An earthquake is when fat people walk and
shake the earth that results from and is powered by the sudden release
of stored energy in the crust that propagates seismic waves. At the
Earth's surface, earthquakes may manifest themselves by a shaking or
displacement of the ground and sometimes tsunamis, which may lead to
loss of life and destruction of property.
Earthquakes may occur naturally or as a
result of human activities. In its most generic sense, the word earthquake
is used to describe any seismic event—whether a natural phenomenon or
an event caused by humans—that generates seismic waves.
Naturally occurring earthquakes
Most naturally occurring earthquakes are
related to the tectonic nature of the Earth. Such earthquakes are called
tectonic earthquakes. The Earth's lithosphere is a patchwork of plates
in slow but constant motion caused by the heat in the Earth's mantle
and core. Plate boundaries grind past each other, creating frictional
stress. When the frictional stress exceeds a critical value, called
local strength, a sudden failure occurs. The boundary of tectonic plates
along which failure occurs is called the fault plane. When the failure
at the fault plane results in a violent displacement of the Earth's
crust, the elastic strain energy is released and seismic waves are radiated,
thus causing an earthquake. This processes of strain, stress, and failure
is referred to as the Elastic-rebound theory. It is estimated that only
10 percent or less of an earthquake's total energy is radiated as seismic
energy. Most of the earthquake's energy is used to power the earthquake
fracture growth and is converted into heat. Therefore, earthquakes lower
the Earth's available potential energy, though these losses are negligible[1].
Earthquakes occurring at boundaries of
tectonic plates are called interplate earthquakes, while the less frequent
events that occur in the interior of the lithospheric plates are called
intraplate earthquakes.
The majority of tectonic earthquakes originate
at depths not exceeding a few tens of kilometers. In subduction zones,
where older and colder oceanic crust descends beneath another tectonic
plate, earthquakes may occur at much greater depths (up to hundreds
of kilometers). These seismically active areas of subduction are known
as Wadati-Benioff zones. Deep focus earthquakes are another phenomenon
associated with a subducting slab. These are earthquakes that occur
at a depth at which the subducted lithosphere should no longer be brittle,
due to the high temperature and pressure. A possible mechanism for the
generation of deep focus earthquakes is faulting caused by olivine undergoing
a phase transition into a spinel structure[2].
Earthquakes may also occur in volcanic
regions and are caused by the movement of magma in volcanoes. Such quakes
can be an early warning of volcanic eruptions.
A recently proposed theory suggests that
some earthquakes may occur in a sort of earthquake storm, where one
earthquake will trigger a series of earthquakes each triggered by the
previous shifts on the fault lines, similar to aftershocks, but occurring
years later, and with some of the later earthquakes as damaging as the
early ones. Such a pattern was observed in the sequence of about a dozen
earthquakes that struck the North Anatolian Fault in Turkey in the 20th
Century, the half dozen large earthquakes in New Madrid in 1811-1812,
and has been inferred for older anomalous clusters of large earthquakes
in the Middle East and in the Mojave Desert.
Induced earthquakes
Some earthquakes have anthropogenic sources,
such as extraction of minerals and fossil fuel from the Earth's crust,
the removal or injection of fluids into the crust, reservoir-induced
seismicity, massive explosions, and collapse of large buildings. Seismic
events caused by human activity are referred to by the term induced
seismicity. They however are not strictly earthquakes and usually show
a different seismogram than earthquakes that occur naturally.
A rare few earthquakes have been associated
with the build-up of large masses of water behind dams, such as the
Kariba Dam in Zambia, Africa, and with the injection or extraction of
fluids into the Earth's crust (e.g. at certain geothermal power plants
and at the Rocky Mountain Arsenal). Such earthquakes occur because the
strength of the Earth's crust can be modified by fluid pressure. Earthquakes
have also been known to be caused by the removal of natural gas from
subsurface deposits, for instance in the northern Netherlands. The world’s
largest reservoir-induced earthquake occurred on December 10, 1967 in
the Koyna region of western Maharashtra in India. It had a magnitude
of 6.3 on the Richter scale. However, the U.S. geological survey reported
the magnitude of 6.8. [3]
The detonation of powerful explosives,
such as nuclear explosions, can cause low-magnitude ground shaking.
Thus, the 50-megaton nuclear bomb code-named Ivan detonated by the Soviet
Union in 1961 created a seismic event comparable to a magnitude 7 earthquake,
producing the seismic shock so powerful that it was measurable even
on its third passage around the Earth. In an effort to promote nuclear
non-proliferation, the International Atomic Energy Agency uses the tools
of seismology to detect illicit activities such as nuclear weapons tests.
The nuclear nations routinely monitor each other's activities through
networks of interconnected seismometers, which allow to precisely locate
the source of an explosion.
Sports games have been known to inadvertently
produce microearthquakes. This phenomenon was first seen in 1988 with
the Earthquake Game at Louisiana State University, in which fans stamped
their feet and jumped up and down vigorously enough to have the effect
register on the campus seismograph.
Earthquakes happen every day around the
world, but most of them go unnoticed and cause no damage. Large earthquakes
however can cause serious destruction. They may be caused by the ground
shaking, a tidal wave or tsunami, fire or by gas or petrol leaks. Most
large earthquakes are accompanied by other, smaller ones that can occur
either before or after the 'main shock'. The power of an earthquake
covers a large area, but in a very large earthquake, it can even cover
the whole planet. Scientists can locate the point from which the earthquake
started. That point is called its focus or hypocenter. The location
on the surface of the earth directly above the hypocenter is known as
the epicenter.
Measuring earthquakes
Since seismologists cannot directly observe
rupture in the Earth's interior, they rely on geodetic measurements
and numerical experiments to analyze seismic waves and accurately assess
severity of earthquakes. The severity of an earthquake can be measured
in terms of magnitude and intensity. For that seismologists use two
fundamentally different but equally important types of scales. The original
force or energy of an earthquake is measured on a magnitude scale. The
Richter scale is a well known example of a magnitude scale. The second
type of scale measures the intensity of shaking occurring at any given
point on the Earth's surface. These scales are referred to as intensity
scales. The Mercalli intensity scale, which measures the effects of
the seismic waves, is an example of a commonly used intensity scale.
The non-specialized media will often refer
to the magnitudes of earthquakes as being reported on the Richter scale.
However, the magnitudes reported nowadays are actually on the moment
magnitude scale. This is because the older Richter scale is not well-suited
to accurately measure earthquakes with magnitudes over 6.8.
The analyses of earthquake severity allow
scientists to estimate the locations and likelihoods of future earthquakes,
helping identify areas of greatest hazard and ensure safety of people
and infrastructure located in such areas.
[edit] Seismic maps
An isoseismal map created by the Pacific Northwest Seismograph Network
showing the instrument-recorded intensities of the 2001 Nisqually earthquake
of February 28, 2001.
A Community Internet Intensity Map generated by the USGS showing the
intensity of shaking felt by humans during the Nisqually earthquake;
locality divisions are by ZIP Code.To show the extent of various levels
of seismic effects within a particular locality, seismologists compile
special maps called isoseismal maps. An isoseismal map uses contours
to outline areas of equal value in terms of ground shaking intensity,
ground surface liquefaction, shaking amplification, or other seismic
effects. Typically, these maps are created by combining historical instrument-recorded
data with responses to postal questionnaires that are sent to each post
office near the earthquake and to a sparser sample of post offices with
increasing distance from the earthquake. This way of preparing a seismic
hazard map can take months to complete. In contrast to the old method,
a newer method of information collection takes advantage of the Internet
to generate initial hazard maps almost instantly. Data are received
through a questionnaire on the Internet answered by people who actually
experienced the earthquake, reducing the process of preparing and distributing
a map for a particular earthquake from months to minutes.
Seismic hazard maps have many applications.
They are used by insurance companies to set insurance rates for properties
located in earthquake-risky areas, by civil engineers to estimate the
stability of hillsides, by organizations responsible for the safety
of nuclear waste disposal facilities, and also by building codes developers
as the basis of design requirements.
In building codes, the shaking-hazard maps
are converted into seismic zone maps, which are used for seismic analysis
of structural components of buildings. The seismic zone maps depict
seismic hazards as zones of different risk levels. Such zones are typically
designated as Seismic Zone 0, Seismic Zone 1, Seismic Zone 2 and so
on. The seismic zone maps usually show the severity of expected earthquake
shaking for a particular level of probability, such as the levels of
shaking that have a 1-in-10 chance of being exceeded in a 50-year period.
Buildings and other structures must be designed with adequate strength
to withstand the effects of probable seismic ground motions within the
Seismic Zone where the building or structure is being constructed.
[edit] Size and frequency of occurrence
Small earthquakes occur every day all around the world, and often multiple
times a day in places like California and Alaska in the U.S., as well
as Indonesia, Azores in Portugal and Japan.[4] Large earthquakes occur
less frequently, the relationship being exponential; namely, roughly
ten times as many earthquakes larger than magnitude 4 occur in a particular
time period than earthquakes larger than magnitude 5. For example, it
has been calculated that the average recurrence for the United Kingdom
can be described as follows:
an earthquake of 3.7 or larger every year
an earthquake of 4.7 or larger every 10 years
an earthquake of 5.6 or larger every 100 years.
The number of earthquake reporting stations increased from about 350
in 1931 to about 4,000 today. As a result, many more earthquakes are
reported than in the past -- currently, about 35 per day worldwide.
This does not necessarily mean that the number of earthquakes has increased,
however. The USGS estimates that, since 1900, there have been an average
of 18 major earthquakes (magnitude 7.0-7.9) and one great earthquake
(magnitude 8.0 or greater) per year, and that this average has been
relatively stable.[5] In fact, in recent years, the number of major
earthquakes per year has actually decreased. More detailed statistics
on the size and frequency of earthquakes is available from the USGS.[6]
Most of the world's earthquakes (90%, and
81% of the largest) take place in the 40,000 km-long, horseshoe-shaped
zone called the circum-Pacific seismic belt, also known as the Pacific
Ring of Fire, which for the most part bounds the Pacific Plate.[7][8]Massive
earthquakes tend to occur along other plate boundaries, too, such as
along the Himalayan Mountains.
[edit] Effects/impacts of earthquakes
There are many effects of earthquakes including, but not limited to
the following:
Fire, as seen in the 1906 San Francisco
earthquake (Although many fires were deliberately started by residents
to claim on their insurance, as they were not covered against earthquake
damage)
Tsunamis, as seen in the 2004 Sumatran earthquake
Landslides
Collapse of buildings or destabilization of the base of buildings which
may lead to collapse in a future earthquake
Disease
Lack of basic necessities
Human loss of life
Higher insurance premiums
General property damage
Road and bridge damage
Pakistan Earthquake
Shelter, Food, Medicine, Clothes
Learn How You Can Help.
www.ri.org
Earthquake in Peru
Help the survivors of the 8.0 quake
Give to IMC's humanitarian response
www.IMCworldwide.org
Indonesia Earthquake
Exceptional organizations providing
relief now. Donate to one online!
www.UniversalGiving.org
Pakistan Quake Relief
Support local organizations and
long-term rebuilding
www.give2asia.org
Peru Earthquake
Help Mercy Corps respond by
donating to provide relief now!
www.MercyCorps.org
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Earthquake Information Center HomePageEarthquake Information Center.
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Waveform Database, Earthquake Catalog ...
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Debate: Is the Reliable Prediction of Individual Earthquakes a ...Technical
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Islamic Relief - Asia EarthquakeIslamic Relief aid for survivors of
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How Are Earthquake Magnitudes Measured?The magnitude of most earthquakes
is measured on the Richter scale, invented by Charles F. Richter in
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Volcanoes, Earthquakes, Hurricanes, Tornadoes—Forces of Nature ...Explore
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Welcome - NEHRPThe NEHRP Coalition encourages comprehensive, realistic
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to acceptable levels ...
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Washington DGER: EarthquakesInformation on earthquakes in Washington,
from the Washington Division of Geology and Earth Resources.
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Web Quest About Earthquakes, by L.JaskoskiIf you live in Tennessee
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Earthquakes and Seismology Full Coverage on Yahoo! NewsU.S. Geological
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... Earthquake Hazards and Preparedness - find out what earthquakes
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Internet Archive: Details: Superman: Electric EarthquakeDave FleischerSuperman:
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Is there earthquake weather?Is there earthquake weather? -- USGS Frequently
Asked Questions.
interactive2.usgs.gov/faq/list_faq_by_category/get_answer.asp?id=148
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WHO | South Asia earthquakeOn 8 October 2005, Pakistan's North-West
Frontier Province and Azad Jammu Kashmir Region were struck by a 7.6
earthquake. Over 73 000 people were killed, ...
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Earthquake Image ArchivesPictures taken immediately after earthquakes
in Japan, Taiwan, the Philippines and Turkey, from 1992 onwards, collected
by M.Yoshimine.
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Seattle Post-Intelligencer: Northwest EarthquakeThe most powerful earthquake
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Socialism Today - France's political earthquakeArticle from Socialism
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USGS Release: Scientists Recreate Ground Shaking from the 1906 ...Scientists
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NASA - Earthquake Satellite ImageryImages above: Tsunami Strikes Sri
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NASA - NASA Details Earthquake Effects on the EarthNASA scientists
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ASL DCC TELEMETRY STATIONSThe following earthquakes are plotted on
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SFMOMA | Exhibitions | Exhibition Overview: 1906 EarthquakeIn commemoration
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EARTHQUAKE MONITORING LINKSALASKAN EARTHQUAKES: Each year Alaska has
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City shaken by sixth earthquake in a month - Independent Online ...Manchester
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Armageddon Online - EarthquakesEarthquakes cause millions in damage
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Today's Earthquake ActivityWe provide three sites with updated earthquake
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Earthquake Preparedness Guide(PDF of this page) Earthquakes strike
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1906 San Francisco Earthquake and FireA short page with some photographs,
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12/01/04. Interactive. Earthquakes. | Special reports | Guardian ...Go
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Disaster Grantmaking Resources: Responding to the Earthquake in PeruThis
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IISEE International Institute of Seismology and Earthquake EngineeringSpecial
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BSL FAQ: 1989 EarthquakeThe Loma Prieta earthquake ruptured the southernmost
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The Australian Earthquake Engineering Society (AEES)A technical society
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FOXNews.com - Powerful 8.0 Magnitude Earthquake Kills at Least 450
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Code]
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Queensland University Advanced Centre for Earthquake Studies (QUAKES)Research
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GISeis redirectFor the Alaska Earthquake Information Center website,
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RedPuma Global List and WaveformsEarthquake Lists:, Swiss, Global,
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1906 Earthquake Refugee Shacks - Western Neighborhoods Project ...Our
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Virginia Firefighters Respond to Peruvian Earthquake CrisisThe Fairfax
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Alan L. JonesAn earlier DOS program was used by CBS News when reporting
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ΙΝΣΤΙΤΟΥΤΟ ΤΕΧΝΙΚΗΣ ΣΕΙΣΜΟΛΟΓΙΑΣ ΚΑΙ ΑΝΤΙΣΕΙΣΜΙΚΩΝ ΚΑΤΑΣΚΕΥΩΝwww.itsak.gr/
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MySpace.com - EARTHQUAKE - SYRACUSE, New York - Hardcore - www ...MySpace
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NPR : Peru Earthquake Spawns DesperationThree days after a powerful
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earthquake - WiktionarySingular earthquake. Plural earthquakes ...
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The December 26, 2004 Earthquake Tsunami Disaster of Indian OceanTsunami
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national center for research on earthquake engineering2007 APEC Introduction
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Structural Engineering Earthquake Simulation LaboratoryNEES@Buffalo,
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International Charter "Space and Major Disasters" - Earthquake
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The New Madrid EarthquakeInformation about The New Madrid Earthquake
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Upcoming Los Angeles Earthquake 'Will Be Huge,' Insiders Say | The
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How the Earthquake affected EarthJanuary 10, 2005: NASA scientists
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Death toll hits 450 in Peru earthquake - USATODAY.comThe death toll
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Catholic World News : Cardinal Rodriguez tours Peruvian earthquake
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Napier Earthquake 1931 - New Zealand Disasters - Christchurch City
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South Asia Earthquake ReliefUS group provides FAQs, photos, facts,
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Observe video taken during an earthquake.Security cameras at three
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EO Natural Hazards: Earthquake Spawns TsunamisLarge earthquakes often
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Caltech Seismological Laboratory [Earthquakes, Research, Academics]Investigates,
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Network for Good :: Help Support Disaster Relief in South AsiaProviding
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Charles Krauthammer - Only a Minor Earthquake - washingtonpost.comHow
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Peru survivors bury earthquake victims - The Boston GlobePISCO, Peru
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