Earthquakes frequently occur near subduction zones because these regions are characterized by one tectonic plate being forced beneath another. This interaction creates significant stress as the plates grind against each other, leading to the accumulation of strain until it's released as seismic energy in the form of an earthquake. Additionally, the complex geological processes involved, including the melting of the subducting plate and the formation of magma, can further contribute to seismic activity in these areas.
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