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Earthquakes occur due to forces within the Earth's structure. The planet's crust is broken into tectonic plates that float on the mantle, sometimes getting stuck and building pressure at the seams. When plates suddenly slip past each other, it causes the ground to shake and structures to fall. Most quakes happen along areas in the Pacific Ocean called the Ring of Fire. Beyond initial shaking, earthquakes can lead to dangerous secondary events like tsunamis, fires, and landslides that claim thousands of lives annually.




