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Earthquakes are strong due to the release of accumulated stress along geological faults in the Earth's crust. When tectonic plates shift, they can become locked due to friction, leading to a buildup of energy. Once the stress exceeds the frictional resistance, the stored energy is released in the form of seismic waves, resulting in the shaking we experience during an earthquake. The intensity of an earthquake depends on the amount of energy released and the depth at which it occurs.

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3w ago

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States that sections of active faults that have had few earthquakes are likely to sites of strong earthquakes?

gap hypothesis


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What area along a fault where few earthquakes have happened recently but where strong earthquakes have happened before?

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