Primary Earthquake Hazards
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Shifting of the Land Surface
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Earthquakes occur along fault zones in the Earth that may experience relative motion. Rocks that slide against each other in a fault accumulate energy for centuries and release it almost instantaneously. This energy radiates out as a series of waves, causing an earthquake. This ground breaking and shifting of the land's surface is a primary hazard of earthquakes.
Release of Seismic Energy
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Ground shaking is caused by a release of seismic energy, which are waves of energy caused by the sudden breaking of rock within the Earth in the earthquake's epicenter. Ground shaking is a primary hazard of earthquakes. The damage the shaking causes is measured according to its intensity and magnitude on the Richter scale. The largest earthquake recorded had a magnitude of 8.9. Grand shaking causes a multitude of secondary earthquake hazards.
Liquefaction
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Liquefaction occurs in water-saturated, unconsolidated sediment. The ground shaking causes soil grains to lose grain-to-grain contact and the soil tends to flow. Liquefaction is a primary hazard of earthquakes. It produces secondary hazards since it can be damaging to bridges and buildings that lose the ground's support.
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