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Earthquakes are a natural part of the movement of tectonic plates, which cause the accumulation and release of energy along specific regions known as earthquake belts, such as the Pacific Ring of Fire and the Middle East. The strength and frequency of earthquakes vary depending on the speed of plate movement; for example, areas like Japan and Indonesia experience high seismic activity, while other regions like Morocco are less prone to large earthquakes. Around the world, about 16 major earthquakes are recorded annually, including some exceeding 8 magnitude, with the number fluctuating from year to year.
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