At a continental-continental convergent boundary

At a continental-continental convergent boundary, two tectonic plates carrying continental crust collide, leading to the formation of mountain ranges and complex geological features. This collision causes intense pressure and results in significant uplift, as neither plate subducts due to their similar densities. The Himalayan range, formed by the convergence of the Indian and Eurasian plates, is a prime example of this geological process. Additionally, such boundaries are often associated with earthquakes due to the stress and strain built up between the colliding plates.