What geological events happen at the Himalayan mountains?

The Himalayan mountains are primarily shaped by the ongoing collision between the Indian and Eurasian tectonic plates, a process that began around 50 million years ago. This tectonic activity leads to frequent earthquakes and the formation of significant geological features such as deep valleys, high peaks, and extensive fault systems. Additionally, glacial activity in the region contributes to erosion and landscape changes, while landslides are common due to the steep terrain and seismic activity. Overall, the Himalayas are a dynamic and geologically active region.