Earth's surface is broken into huge pieces called tectonic plates. When two plates push into each other, the land in between can buckle and rise. That slow squeeze builds tall mountains over a very long time. You cannot watch a mountain pop up in one day. The crash is powerful, but the rise is patient. Fold mountains grow where colliding plates force rock upward into the sky.
⚡ DID YOU KNOW?
The Himalayas are still rising because the Indian Plate keeps pushing into the Eurasian Plate.