Final answer:
At convergent boundaries, you can find earthquakes, mountain building, and volcanic eruptions due to the collision or subduction of tectonic plates.
Step-by-step explanation:
The geological feature that typically occurs at a convergent boundary is characterized by a range of geological phenomena including earthquakes, mountain building, and volcanic eruptions. At convergent boundaries, plates move towards each other, and this can result in one plate sliding beneath the other in a process called subduction, which leads to volcanic activity.
Additionally, the collision of two continental plates can create mountain ranges due to the compression. Mid-ocean ridges, such as the one mentioned, are formed at divergent boundaries where plates are moving apart, not at convergent boundaries.