Final answer:
At a convergent boundary between an oceanic plate and a continental plate, subduction occurs where the oceanic plate is forced beneath the continental plate. This leads to the formation of features such as deep ocean trenches, volcanic activity, and mountain belts.
Step-by-step explanation:
Along a convergent boundary between an oceanic plate and a continental plate, the denser oceanic plate is forced beneath the less dense continental plate in a process called subduction. This creates a subduction zone where the oceanic plate descends into the mantle beneath the continental plate. This subduction can result in various geologic features such as deep ocean trenches, volcanic activity, and the formation of linear and curved mountain belts.