Which is a result of convergent boundaries?

Convergent boundaries occur where tectonic plates move toward each other, resulting in several geological phenomena. The subduction of oceanic lithosphere is a key result of these convergent interactions. When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the lighter continental plate, leading to subduction. This process can create deep ocean trenches, volcanic arcs, and intense seismic activity associated with earthquakes.

In contrast, the creation of mid-ocean ridges typically occurs at divergent boundaries, where tectonic plates move apart, generating new oceanic crust. The formation of transform faults happens at transform boundaries, where plates slide past each other horizontally. Since subduction is a direct consequence of the actions at convergent boundaries, it highlights the dynamic interplay of Earth's lithospheric plates.