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How are earthquakes at continental plate boundaries different from earthquakes at mid-ocean ridges

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Earthquakes at continental plate boundaries are usually more intense and destructive than earthquakes at mid-ocean ridges. This is because continental plates are thicker and more rigid than oceanic plates, so the energy released during an earthquake is greater. Earthquakes at mid-ocean ridges are usually less intense and less destructive because the plates are thinner and more flexible.

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