Earthquake

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An earthquake is a sudden, rapid shaking of the Earth's crust caused by the breaking and shifting of rock beneath the Earth's surface.  Shaking as a result of an earthquake can cause buildings and bridges to collapse; disrupt gas, electric, and phone service; and sometimes trigger landslides, avalanches, flashfloods, fires, and huge, destructive oceanwaves (tsunamis).  Buildings with foundations resting on unconsolidated landfill, old waterways, or other unstable soil are most at risk.  Buildings or trailers and manufactured homes not tied to a reinforced foundation anchored to the ground are also at risk since they can be shaken off their mountings during an earthquake.  Earthquakes can occur at any time of the year.  Aftershocks are smaller earthquakes that follow the main shock and can cause further damage to weakened buildings.  After-shocks can occur in the first hours, days, weeks, or even months after the quake.  Be aware that some earthquakes are actually foreshock's, and a larger earthquake might occur.

Ground movement during an earthquake is seldom the direct cause of death or injury.  Most earthquake-related  injuries result from collapsing walls, flying glass, and falling objects as result of the ground shaking, or people trying to move more than a few feet during the shaking.  Much of the damage in earthquakes is predictable and preventable.  We must all work together in our communities to apply our knowledge to building codes, retrofitting programs, hazard hunts, and neighborhood and family emergency plans.  Earthquakes occur most frequently west of the Rocky Mountains, although historically the most violent earthquakes have occurred in the central United States.  All 50 states and all U.S. territories are vulnerable to earthquakes.  Forty-one states or territories are at moderate to high risk.

 

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