How are mountains formed?

Check out these three massive ways Earth's surface reshapes itself into mountains! First, think of the Continental Crust as huge, rocky slabs. When these plates collide with nowhere to go but *inward*, the pressure is intense. This creates Compression, where the rock layers actually buckle and fold like a squeezed carpet, wrinkling the ground into high peaks. But rock doesn't always bend; sometimes it snaps along Fault Lines. When the crust breaks apart under stress, it creates these sharp cracks in the Earth. Large sections of rock get pushed upward along those cracks, forming Tilted Blocks that look like giant, jagged stairs reaching for the sky. Then there’s the heat! In a Subduction Zone, a heavy oceanic plate sinks deep under a lighter one, melting as it goes. That melted rock pools into a Magma Chamber, building up massive pressure until the hot liquid rises to the surface and erupts into a volcano! It's all about how Earth handles pressure. Tiny Concepts.