Report Text Earthquake
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At the Earth’s surface, earthquakes manifest themselves by shaking
and sometimes displacement of the ground. When the epicenter of a large
earthquake is located offshore, the seabed may be displaced sufficiently
to cause a tsunami. Earthquakes can also trigger landslides, and
occasionally volcanic activity.
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Earthquake
An earthquake (also known as a quake, tremor or temblor) is the result
of a sudden release of energy in the Earth’s crust that creates seismic
waves. The seismicity or seismic activity of an area refers to the
frequency, type and size of earthquakes experienced over a period of
time. Earthquakes are measured using observations from seismometers. The
moment magnitude is the most common scale on which earthquakes larger
than approximately 5 are reported for the entire globe. The more
numerous earthquakes smaller than magnitude 5 reported by national
seismological observatories are measured mostly on the local magnitude
scale, also referred to as the Richter scale. These two scales are
numerically similar over their range of validity. Magnitude 3 or lower
earthquakes are mostly almost imperceptible and magnitude 7 and over
potentially cause serious damage over large areas, depending on their
depth. The largest earthquakes in historic times have been of magnitude
slightly over 9, although there is no limit to the possible magnitude.
The most recent large earthquake of magnitude 9.0 or larger was a 9.0
magnitude earthquake in Japan in 2011 (as of March 2011), and it was the
largest Japanese earthquake since records began. Intensity of shaking
is measured on the modified Mercalli scale. The shallower an earthquake,
the more damage to structures it causes, all else being equal.
In its most general sense, the word
earthquake is used to describe any seismic event — whether natural or
caused by humans — that generates seismic waves. Earthquakes are caused
mostly by rupture of geological faults, but also by other events such as
volcanic activity, landslides, mine blasts, and nuclear tests. An
earthquake’s point of initial rupture is called its focus or hypocenter.
The epicenter is the point at ground level directly above the
hypocenter.
Taken from: http://en.wikipedia.org/wiki/Earthquake
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