What is an example of a continental-continental convergent boundary?

A continental-continental convergent boundary occurs when two continental plates collide, often resulting in the formation of mountain ranges due to the intense pressure and uplift generated by the collision. The collision between the Indian Plate and the Eurasian Plate exemplifies this process, leading to the formation of the Himalayas, the world's highest mountain range.

This specific boundary type contrasts with other forms of plate interactions. For instance, the Mid-Atlantic Ridge is a divergent boundary where two tectonic plates move apart, forming new oceanic crust, while the boundary between the Pacific Plate and the North American Plate represents a transform boundary, where plates slide past one another. The Mariana Trench, on the other hand, is an example of an oceanic-continental convergent boundary, where an oceanic plate is subducting beneath a continental plate, resulting in trench formation rather than mountain building. Thus, understanding the nature of plate boundaries is crucial in identifying the geological features produced by these interactions.