Mount Everest, the highest peak in the world, is primarily formed through a process known as continental collision. This occurs when two tectonic plates collide, causing the Earth’s crust to buckle and fold, resulting in the uplift of mountains.
In the case of Mount Everest, it is part of the Himalayas, which were formed by the collision of the Indian Plate and the Eurasian Plate. This specific region of mountain formation is categorized as a fold mountain formation, characterized by the extensive folding of the earth’s crust. Over millions of years, the immense pressure from these tectonic movements caused the rocks to fold, creating the towering peaks we see today.
Moreover, the ongoing tectonic activity continues to raise Mount Everest slightly each year, making it a dynamic geographic feature. The formation of Mount Everest is a perfect example of how powerful geological forces create some of the most breathtaking landscapes on our planet.