Folded mountains are majestic features that result from the immense forces of tectonic plate movements. They form when two tectonic plates collide, causing the Earth's crust to crumple and fold. Unlike the imaginary lines of the prime meridian and equator, folded mountains are tangible geological formations that shape landscapes.
Some important points about folded mountains include:
- They often form at convergent plate boundaries, where two plates push against each other.
- The process of folding creates distinct, often sharp, ridges in the landscape, leading to breathtaking terrains.
- Examples of folded mountains include the Himalayas, the Alps, and the Andes.
Folded mountains are crucial to understanding Earth's geological activity and the processes that have shaped the planet over millions of years. Unlike the prime meridian and equator, which are concepts used for orientation and mapping, folded mountains have a profound, physical presence and influence on our surroundings.