* Convergent Plate Boundaries: These boundaries occur where two tectonic plates collide. The immense pressure from the collision forces the edges of the plates to buckle, fold, and uplift.

* Continental Crust: Continental crust is thicker and less dense than oceanic crust. When two continents collide, the pressure is so intense that it causes massive mountain ranges to rise. The less dense continental crust is too buoyant to subduct (slide beneath) the other.

Example:

The Himalayas, the tallest mountain range on Earth, were formed by the collision of the Indian and Eurasian tectonic plates. Both plates are composed of continental crust, and the ongoing collision has created the towering peaks we see today.

Other Factors:

While the combination of convergent boundaries and continental crust is crucial, other factors also contribute to mountain formation:

* Rate of Convergence: Faster convergence rates result in more rapid uplift and higher mountains.

* Thickness of the Crust: Thicker crust will produce taller mountains.

* Subduction Zone Activity: If one of the converging plates is oceanic, it can be subducted beneath the continental plate, creating additional uplift and volcanic activity.

Let me know if you'd like to delve deeper into any of these aspects!