressure and geological activity.
When two continental plates collide, they push upwards, forming mountain ranges like the Himalayas.
Collisions between plates can trigger seismic activity, including earthquakes and volcanic eruptions.
When oceanic plates collide, they form deep ocean trenches and can create volcanic islands.
These crustal collisions occur gradually over millions of years, yet have a profound impact in reshaping the Earth's surface.