What features are typically created at convergent boundaries?

Convergent boundaries occur where two tectonic plates collide, leading to significant geological features due to the immense pressure and force involved in the interaction. When an oceanic plate converges with a continental plate, the denser oceanic plate is often forced beneath the continental plate in a process known as subduction. This subduction can create deep ocean trenches, which are some of the deepest parts of the ocean.

As the descending plate melts in the mantle, it can lead to the formation of magma, which rises to the surface and contributes to the creation of volcanic arcs. Additionally, when two continental plates collide, they can push up the crust, leading to the formation of mountain ranges. Classic examples of such mountain ranges include the Himalayas, formed by the collision of the Indian and Eurasian plates.

These processes and formations at convergent boundaries are fundamental to the structure of the Earth's geology, distinguishing them as significant features of plate tectonics. The other options refer to features that are not primarily associated with the dynamics and processes that occur at convergent plate boundaries.