The Oceanic and continental plates are colliding at a subduction zone, where the oceanic plate is being subducted beneath the continental plate, leading to volcanic activity.
Based on the image description provided, two lithosphere layers are interacting along their boundaries, with one moving left and the other moving right and down.
This indicates that the lithospheric plates involved are converging. Specifically, volcanic activity above the meeting point suggests a subduction zone, where one plate, typically the oceanic lithosphere, is subducted beneath another plate.
Since the oceanic crust is mentioned to be above the lithosphere on one side, and it gives way to continental crust on the other, this typically results in oceanic-continental convergence.
The oceanic plate is forced below the continental plate and melts into the asthenosphere, leading to volcanic activity.
This scenario matches the process of an oceanic and continental plate colliding, forming a subduction zone, which is often marked by ocean trenches and volcanic arcs.