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Seismology (from the Greek seismos(σεισμός) = earthquake and λόγος,logos = knowledge ) is the scientific study of earthquakes and the propagation of elastic waves through the Earth. The field also includes studies of earthquake effects, such as tsunamis as well as diverse seismic sources such as volcanic, tectonic, oceanic, atmospheric, and artificial processes (such as explosions). A related field that uses geology to infer information regarding past earthquakes is paleoseismology. A recording of earth motion as a function of time is called a seismogram.

Seismic waves

Earthquakes, and other sources, produce different types of seismic waves which travel through rock, and provide an effective way to image both sources and structures deep within the Earth. There are three basic types of seismic waves in solids: P-waves, S-waves (both body waves) and interface waves. The two basic kinds of surface waves (Rayleigh and Love) which travel along a solid-air interface, can be fundamentally explained in terms of interacting P- and/or S-waves.

Propagation of seismic wave in the ground and the effect of presence of land mine.

Pressure waves (P-waves), are longitudinal waves that travel at maximum velocity within solids and are therefore the first waves to appear on a seismogram.

S-waves, also called Shear waves or secondary waves, are transverse waves that travel more slowly than P-waves and thus appear later than P-waves on a seismogram. Particle motion is perpendicular to the direction of wave propagation. Shear waves do not exist in fluids such as air or water.

Surface waves travel more slowly than P-waves and S-waves, but because they are guided by the surface of the Earth (and their energy is thus trapped near the Earth's surface) they can be much larger in amplitude than body waves, and can be the largest signals seen in earthquake seismograms. They are particularly strongly excited when the seismic source is close to the surface of the Earth, such as the case of a shallow earthquake.

For large enough earthquakes, one can observe the normal modes of the Earth. These modes are excited as discrete frequencies and can be observed for days after the generating event. The first observations were made in the 1960s as the advent of higher fidelity instruments coincided with two of the largest earthquakes of the 20th century - the 1960 Great Chilean earthquake and the 1964 Great Alaskan earthquake. Since then, the normal modes of the Earth have given us some of the strongest constraints on the deep structure of the Earth.

One of the earliest important discoveries (suggested by Richard Dixon Oldham in 1906 and definitively shown by Harold Jeffreys in 1926) was that the outer core of the Earth is liquid. Pressure waves (P-waves) pass through the core. Transverse or shear waves (S-waves) that shake side-to-side require rigid material so they do not pass through the outer core. Thus, the liquid core causes a "shadow" on the side of the planet opposite of the earthquake where no direct S-waves are observed. The reduction in P-wave velocity of the outer core also causes a substantial delay for P waves penetrating the core from the (seismically faster velocity) mantle.

Seismic waves produced by explosions or vibrating controlled sources are the primary method of underground exploration. Controlled source seismology has been used to map salt domes, faults, anticlines and other geologic traps in petroleum-bearing rocks, geological faults, rock types, and long-buried giant meteor craters. For example, the Chicxulub impactor, which is believed to have killed the dinosaurs, was localized to Central America by analyzing ejecta in the cretaceous boundary, and then physically proven to exist using seismic maps from oil exploration.

Using seismic tomography with earthquake waves, the interior of the Earth has been completely mapped to a resolution of several hundred kilometers. This process has enabled scientists to identify convection cells, mantle plumes and other large-scale features of the inner Earth.

Seismographs are instruments that sense and record the motion of the Earth. Networks of seismographs today continuously monitor the seismic environment of the planet, allowing for the monitoring and analysis of global earthquakes and tsunami warnings, as well as recording a variety of seismic signals arising from non-earthquake sources ranging from explosions (nuclear and chemical), to pressure variations on the ocean floor induced by ocean waves (the global microseism), to cryospheric events associated with large icebergs and glaciers. Above-ocean meteor strikes as large as ten kilotons of TNT, (equivalent to about 4.2 × 10¹³ J of effective explosive force) have been recorded by seismographs. A major motivation for the global instrumentation of the Earth with seismographs has been for the monitoring of nuclear testing.

One of the first attempts at the scientific study of earthquakes followed the 1755 Lisbon earthquake. Other especially notable earthquakes that spurred major developments in the science of seismology include the 1906 San Francisco earthquake, the 1964 Alaska earthquake and the 2004 Sumatra-Andaman earthquake. An extensive list of famous earthquakes can be found on the earthquake page.

Earthquake prediction

Most seismologists do not believe that a system to provide timely warnings for individual earthquakes has yet to be developed, and many believe that such a system would be unlikely to give significant warning of impending seismic events. More general forecasts, however, are routinely used to establish seismic hazard. Such forecasts estimate the probability of an earthquake of a particular size affecting a particular location within a particular time span.

Various attempts have been made by seismologists and others to create effective systems for precise earthquake predictions, including the VAN method. Such methods have yet to be generally accepted in the seismology community.

Notable seismologists

Aki, Keiiti
Beroza, Gregory
Bolt, Bruce
Dziewonski, Adam Marian
Galitzine, Boris Borisovich
Gamburtsev, Grigory A.
Gutenberg, Beno
Hutton, Kate
Jordan, Thomas
Jeffreys, Harold
Kanamori, Hiroo
Keilis-Borok, Vladimir
Knopoff, Leon
Lehmann, Inge
Mercalli, Giuseppe
Hanks, Thomas C.
Milne, John
Mohorovičić, Andrija
Oldham, Richard Dixon
Sebastião de Melo, Marquis of Pombal
Press, Frank
Richter, Charles Francis
Zhang Heng

References
ISBN links support NWE through referral fees

ar:علم الزلازل bs:Seizmologija br:Seismologiezh bg:Сеизмология ca:Sismologia cs:Seismologie cy:Seismoleg da:Seismologi de:Seismologie et:Seismoloogia el:Σεισμολογία es:Sismología eo:Sismologio fa:زلزله‌شناسی fr:Sismologie gl:Sismoloxía hy:Սեյսմալոգիա hr:Seizmologija id:Seismologi is:Jarðskjálftafræði it:Sismologia he:סייסמולוגיה lv:Seismoloģija lt:Seismologija ms:Seismologi nah:Tlālolīniliztli nl:Seismologie ja:地震学 no:Seismologi pl:Sejsmologia pt:Sismologia ro:Seismologie ru:Сейсмология sk:Seizmológia sl:Seizmologija sr:Сеизмологија sh:Seizmologija fi:Seismologia sv:Seismologi tl:Seismology th:วิทยาแผ่นดินไหว vi:Địa chấn học tr:Sismoloji uk:Сейсмологія zh:地震学

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-'''Seismology''' (from the [[Greek language|Greek]] ''seismos'' = earthquake and ''λόγος,logos'' = knowledge ) is the scientific study of [[earthquake]]s and the propagation of elastic waves through the [[Earth]].  The field also includes studies of earthquake effects, such as [[tsunamis]] as well as diverse seismic sources such as volcanic, tectonic, oceanic, atmospheric, and artificial processes (such as explosions).  A related field that uses [[geology]] to infer information regarding past earthquakes is [[paleoseismology]].  A recording of earth motion as a function of time is called a [[seismogram]].
+'''Seismology''' (from the [[Greek language|Greek]] ''seismos(σεισμός)'' = earthquake and ''λόγος,logos'' = knowledge ) is the scientific study of [[earthquake]]s and the propagation of [[Linear elasticity#Elastic wave|elastic wave]]s through the [[Earth]].  The field also includes studies of earthquake effects, such as [[tsunamis]] as well as diverse seismic sources such as volcanic, tectonic, oceanic, atmospheric, and artificial processes (such as explosions).  A related field that uses [[geology]] to infer information regarding past earthquakes is [[paleoseismology]].  A recording of earth motion as a function of time is called a [[seismogram]].
-Earthquakes, and other sources, produce different types of [[seismic wave]]s.  These waves travel through rock, and provide an effective way to image both sources and structures deep within the Earth.  There are three basic types of seismic waves in solids: [[P-waves]] and [[S-waves]] (both body waves) and surface waves. The two basic kinds of surface waves ([[Rayleigh wave|Rayleigh]] and [[Love wave|Love]]), can be fundamentally explained in terms of interacting P- and/or S-waves.
+==Seismic waves==
+{{Main|Seismic wave}}
+Earthquakes, and other sources, produce different types of seismic waves which travel through rock, and provide an effective way to image both sources and structures deep within the Earth.  There are three basic types of seismic waves in solids: [[P-waves]], [[S-waves]] (both body waves) and interface waves. The two basic kinds of surface waves ([[Rayleigh wave|Rayleigh]] and [[Love wave|Love]]) which travel along a solid-air interface, can be fundamentally explained in terms of interacting P- and/or S-waves.
+[[Image:Seismic wave prop mine.gif|thumb|right|400px|[[Propagation]] of [[seismic wave]] in the ground and the effect of presence of [[land mine]].]]
-[[Pressure wave]]s, also called Primary waves or P-waves, travel at the greatest velocity within solids and are therefore the first waves to appear on a seismogram.  P-waves are fundamentally pressure disturbances that propagate through a material by alternately compressing and expanding (dialating) the medium, where particle motion is parallel to the direction of wave propagation. For a visual example of this movement,  try laying a coil (like a Slinky) on a flat surface.  Tap lightly on one end, and you will see the coil compress and then expand along the whole length of the coil.  This is a P-wave-like phenomenon.
+[[Pressure wave]]s (P-waves), are [[longitudinal wave]]s that travel at maximum velocity within solids and are therefore the first waves to appear on a seismogram.
-S-waves, also called [[Shear]] [[wave]]s or secondary waves, are [[transverse waves]] that travel more slowly than P-waves and thus appear later than P-waves on a seismogram. Particle motion is perpendicular to the direction of wave propagation. Shear waves do not exist in fluids such as air or water.
+S-waves, also called [[Shear]] [[wave]]s or secondary waves, are [[transverse wave]]s that travel more slowly than P-waves and thus appear later than P-waves on a seismogram. Particle motion is perpendicular to the direction of wave propagation. Shear waves do not exist in fluids such as air or water.
-Surface waves travel more slowly than P-waves and S-waves, however, because they are trapped in the vicinity of the Earth's surface, they can be much larger in amplitude than body waves, and can form the largest signals seen in earthquake seismograms.  They are particularly strongly excited when the seismic source is close to the surface of the Earth.
+Surface waves travel more slowly than P-waves and S-waves, but because they are guided by the surface of the Earth (and their energy is thus trapped near the Earth's surface) they can be much larger in amplitude than body waves, and can be the largest signals seen in earthquake seismograms.  They are particularly strongly excited when the seismic source is close to the surface of the Earth, such as the case of a shallow earthquake.
-For large enough earthquakes, one can observe the [[normal modes]] of the Earth.  These modes are excited as discrete frequencies and can be observed for days after the generating event.  The first observations were made in the 1960s as the advent of higher fidelity instruments coincided with two of the largest earthquakes of the [[20th century]] - the [[Great_Chilean_Earthquake|1960 Great Chilean earthquake]] and the [[Good_Friday_Earthquake|1964 Great Alaskan earthquake]].  Since then, the normal modes of the Earth have given us some of the strongest constraints on the deep structure of the Earth.
+For large enough earthquakes, one can observe the [[normal modes]] of the Earth.  These modes are excited as discrete frequencies and can be observed for days after the generating event.  The first observations were made in the 1960s as the advent of higher fidelity instruments coincided with two of the largest earthquakes of the 20th century - the [[Great Chilean Earthquake|1960 Great Chilean earthquake]] and the [[Good Friday Earthquake|1964 Great Alaskan earthquake]].  Since then, the normal modes of the Earth have given us some of the strongest constraints on the deep structure of the Earth.
-One of the earliest important discoveries (suggested by [[Richard Dixon Oldham]] in 1906 and definitively shown by [[Harold Jeffreys]] in 1926) was that the [[outer core]] of the Earth is [[liquid]].  [[Pressure wave]]s (P-waves) pass through the core. [[Transverse wave|Transverse]] or [[shear]] [[wave]]s (S-waves) that shake side-to-side require rigid material so they do not pass through the outer core.  Thus, the liquid core causes a "shadow" on the side of the planet opposite of the earthquake where no direct S-waves are observed.  The reduction in P-wave velocity of the outer core also causes a substantial delay for P waves penetrating the core from the (sesimically faster velocity) mantle.
+One of the earliest important discoveries (suggested by [[Richard Dixon Oldham]] in 1906 and definitively shown by [[Harold Jeffreys]] in 1926) was that the [[outer core]] of the Earth is [[liquid]].  [[Pressure wave]]s (P-waves) pass through the core. [[Transverse wave|Transverse]] or [[shear]] [[wave]]s (S-waves) that shake side-to-side require rigid material so they do not pass through the outer core.  Thus, the liquid core causes a "shadow" on the side of the planet opposite of the earthquake where no direct S-waves are observed.  The reduction in P-wave velocity of the outer core also causes a substantial delay for P waves penetrating the core from the (seismically faster velocity) mantle.
 Seismic waves produced by [[explosion]]s or vibrating controlled sources are the primary method of underground exploration.  Controlled source seismology has been used to map [[salt dome]]s, faults, anticlines and other geologic traps in [[petroleum]]-bearing [[rock (geology)|rocks]], [[geological fault]]s, rock types, and long-buried giant [[meteor]] [[Impact crater|craters]]. For example, the [[Chicxulub Crater|Chicxulub]] impactor, which is believed to have killed the [[dinosaur]]s, was localized to Central America by analyzing ejecta in the cretaceous boundary, and then physically proven to exist using seismic maps from [[oil exploration]].
-Using [[seismic tomography]] with earthquake waves, the interior of the Earth has been completely mapped to a resolution of several hundred kilometers.  This process has enabled scientists to identify convection cells, [[mantle plume]]s and other large-scale features of the inner Earth.
+<!-- Unsourced image removed: [[Image:hydro-seismic.jpg|right|200px]] —>Using [[seismic tomography]] with earthquake waves, the interior of the Earth has been completely mapped to a resolution of several hundred kilometers.  This process has enabled scientists to identify convection cells, [[mantle plume]]s and other large-scale features of the inner Earth.
-[[Seismograph]]s are instruments that sense and record the motion of the Earth.  Networks of seismographs today continuously monitor the seismic environment of the planet, allowing for the  monitoring and analysis of global earthqaukes and tsunami warnings, as well as recording a variety of seismic signals arising from nonearthquake phenomena such as large meteors entering the atmosphere, pressure variations on the ocean floor induced by ocean waves (the global microseism), [[cryosphere|cryospheric]] events associated with large icebergs and glaciers, or underground nuclear tests.  Above-ocean meteor strikes as large as ten kilotons of TNT, (equivalent to about 4.2 &times; 10<SUP>13</SUP> [[joule|J]] of effective explosive force) have been reported.
+[[Seismograph]]s are instruments that sense and record the motion of the Earth.  Networks of seismographs today continuously monitor the seismic environment of the planet, allowing for the  monitoring and analysis of global earthquakes and tsunami warnings, as well as recording a variety of seismic signals arising from non-earthquake sources ranging from explosions (nuclear and chemical), to pressure variations on the ocean floor induced by ocean waves (the global microseism), to [[cryosphere|cryospheric]] events associated with large icebergs and glaciers. Above-ocean meteor strikes as large as ten kilotons of TNT, (equivalent to about 4.2 &times; 10<SUP>13</SUP> [[joule|J]] of effective explosive force) have been recorded by seismographs.  A major motivation for the global instrumentation of the Earth with seismographs has been for the monitoring of [[nuclear testing]].
 One of the first attempts at the scientific study of earthquakes followed the [[1755 Lisbon earthquake]].  Other especially notable earthquakes that spurred major developments in the science of seismology include the [[1906 San Francisco earthquake]], the [[1964 Alaska earthquake]] and the 2004 [[Sumatra-Andaman earthquake]].  An extensive list of famous earthquakes can be found on the [[earthquake]] page.
 ==Earthquake prediction==
-:''Main article: [[Earthquake prediction]]
+{{main|Earthquake prediction}}
+Most seismologists do not believe that a system to provide timely warnings for individual earthquakes has yet to be developed, and many believe that such a system would be unlikely to give significant warning of impending seismic events. More general forecasts, however, are routinely used to establish seismic hazard. Such forecasts estimate the probability of an earthquake of a particular size affecting a particular location within a particular time span.
-Most seismologists do not believe that a system to provide timely warnings for individual earthquakes has yet been developed, and many believe that such a system would be unlikely to give significant warning of impending seismic events. More general forecasts, however, are routinely used to establish seismic hazard. Such forecasts estimate the probability of an earthquake of a particular size affecting a particular location within a particular time span.
 Various attempts have been made by seismologists and others to create effective systems for precise earthquake predictions, including the [[VAN method]].  Such methods have yet to be generally accepted in the seismology community.
 ==Notable seismologists==
+<!--only add those who have articles in Wikipedia—>
+<div class="references-small" style="-moz-column-count:3; column-count:3;">
 * [[Keiiti Aki|Aki, Keiiti]]
+* [[Gregory Beroza|Beroza, Gregory]]
 * [[Bruce Bolt|Bolt, Bruce]]
 * [[Adam Dziewonski|Dziewonski, Adam Marian]]
@@ Line 38: / Line 44: @@
 * [[Beno Gutenberg|Gutenberg, Beno]]
 * [[Kate Hutton|Hutton, Kate]]
+* [[Thomas Jordan|Jordan, Thomas]]
 * [[Harold Jeffreys|Jeffreys, Harold]]
 * [[Hiroo Kanamori|Kanamori, Hiroo]]
 * [[Vladimir Keilis-Borok|Keilis-Borok, Vladimir]]
+* [[Leon Knopoff| Knopoff, Leon]]
 * [[Inge Lehmann|Lehmann, Inge]]
 * [[Giuseppe Mercalli|Mercalli, Giuseppe]]
+* [[Tom Hanks (seismologist)|Hanks, Thomas C.]]
 * [[John Milne|Milne, John]]
-* [[Andrija Mohorovicic|Mohorovičić, Andrija]]
+* [[Andrija Mohorovičić|Mohorovičić, Andrija]]
 * [[Richard Dixon Oldham|Oldham, Richard Dixon]]
-* [[Vassilis Papazachos|Papazachos, Vassilis]]
 * [[Marquis of Pombal|Sebastião de Melo, Marquis of Pombal]]
 * [[Frank Press|Press, Frank]]
 * [[Charles Francis Richter|Richter, Charles Francis]]
-* [[Panayotis Varotsos|Varotsos, Panayotis]]
 * [[Zhang Heng]]
+</div>
 ==See also==
+<div class="references-small" style="-moz-column-count:3; column-count:3;">
 *[[Catastrophe modeling]]
 *[[Cryoseism]]
+*[[Earthquake engineering]]
 *[[Engineering geology]]
 *[[Geophysics]]
+*[[GNS Science]] (formerly the Institute of Geological and Nuclear Sciences) (in New Zealand)
 *[[Helioseismology]]
 *[[Incorporated Research Institutions for Seismology|The IRIS Consortium]]
 *[[Plate tectonics]]
 *[[Reflection seismology]]
+*[[Seismic loading]]
+*[[Seismic performance analysis]]
 *[[Seismometer]]
 *[[Seismic source]]
 *[[Volcanology]]
+</div>
+==References==
+<!-- ----------------------------------------------------------
+  See http://en.wikipedia.org/wiki/Wikipedia:Footnotes for a
+  discussion of different citation methods and how to generate
+  footnotes using the <ref>, </ref> and  <reference /> tags
+----------------------------------------------------------- —>
+{{reflist}}
+{{reflist}}
+[[Category:Seismology| ]]
-[[Category:Physical_sciences]]
+[[ar:علم الزلازل]]
-[[Category:Earth sciences]]
+[[bs:Seizmologija]]
-{{credits|170549292}}
+[[br:Seismologiezh]]
+[[bg:Сеизмология]]
+[[ca:Sismologia]]
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+[[es:Sismología]]
+[[eo:Sismologio]]
+[[fa:زلزله‌شناسی]]
+[[fr:Sismologie]]
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+[[hr:Seizmologija]]
+[[id:Seismologi]]
+[[is:Jarðskjálftafræði]]
+[[it:Sismologia]]
+[[he:סייסמולוגיה]]
+[[lv:Seismoloģija]]
+[[lt:Seismologija]]
+[[ms:Seismologi]]
+[[nah:Tlālolīniliztli]]
+[[nl:Seismologie]]
+[[ja:地震学]]
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+[[pt:Sismologia]]
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+[[sk:Seizmológia]]
+[[sl:Seizmologija]]
+[[sr:Сеизмологија]]
+[[sh:Seizmologija]]
+[[fi:Seismologia]]
+[[sv:Seismologi]]
+[[tl:Seismology]]
+[[th:วิทยาแผ่นดินไหว]]
+[[vi:Địa chấn học]]
+[[tr:Sismoloji]]
+[[uk:Сейсмологія]]
+[[zh:地震学]]