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Entire structures, including houses and dams, have been known to collapse in an earthquake.
Earthquakes occur along fault lines, which are boundaries of different layers, or plates, of rock masses on the crust and within the Earth. The movement of one immense plate can shift great masses of weight and pressure onto other weaker layers. When this pressure gives way, an earthquake can take place.
An earthquake's power can be measured in two ways: by intensity and magnitude. While intensity of a quake is usually described through people's perceptions and the severity of building destruction, magnitude is measured by using seismographs or devices which detect ground movement...
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