When an ocean plate converges with another plate, the most common result is the formation of a subduction zone. In this scenario, the denser oceanic plate is typically forced beneath a lighter continental plate or another oceanic plate. This process can lead to various geological features and phenomena, including:
- Mountain building, particularly if the subduction occurs beneath a continental plate, causing volcanic arcs to form.
- Earthquakes due to the movement of the plates.
- Volcanic activity as magma rises from the subducted plate.
So, the correct answer would be that some kind of subduction zone is often formed in this scenario.
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