The Himalayan Orogeny refers to the geological process that formed the Himalayas, one of the highest mountain ranges in the world. This orogeny began around 50 million years ago when the Indian Plate collided with the Eurasian Plate. The immense pressure from this collision caused the Earth's crust to fold and uplift, creating the towering peaks we see today. The ongoing tectonic activity continues to shape the region, leading to earthquakes and further geological changes. The Himalayas not only influence local climate patterns but also serve as a vital water source for major rivers in Asia, impacting millions of people living downstream.