The two important processes in the formation of volcanic arcs at the edge of continental plates are:
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Subduction: This occurs when one tectonic plate is forced beneath another, leading to melting of the subducting plate and the formation of magma, which can result in volcanic activity.
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Uplift: This can occur as a result of tectonic processes including subduction, contributing to the formation of mountain ranges and volcanic arcs.
The other options, "passing over a hotspot" and "plate divergence," are not primarily associated with the formation of volcanic arcs at the edge of continental plates. Passing over a hotspot typically creates volcanic activity away from plate boundaries, while plate divergence generally leads to the formation of mid-ocean ridges rather than volcanic arcs.