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Subduction zone earthquakes occur when tectonic plates converge, and one plate is forced beneath another, creating immense stress along the fault interface. Over decades or even centuries, strain accumulates until the rocks can no longer withstand the pressure, resulting in a sudden, violent slip that releases energy as a megathrust earthquake. These earthquakes are among the most powerful on Earth, with recurrence intervals ranging from hundreds to thousands of years, depending on the subductio
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