When two continental plates converge, they can form a geologic feature known as a continental collision zone or a continental suture. In this type of boundary, the plates move towards each other, and as they collide, the force of their movement causes the plates to crumple and fold, forming mountain ranges and other geologic features.
One example of a continental collision zone is the Himalayan mountain range in Asia, which was formed by the collision of the Indian and Eurasian plates. As the Indian plate moved northwards towards the Eurasian plate, it was forced to crumple and fold, creating the massive peaks and valleys that make up the Himalayas. The process of collision and folding is ongoing and continues to this day, leading to the gradual uplift and growth of the mountain range.
Other examples of continental collision zones include the Alps in Europe, the Andes in South America, and the Appalachian Mountains in North America. These mountain ranges were all formed by the collision of continental plates and are characterized by their high peaks, steep slopes, and complex geological structures.