* Mountain ranges: This is the most prominent feature. The immense pressure from the colliding plates forces the crust upwards, creating towering mountains like the Himalayas.
* Plateaus: As the crust is pushed upwards, it can also form vast, elevated plateaus, like the Tibetan Plateau.
* Fold mountains: The intense pressure can also cause the crust to buckle and fold, forming intricate mountain ranges.
* Fault lines: The stress of the collision can cause the crust to fracture, creating fault lines. These can be the sites of earthquakes.
* Volcanic activity: While less common than with oceanic-continental collisions, some volcanic activity can occur along the collision zone due to the melting of the lower crust or the subduction of small oceanic plates.
Overall, the collision of two continental plates is a major geological event that shapes the Earth's surface and leads to the formation of some of its most dramatic and impressive landforms.
