An earthquake is a vibration or shock that occurs on the surface of the earth. Earthquakes are usually caused by movement of the earth's crust.
Earthquakes are measured with a seismometer; a device which also records is known as a seismograph.
Most earthquakes result from the release of energy generated by the pressure exerted by a moving plate.
The longer the pressure was becoming enlarged and eventually reach the state where the pressure can not be arrested again by the edge of plate. That's when an earthquake will occur.
At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacing the ground. When a large earthquake epicenter is located offshore, the seabed sometimes suffers sufficient displacement to cause a tsunami. The shaking in earthquakes can also trigger landslides and occasionally volcanic activity.
There is no known way to prevent earthquakes, but it is possible to lessen the impact. The amount of devastation from an earthquake can be greatly diminished by building structures using earthquake resistant design, making the interiors of buildings safe from falling objects, and educating people about earthquake safety.
-Global plate tectonic movement
-Result of the Earthquake
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