Earthquake: Difference between revisions

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	An '''earthquake''' is a trembling or shaking movement of the earth's surface. Earthquakes occur every day, however the vast majority of them are minor and cause no damage. Large earthquakes can cause serious destruction and massive loss of life. Large earthquakes usually have a substantial initial tremour, followed by numerous aftershocks (smaller tremours). The underground point of origin of an earthquake is called its "focus" and the location on the surface directly above the focus is the epicentre.		An '''earthquake''' is a trembling or shaking movement of the earth's surface. Earthquakes occur every day, however the vast majority of them are minor and cause no damage. Large earthquakes can cause serious destruction and massive loss of life. Large earthquakes usually have a substantial initial tremour, followed by numerous aftershocks (smaller tremours). The underground point of origin of an earthquake is called its "focus" and the location on the surface directly above the focus is the epicentre.

	The magnitude and intensity of an earthquake is measured using the ].		The magnitude and intensity of an earthquake used to be measured measured using the ]. Now there are multiple scales used to measure an earthquakes's magnitude and intensity. The scale reported to the public is so close to the ] that the seismologists don't bother to explain the difference.

	Earthquakes typically result from the movement of continental and oceanic plates, as described by ]. Pressures are built up along the boundaries of these plates in regions called '''faults''' until this pressure is released by a slippage of the plates some distance. The resulting release of energy creates a wave in the surrounding terrain, causing it to shake in an earthquake.		Earthquakes typically result from the movement of continental and oceanic plates, as described by ]. Pressures are built up along the boundaries of these plates in regions called '''faults''' until this pressure is released by a slippage of the plates some distance. The resulting release of energy creates a wave in the surrounding terrain, causing it to shake in an earthquake.

Revision as of 05:09, 20 February 2002

An earthquake is a trembling or shaking movement of the earth's surface. Earthquakes occur every day, however the vast majority of them are minor and cause no damage. Large earthquakes can cause serious destruction and massive loss of life. Large earthquakes usually have a substantial initial tremour, followed by numerous aftershocks (smaller tremours). The underground point of origin of an earthquake is called its "focus" and the location on the surface directly above the focus is the epicentre.

The magnitude and intensity of an earthquake used to be measured measured using the Richter scale. Now there are multiple scales used to measure an earthquakes's magnitude and intensity. The scale reported to the public is so close to the Richter scale that the seismologists don't bother to explain the difference.

Earthquakes typically result from the movement of continental and oceanic plates, as described by plate tectonics. Pressures are built up along the boundaries of these plates in regions called faults until this pressure is released by a slippage of the plates some distance. The resulting release of energy creates a wave in the surrounding terrain, causing it to shake in an earthquake.

Some earthquakes are caused by the movement of magma in volcanoes, and such quakes can be an early warning of volcanic eruptions. A rare few earthquakes are caused by the build-up of large masses of water behind dams, such as the Kariba Dam.

Two types of waves are generated during an earthquake, known as "P" and "S" waves. "P" waves are longitudinal waves resulting from the compression of rock, while the "S" waves are tranverse waves caused by up-and-down motions. There is a difference in travel times between the two types of wave, depending on the material travelled through; and "P" waves are damped out in the earth's core. The combination of these factors has allowed scientists both to locate earthquake epicenters precisely, and to determine in general the structure of the earth's interior. The study of this process is known as seismology. This paragraph requires fact-checking and elaboration.