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Technically, an earthquake (also known as tremor, quake or temblor) is a kind of vibration through earth's crust. This vibration occurs as a result of powerful movement of rocks in the earth's crust. These powerful movements trigger a rapid release of energy that creates seismic waves that travel through the earth. Earthquakes are usually brief, but may repeat over a long period of time. (Earth Science. 2001) Earthquakes are classified as large and small. Large earthquakes usually begin with slight tremors but rapidly take form of violent shocks. The vibrations from a large earthquake last for few days known as aftershocks. Small earthquakes are usually slight tremors and do not cause much damage. Large earthquakes are known to take down buildings and cause death and injury (Richter, 1935). According to some statistics, there may be an average of 500,000 earthquakes every year but only about 100,000 can be felt and about 100 or so can cause damage each year.
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