When an oceanic plate converges with another tectonic plate, the most common outcome is the formation of a subduction zone. In this process, the denser oceanic plate is forced beneath the less dense continental or another oceanic plate. This can lead to various geological features, including:
- Subduction zones: Areas where an oceanic plate is being pushed down into the mantle, creating a trench.
- Volcanic arcs: Associated stratovolcanoes often form on the continental plate above the subduction zone due to the melting of the subducted plate and the rise of magma.
- Earthquakes: Subduction zones are often sites of significant seismic activity.
Therefore, among the options provided, "some kind of subduction zone" is the most accurate description of what occurs when an ocean plate converges with another plate.
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