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VolcanoFrom Wikipedia, the free encyclopedia

This article is about the geological feature. For other uses, see Volcano (disambiguation).

Cleveland Volcano in theAleutian IslandsofAlaskaphotographed from theInternational Space Station, May 2006.

Ashplumes reached a height of 19 km during the climactic eruption at Mount Pinatubo,Philippinesin 1991.

A volcano is an opening, orrupture, in a planet's surface orcrust, which allows hotmagma,volcanic

ashand gases to escape from below the surface.

Volcanoes are generally found wheretectonic platesarediverging orconverging. Amid-oceanic ridge,

for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic

platespulling apart; the Pacific Ring of Fire has examples of volcanoes caused byconvergent tectonic

platescoming together. By contrast, volcanoes are usually not created where two tectonic plates slidepast one another. Volcanoes can also form where there is stretching and thinning of theEarth's crust in

the interiors of plates, e.g., in theEast African Rift, the Wells Gray-Clearwater volcanic fieldand

the Rio Grande Riftin North America. This type of volcanism falls under the umbrella of "Plate

hypothesis" volcanism.[1]Volcanism away from plate boundaries has also been explained asmantle
http://en.wikipedia.org/wiki/Volcano_(disambiguation)http://en.wikipedia.org/wiki/Volcano_(disambiguation)http://en.wikipedia.org/wiki/Mount_Cleveland_(Alaska)http://en.wikipedia.org/wiki/Aleutian_Islandshttp://en.wikipedia.org/wiki/Aleutian_Islandshttp://en.wikipedia.org/wiki/Aleutian_Islandshttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/International_Space_Stationhttp://en.wikipedia.org/wiki/International_Space_Stationhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Mount_Pinatubohttp://en.wikipedia.org/wiki/Mount_Pinatubohttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Rupture_(engineering)http://en.wikipedia.org/wiki/Rupture_(engineering)http://en.wikipedia.org/wiki/Rupture_(engineering)http://en.wikipedia.org/wiki/Crust_(geology)http://en.wikipedia.org/wiki/Crust_(geology)http://en.wikipedia.org/wiki/Magmahttp://en.wikipedia.org/wiki/Magmahttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Tectonic_plateshttp://en.wikipedia.org/wiki/Tectonic_plateshttp://en.wikipedia.org/wiki/Tectonic_plateshttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Mid-oceanic_ridgehttp://en.wikipedia.org/wiki/Mid-Atlantic_Ridgehttp://en.wikipedia.org/wiki/Mid-Atlantic_Ridgehttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Crust_(geology)http://en.wikipedia.org/wiki/East_African_Rifthttp://en.wikipedia.org/wiki/East_African_Rifthttp://en.wikipedia.org/wiki/Wells_Gray-Clearwater_volcanic_fieldhttp://en.wikipedia.org/wiki/Wells_Gray-Clearwater_volcanic_fieldhttp://en.wikipedia.org/wiki/Rio_Grande_Rifthttp://en.wikipedia.org/wiki/Rio_Grande_Rifthttp://en.wikipedia.org/wiki/Volcano#cite_note-Foulger-0http://en.wikipedia.org/wiki/Volcano#cite_note-Foulger-0http://en.wikipedia.org/wiki/Mantle_plumehttp://en.wikipedia.org/wiki/Mantle_plumehttp://en.wikipedia.org/wiki/File:Pinatubo_ash_plume_910612.jpghttp://en.wikipedia.org/wiki/File:Pinatubo_ash_plume_910612.jpghttp://en.wikipedia.org/wiki/File:MtCleveland_ISS013-E-24184.jpghttp://en.wikipedia.org/wiki/File:MtCleveland_ISS013-E-24184.jpghttp://en.wikipedia.org/wiki/Volcano_(disambiguation)http://en.wikipedia.org/wiki/Mount_Cleveland_(Alaska)http://en.wikipedia.org/wiki/Aleutian_Islandshttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/International_Space_Stationhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Mount_Pinatubohttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Rupture_(engineering)http://en.wikipedia.org/wiki/Crust_(geology)http://en.wikipedia.org/wiki/Magmahttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Tectonic_plateshttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Mid-oceanic_ridgehttp://en.wikipedia.org/wiki/Mid-Atlantic_Ridgehttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Crust_(geology)http://en.wikipedia.org/wiki/East_African_Rifthttp://en.wikipedia.org/wiki/Wells_Gray-Clearwater_volcanic_fieldhttp://en.wikipedia.org/wiki/Rio_Grande_Rifthttp://en.wikipedia.org/wiki/Volcano#cite_note-Foulger-0http://en.wikipedia.org/wiki/Mantle_plume


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plumes. These so-called "hotspots", for example Hawaii, are postulated to arise from

upwellingdiapirswith magma from thecore-mantle boundary, 3,000 km deep in the Earth.

Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic

ash can be a threat toaircraft, in particular those withjet engines where ash particles can be melted by

the high operating temperature. Large eruptions can affect temperature as ash and droplets ofsulfuric

acidobscure thesun and cool the Earth's lower atmosphere ortroposphere; however, they also absorb

heat radiated up from the Earth, thereby warming thestratosphere. Historically, so-called volcanic

winters have caused catastrophic famines.

Contents

[hide]

1 Etymology

2 Plate tectonics

o 2.1 Divergent plate boundaries

o 2.2 Convergent plate boundaries

o 2.3 "Hotspots"

3 Volcanic features

o 3.1 Fissure vents

o 3.2 Shield volcanoes

o 3.3 Lava domes

o 3.4 Cryptodomes

o 3.5 Volcanic cones (cinder cones)

o 3.6 Stratovolcanoes (composite volcanoes)

o 3.7 Supervolcanoes

o 3.8 Submarine volcanoes

o 3.9 Subglacial volcanoes

o 3.10 Mud volcanoes

4 Erupted material

o 4.1 Lava composition

o 4.2 Lava texture

5 Volcanic activity

o 5.1 Popular classification of volcanoes

5.1.1 Active

5.1.2 Extinct
http://en.wikipedia.org/wiki/Mantle_plumehttp://en.wikipedia.org/wiki/Hotspot_(geology)http://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Diapirhttp://en.wikipedia.org/wiki/Diapirhttp://en.wikipedia.org/wiki/Core-mantle_boundaryhttp://en.wikipedia.org/wiki/Core-mantle_boundaryhttp://en.wikipedia.org/wiki/Aircrafthttp://en.wikipedia.org/wiki/Aircrafthttp://en.wikipedia.org/wiki/Jet_enginehttp://en.wikipedia.org/wiki/Sulfuric_acidhttp://en.wikipedia.org/wiki/Sulfuric_acidhttp://en.wikipedia.org/wiki/Sulfuric_acidhttp://en.wikipedia.org/wiki/Sunhttp://en.wikipedia.org/wiki/Sunhttp://en.wikipedia.org/wiki/Tropospherehttp://en.wikipedia.org/wiki/Stratospherehttp://en.wikipedia.org/wiki/Volcanic_winterhttp://en.wikipedia.org/wiki/Volcanic_winterhttp://en.wikipedia.org/wiki/Faminehttp://en.wikipedia.org/wiki/Faminehttp://en.wikipedia.org/wiki/Volcanohttp://en.wikipedia.org/wiki/Volcano#Etymologyhttp://en.wikipedia.org/wiki/Volcano#Plate_tectonicshttp://en.wikipedia.org/wiki/Volcano#Divergent_plate_boundarieshttp://en.wikipedia.org/wiki/Volcano#Convergent_plate_boundarieshttp://en.wikipedia.org/wiki/Volcano#.22Hotspots.22http://en.wikipedia.org/wiki/Volcano#Volcanic_featureshttp://en.wikipedia.org/wiki/Volcano#Fissure_ventshttp://en.wikipedia.org/wiki/Volcano#Shield_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Lava_domeshttp://en.wikipedia.org/wiki/Volcano#Cryptodomeshttp://en.wikipedia.org/wiki/Volcano#Volcanic_cones_.28cinder_cones.29http://en.wikipedia.org/wiki/Volcano#Stratovolcanoes_.28composite_volcanoes.29http://en.wikipedia.org/wiki/Volcano#Supervolcanoeshttp://en.wikipedia.org/wiki/Volcano#Submarine_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Subglacial_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Mud_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Erupted_materialhttp://en.wikipedia.org/wiki/Volcano#Erupted_materialhttp://en.wikipedia.org/wiki/Volcano#Lava_compositionhttp://en.wikipedia.org/wiki/Volcano#Lava_texturehttp://en.wikipedia.org/wiki/Volcano#Volcanic_activityhttp://en.wikipedia.org/wiki/Volcano#Popular_classification_of_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Activehttp://en.wikipedia.org/wiki/Volcano#Extincthttp://en.wikipedia.org/wiki/Mantle_plumehttp://en.wikipedia.org/wiki/Hotspot_(geology)http://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Diapirhttp://en.wikipedia.org/wiki/Core-mantle_boundaryhttp://en.wikipedia.org/wiki/Aircrafthttp://en.wikipedia.org/wiki/Jet_enginehttp://en.wikipedia.org/wiki/Sulfuric_acidhttp://en.wikipedia.org/wiki/Sulfuric_acidhttp://en.wikipedia.org/wiki/Sunhttp://en.wikipedia.org/wiki/Tropospherehttp://en.wikipedia.org/wiki/Stratospherehttp://en.wikipedia.org/wiki/Volcanic_winterhttp://en.wikipedia.org/wiki/Volcanic_winterhttp://en.wikipedia.org/wiki/Faminehttp://en.wikipedia.org/wiki/Volcanohttp://en.wikipedia.org/wiki/Volcano#Etymologyhttp://en.wikipedia.org/wiki/Volcano#Plate_tectonicshttp://en.wikipedia.org/wiki/Volcano#Divergent_plate_boundarieshttp://en.wikipedia.org/wiki/Volcano#Convergent_plate_boundarieshttp://en.wikipedia.org/wiki/Volcano#.22Hotspots.22http://en.wikipedia.org/wiki/Volcano#Volcanic_featureshttp://en.wikipedia.org/wiki/Volcano#Fissure_ventshttp://en.wikipedia.org/wiki/Volcano#Shield_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Lava_domeshttp://en.wikipedia.org/wiki/Volcano#Cryptodomeshttp://en.wikipedia.org/wiki/Volcano#Volcanic_cones_.28cinder_cones.29http://en.wikipedia.org/wiki/Volcano#Stratovolcanoes_.28composite_volcanoes.29http://en.wikipedia.org/wiki/Volcano#Supervolcanoeshttp://en.wikipedia.org/wiki/Volcano#Submarine_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Subglacial_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Mud_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Erupted_materialhttp://en.wikipedia.org/wiki/Volcano#Lava_compositionhttp://en.wikipedia.org/wiki/Volcano#Lava_texturehttp://en.wikipedia.org/wiki/Volcano#Volcanic_activityhttp://en.wikipedia.org/wiki/Volcano#Popular_classification_of_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Activehttp://en.wikipedia.org/wiki/Volcano#Extinct


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5.1.3 Dormant

o 5.2 Technical classification of volcanoes

5.2.1 Volcanic-alert level

5.2.2 Volcano warning schemes of the United States

6 Notable volcanoes

7 Effects of volcanoes

8 Volcanoes on other planetary bodies

9 Traditional beliefs about volcanoes

10 See also

11 References

12 Further reading

13 External links

Etymology

The word volcano is derived from the name ofVulcano, a volcanic island in theAeolian Islands of Italy

whose name in turn originates fromVulcan, the name of a god offire inRoman mythology.[2] The study

of volcanoes is called volcanology, sometimes spelled vulcanology.

Plate tectonics

Map showing the divergent plate boundaries (OSR Oceanic Spreading Ridges) and recent sub aerial volcanoes.

Divergent plate boundaries

Main article: Divergent boundary

At themid-oceanic ridges, two tectonic plates diverge from one another. Newoceanic crustis being

formed by hot molten rock slowly cooling and solidifying. The crust is very thin at mid-oceanic ridges

due to the pull of the tectonic plates. The release of pressure due to the thinning of the crust leads
http://en.wikipedia.org/wiki/Volcano#Extincthttp://en.wikipedia.org/wiki/Volcano#Dormanthttp://en.wikipedia.org/wiki/Volcano#Technical_classification_of_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Volcanic-alert_levelhttp://en.wikipedia.org/wiki/Volcano#Volcano_warning_schemes_of_the_United_Stateshttp://en.wikipedia.org/wiki/Volcano#Notable_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Effects_of_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Volcanoes_on_other_planetary_bodieshttp://en.wikipedia.org/wiki/Volcano#Traditional_beliefs_about_volcanoeshttp://en.wikipedia.org/wiki/Volcano#See_alsohttp://en.wikipedia.org/wiki/Volcano#Referenceshttp://en.wikipedia.org/wiki/Volcano#Further_readinghttp://en.wikipedia.org/wiki/Volcano#External_linkshttp://en.wikipedia.org/wiki/Vulcanohttp://en.wikipedia.org/wiki/Vulcanohttp://en.wikipedia.org/wiki/Aeolian_Islandshttp://en.wikipedia.org/wiki/Aeolian_Islandshttp://en.wikipedia.org/wiki/Vulcan_(mythology)http://en.wikipedia.org/wiki/Vulcan_(mythology)http://en.wikipedia.org/wiki/Firehttp://en.wikipedia.org/wiki/Firehttp://en.wikipedia.org/wiki/Roman_mythologyhttp://en.wikipedia.org/wiki/Roman_mythologyhttp://en.wikipedia.org/wiki/Volcano#cite_note-1http://en.wikipedia.org/wiki/Volcano#cite_note-1http://en.wikipedia.org/wiki/Volcanologyhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Mid-oceanic_ridgeshttp://en.wikipedia.org/wiki/Mid-oceanic_ridgeshttp://en.wikipedia.org/wiki/Mid-oceanic_ridgeshttp://en.wikipedia.org/wiki/Tectonic_platehttp://en.wikipedia.org/wiki/Oceanic_crusthttp://en.wikipedia.org/wiki/Oceanic_crusthttp://en.wikipedia.org/wiki/Oceanic_crusthttp://en.wikipedia.org/wiki/File:Spreading_ridges_volcanoes_map-en.svghttp://en.wikipedia.org/wiki/File:Spreading_ridges_volcanoes_map-en.svghttp://en.wikipedia.org/wiki/Volcano#Dormanthttp://en.wikipedia.org/wiki/Volcano#Technical_classification_of_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Volcanic-alert_levelhttp://en.wikipedia.org/wiki/Volcano#Volcano_warning_schemes_of_the_United_Stateshttp://en.wikipedia.org/wiki/Volcano#Notable_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Effects_of_volcanoeshttp://en.wikipedia.org/wiki/Volcano#Volcanoes_on_other_planetary_bodieshttp://en.wikipedia.org/wiki/Volcano#Traditional_beliefs_about_volcanoeshttp://en.wikipedia.org/wiki/Volcano#See_alsohttp://en.wikipedia.org/wiki/Volcano#Referenceshttp://en.wikipedia.org/wiki/Volcano#Further_readinghttp://en.wikipedia.org/wiki/Volcano#External_linkshttp://en.wikipedia.org/wiki/Vulcanohttp://en.wikipedia.org/wiki/Aeolian_Islandshttp://en.wikipedia.org/wiki/Vulcan_(mythology)http://en.wikipedia.org/wiki/Firehttp://en.wikipedia.org/wiki/Roman_mythologyhttp://en.wikipedia.org/wiki/Volcano#cite_note-1http://en.wikipedia.org/wiki/Volcanologyhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Mid-oceanic_ridgeshttp://en.wikipedia.org/wiki/Tectonic_platehttp://en.wikipedia.org/wiki/Oceanic_crust


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toadiabatic expansion, and the partial melting of themantlecausing volcanism and creating new

oceanic crust. Mostdivergent plate boundariesare at the bottom of the oceans, therefore most

volcanic activity is submarine, forming new seafloor.Black smokers or deep sea vents are an example

of this kind of volcanic activity. Where the mid-oceanic ridge is above sea-level, volcanic islands are

formed, for example,Iceland.

Convergent plate boundaries

Main article: Convergent boundary

Subduction zonesare places where two plates, usually an oceanic plate and a continental plate,

collide. In this case, the oceanic plate subducts, or submerges under the continental plate forming a

deep ocean trench just offshore. Water released from the subducting plate lowers the melting

temperature of the overlying mantle wedge, creating magma. This magma tends to be

veryviscousdue to its high silicacontent, so often does not reach the surface and cools at depth.

When it does reach the surface, a volcano is formed. Typical examples for this kind of volcano

areMount Etna and the volcanoes in thePacific Ring of Fire.

"Hotspots"

Main article: Hotspot (geology)

"Hotspots" is the name given to volcanic provinces postulated to be formed by mantle plumes. These

are postulated to comprise columns of hot material that rise from the core-mantle boundary. They are

suggested to be hot, causing large-volume melting, and to be fixed in space. Because the tectonic

plates move across them, each volcano becomes dormant after a while and a new volcano is thenformed as the plate shifts over the postulated plume. TheHawaiian Islandshave been suggested to

have been formed in such a manner, as well as theSnake River Plain, with the Yellowstone

Calderabeing the part of the North American plate currently above the hot spot. This theory is

currently under criticism, however. [1]

Volcanic features
http://en.wikipedia.org/wiki/Adiabatic_processhttp://en.wikipedia.org/wiki/Adiabatic_processhttp://en.wikipedia.org/wiki/Mantle_(geology)http://en.wikipedia.org/wiki/Mantle_(geology)http://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Black_smokerhttp://en.wikipedia.org/wiki/Black_smokerhttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Subduction_zoneshttp://en.wikipedia.org/wiki/Subduction_zoneshttp://en.wikipedia.org/wiki/Magmahttp://en.wikipedia.org/wiki/Magmahttp://en.wikipedia.org/wiki/Viscoushttp://en.wikipedia.org/wiki/Viscoushttp://en.wikipedia.org/wiki/Viscoushttp://en.wikipedia.org/wiki/Silicahttp://en.wikipedia.org/wiki/Mount_Etnahttp://en.wikipedia.org/wiki/Mount_Etnahttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Hotspot_(geology)http://en.wikipedia.org/wiki/Hotspot_(geology)http://en.wikipedia.org/wiki/Mantle_plumehttp://en.wikipedia.org/wiki/Hawaiian_Islandshttp://en.wikipedia.org/wiki/Hawaiian_Islandshttp://en.wikipedia.org/wiki/Hawaiian_Islandshttp://en.wikipedia.org/wiki/Snake_River_Plainhttp://en.wikipedia.org/wiki/Snake_River_Plainhttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Volcano#cite_note-Foulger-0http://en.wikipedia.org/wiki/File:Lakagigar_Iceland_2004-07-01.jpghttp://en.wikipedia.org/wiki/File:Lakagigar_Iceland_2004-07-01.jpghttp://en.wikipedia.org/wiki/Adiabatic_processhttp://en.wikipedia.org/wiki/Mantle_(geology)http://en.wikipedia.org/wiki/Divergent_boundaryhttp://en.wikipedia.org/wiki/Black_smokerhttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Convergent_boundaryhttp://en.wikipedia.org/wiki/Subduction_zoneshttp://en.wikipedia.org/wiki/Magmahttp://en.wikipedia.org/wiki/Viscoushttp://en.wikipedia.org/wiki/Silicahttp://en.wikipedia.org/wiki/Mount_Etnahttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Hotspot_(geology)http://en.wikipedia.org/wiki/Hotspot_(geology)http://en.wikipedia.org/wiki/Mantle_plumehttp://en.wikipedia.org/wiki/Hawaiian_Islandshttp://en.wikipedia.org/wiki/Snake_River_Plainhttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Volcano#cite_note-Foulger-0


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Lakagigarfissure vent inIceland, source of the major world climate alteration of 178384.

Skjaldbreiur, a shield volcano whose name means "broad shield"

The most common perception of a volcano is of a conical mountain, spewinglava and

poisonousgases from a craterat its summit. This describes just one of many types of volcano, and the

features of volcanoes are much more complicated. The structure and behavior of volcanoes depends

on a number of factors. Some volcanoes have rugged peaks formed bylava domesrather than a

summit crater, whereas others present landscape features such as massiveplateaus. Vents that issue

volcanic material (lava, which is what magma is called once it has escaped to the surface, and ash)

and gases (mainly steam and magmatic gases) can be located anywhere on thelandform. Many of

these vents give rise to smaller cones such asPuu on a flank ofHawaii'sKlauea. Other

types of volcano include cryovolcanoes (or ice volcanoes), particularly on some moons

ofJupiter,SaturnandNeptune; andmud volcanoes, which are formations often not associated with

known magmatic activity. Active mud volcanoes tend to involve temperatures much lower than those

ofigneous volcanoes, except when a mud volcano is actually a vent of an igneous volcano.

Fissure vents

Main article: Fissure vent

Volcanic fissure vents are flat, linear cracks through which lavaemerges.

Shield volcanoes

Main article: Shield volcano

Shield volcanoes, so named for their broad, shield-like profiles, are formed by the eruption of low-

viscosity lava that can flow a great distance from a vent, but not generally explode catastrophically.

Since low-viscosity magma is typically low in silica, shield volcanoes are more common in oceanic

than continental settings. The Hawaiian volcanic chain is a series of shield cones, and they are

common in Iceland, as well.

Lava domes

Main article: Lava dome
http://en.wikipedia.org/wiki/Lakihttp://en.wikipedia.org/wiki/Lakihttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Skjaldbrei%C3%B0urhttp://en.wikipedia.org/wiki/Skjaldbrei%C3%B0urhttp://en.wikipedia.org/wiki/Cone_(geometry)http://en.wikipedia.org/wiki/Lavahttp://en.wikipedia.org/wiki/Lavahttp://en.wikipedia.org/wiki/Volcanic_gashttp://en.wikipedia.org/wiki/Volcanic_craterhttp://en.wikipedia.org/wiki/Volcanic_craterhttp://en.wikipedia.org/wiki/Lava_domehttp://en.wikipedia.org/wiki/Lava_domehttp://en.wikipedia.org/wiki/Lava_domehttp://en.wikipedia.org/wiki/Landscapehttp://en.wikipedia.org/wiki/Plateauhttp://en.wikipedia.org/wiki/Plateauhttp://en.wikipedia.org/wiki/Plateauhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Volcano#Effects_of_volcanoeshttp://en.wikipedia.org/wiki/Landformhttp://en.wikipedia.org/wiki/Landformhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/K%C4%ABlaueahttp://en.wikipedia.org/wiki/Cryovolcanohttp://en.wikipedia.org/wiki/Jupiterhttp://en.wikipedia.org/wiki/Jupiterhttp://en.wikipedia.org/wiki/Saturnhttp://en.wikipedia.org/wiki/Saturnhttp://en.wikipedia.org/wiki/Saturnhttp://en.wikipedia.org/wiki/Neptunehttp://en.wikipedia.org/wiki/Neptunehttp://en.wikipedia.org/wiki/Mud_volcanohttp://en.wikipedia.org/wiki/Mud_volcanohttp://en.wikipedia.org/wiki/Mud_volcanohttp://en.wikipedia.org/wiki/Igneoushttp://en.wikipedia.org/wiki/Igneoushttp://en.wikipedia.org/wiki/Fissure_venthttp://en.wikipedia.org/wiki/Lavahttp://en.wikipedia.org/wiki/Lavahttp://en.wikipedia.org/wiki/Shield_volcanohttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Lava_domehttp://en.wikipedia.org/wiki/File:Skjaldbreidur_Herbst_2004.jpghttp://en.wikipedia.org/wiki/File:Skjaldbreidur_Herbst_2004.jpghttp://en.wikipedia.org/wiki/Lakihttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Skjaldbrei%C3%B0urhttp://en.wikipedia.org/wiki/Cone_(geometry)http://en.wikipedia.org/wiki/Lavahttp://en.wikipedia.org/wiki/Volcanic_gashttp://en.wikipedia.org/wiki/Volcanic_craterhttp://en.wikipedia.org/wiki/Lava_domehttp://en.wikipedia.org/wiki/Landscapehttp://en.wikipedia.org/wiki/Plateauhttp://en.wikipedia.org/wiki/Volcanic_ashhttp://en.wikipedia.org/wiki/Volcano#Effects_of_volcanoeshttp://en.wikipedia.org/wiki/Landformhttp://en.wikipedia.org/wiki/Pu'u_'%C5%8C'%C5%8Dhttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/K%C4%ABlaueahttp://en.wikipedia.org/wiki/Cryovolcanohttp://en.wikipedia.org/wiki/Jupiterhttp://en.wikipedia.org/wiki/Saturnhttp://en.wikipedia.org/wiki/Neptunehttp://en.wikipedia.org/wiki/Mud_volcanohttp://en.wikipedia.org/wiki/Igneoushttp://en.wikipedia.org/wiki/Fissure_venthttp://en.wikipedia.org/wiki/Lavahttp://en.wikipedia.org/wiki/Shield_volcanohttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Icelandhttp://en.wikipedia.org/wiki/Lava_dome


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Lava domes are built by slow eruptions of highly viscous lavas. They are sometimes formed within the

crater of a previous volcanic eruption (as in Mount Saint Helens), but can also form independently, as

in the case ofLassen Peak. Like stratovolcanoes, they can produce violent, explosive eruptions, but

their lavas generally do not flow far from the originating vent.

Cryptodomes

Cryptodomes are formed when viscous lava forces its way up and causes a bulge. The1980 eruption

of Mount St. Helenswas an example. Lava was under great pressure and forced a bulge in the

mountain, which was unstable and slid down the north side.

Volcanic cones (cinder cones)

Main articles:volcanic cone andCinder cone

Volcanic cones orcinder cones are the result from eruptions that erupt mostly small pieces

ofscoria and pyroclastics (both resemble cinders, hence the name of this volcano type) that build up

around the vent. These can be relatively short-lived eruptions that produce a cone-shaped hill perhaps

30 to 400 meters high. Most cinder cones erupt onlyonce. Cinder cones may form as flank vents on

larger volcanoes, or occur on their own. Parcutinin MexicoandSunset CraterinArizona are

examples of cinder cones. InNew Mexico,Caja del Riois avolcanic fieldof over 60 cinder cones.

Stratovolcanoes (composite volcanoes)

Cross-section through astratovolcano(vertical scale is exaggerated):

1. Large magma chamber2. Bedrock3. Conduit (pipe)4. Base

9. Layers of lava emitted by the volcano10. Throat11. Parasitic cone12. Lava flow
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5. Sill6. Dike7. Layers of ash emitted by the volcano

8. Flank

13. Vent14. Crater15. Ash cloud

Main article: Stratovolcano

Stratovolcanoes orcomposite volcanoes are tall conical mountains composed of lava flows andother ejecta in alternate layers, thestrata that give rise to the name. Stratovolcanoes are also known

as composite volcanoes, created from several structures during different kinds of eruptions.

Strato/composite volcanoes are made of cinders, ash and lava. Cinders and ash pile on top of each

other, lava flows on top of the ash, where it cools and hardens, and then the process begins again.

Classic examples includeMt. Fujiin Japan,Mayon Volcano in the Philippines, and Mount

Vesuvius and Stromboli in Italy.

In recorded history, explosive eruptions by stratovolcanoes have posed the greatest hazard to

civilizations, as ashis produced by anexplosive eruption. No supervolcano erupted in recorded

history. Shield volcanoes have not an enormous pressure build up from the lava flow. Fissure vents

andmonogenetic volcanic fields (volcanic cones) have not powerful explosive eruptions, as they are

many times underextension. Stratovolcanoes (3035) are steeper than shield volcanoes (generally

510), their loose tephra are material for dangerouslahars.[3]

Supervolcanoes

Main article: Supervolcano

See also:List of largest volcanic eruptions

A supervolcano is a large volcano that usually has a largecalderaand can potentially producedevastation on an enormous, sometimes continental, scale. Such eruptions would be able to cause

severe cooling of global temperatures for many years afterwards because of the huge volumes

ofsulfurand ash erupted. They are the most dangerous type of volcano. Examples

include Yellowstone Caldera inYellowstone National Park and Valles Caldera inNew Mexico (both

western United States),Lake Taupo inNew Zealand,Lake Tobain Sumatra,Indonesia andNgorogoro

Craterin Tanzania,KrakatoanearJava and Sumatra,Indonesia. Supervolcanoes are hard to identify

centuries later, given the enormous areas they cover.Large igneous provinces are also considered

supervolcanoes because of the vast amount ofbasaltlava erupted, but are non-explosive.

Submarine volcanoes

Main article: Submarine volcano

Submarine volcanoes are common features on the ocean floor. Some are active and, in shallow

water, disclose their presence by blasting steam and rocky debris high above the surface of the sea.

Many others lie at such great depths that the tremendous weight of the water above them prevents the
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explosive release of steam and gases, although they can be detected by hydrophones and

discoloration of water because ofvolcanic gases. Pumice rafts may also appear. Even large

submarine eruptions may not disturb the ocean surface. Because of the rapid cooling effect of water as

compared to air, and increased buoyancy, submarine volcanoes often form rather steep pillars over

their volcanic vents as compared to above-surface volcanoes. They may become so large that they

break the ocean surface as new islands. Pillow lava is a common eruptive product of submarine

volcanoes. Hydrothermal ventsare common near these volcanoes, andsome support peculiar

ecosystems based on dissolved minerals.

Subglacial volcanoes

Main article: Subglacial volcano

Subglacial volcanoes develop underneath icecaps. They are made up of flat lava which flows at the

top of extensive pillow lavas andpalagonite. When the icecap melts, the lavas on the top collapse,

leaving a flat-topped mountain. These volcanoes are also called table mountains,tuyas or

(uncommonly) mobergs. Very good examples of this type of volcano can be seen in Iceland, however,

there are also tuyas in British Columbia. The origin of the term comes from Tuya Butte, which is one of

the several tuyas in the area of theTuya RiverandTuya Range in northern British Columbia. Tuya

Butte was the first such landform analyzed and so its name has entered the geological literature for

this kind of volcanic formation. The Tuya Mountains Provincial Parkwas recently established to protect

this unusual landscape, which lies north ofTuya Lake and south of theJennings Rivernear the

boundary with the Yukon Territory.

Mud volcanoes

Main article: Mud volcano

Mud volcanoes ormud domes are formations created by geo-excreted liquids and gases, although

there are several processes which may cause such activity. The largest structures are 10 kilometers in

diameter and reach 700 meters high.

Erupted material
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Phoehoe Lava flow onHawaii. The picture shows overflows of a mainlava channel.

The Stromboli stratovolcano off the coast ofSicily has erupted continuously for thousands of years, giving rise to

the termstrombolian eruption.

Lava composition

Another way of classifying volcanoes is by the composition of material erupted(lava), since this affects

the shape of the volcano. Lava can be broadly classified into 4 different compositions (Cas & Wright,

1987):

If the erupted magmacontains a high percentage (>63%) ofsilica, the lava is called felsic.

Felsic lavas (dacites orrhyolites) tend to be highly viscous(not very fluid) and are

erupted as domes or short, stubby flows. Viscous lavas tend to formstratovolcanoes or lava

domes.Lassen PeakinCaliforniais an example of a volcano formed from felsic lava and is

actually a large lava dome.

Because siliceous magmas are so viscous, they tend to trap volatiles(gases) that are

present, which cause the magma to erupt catastrophically, eventually

formingstratovolcanoes. Pyroclastic flows (ignimbrites) are highly hazardous products of such

volcanoes, since they are composed of molten volcanic ash too heavy to go up into the

atmosphere, so they hug the volcano's slopes and travel far from their vents during large

eruptions. Temperatures as high as 1,200 C are known to occur in pyroclastic flows, which

will incinerate everything flammable in their path and thick layers of hot pyroclastic flow

deposits can be laid down, often up to many meters thick.Alaska'sValley of Ten Thousand

Smokes, formed by the eruption ofNovarupta nearKatmai in 1912, is an example of a

thickpyroclastic floworignimbritedeposit. Volcanic ash that is light enough to be erupted high

into theEarth's atmospheremay travel many kilometres before it falls back to ground as atuff.

If the erupted magma contains 5263% silica, the lava is ofintermediate composition.

These "andesitic" volcanoes generally only occur above subduction

zones (e.g. Mount Merapiin Indonesia).
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Andesitic lava is typically formed at convergent boundarymargins oftectonic plates,

by several processes:

Hydration melting of peridotite and fractional crystallization

Sarychev Peak eruption,Matua Island, oblique satellite view

Melting of subductedslab containing sediments[citation needed]

Magma mixing between felsic rhyolitic and mafic basaltic magmas in an

intermediate reservoir prior to emplacement or lava flow.

If the erupted magma contains 45% silica, the lava is called mafic (because it

contains higher percentages ofmagnesium (Mg) and iron (Fe)) orbasaltic. These lavas are

usually much less viscous than rhyolitic lavas, depending on their eruption temperature; they also

tend to be hotter than felsic lavas. Mafic lavas occur in a wide range of settings:

At mid-ocean ridges, where two oceanic platesare pulling apart, basaltic lava erupts

aspillows to fill the gap;

Shield volcanoes (e.g. the Hawaiian Islands, including Mauna Loa and Kilauea), on

bothoceanic and continental crust;

As continental flood basalts.

Some erupted magmas contain


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Lava texture

Two types of lava are named according to the surface texture: Aa (pronounced [ a a] )

andphoehoe([pa ho.e h o.e] ), bothHawaiian words. Aa is characterized by a rough,

clinkery surface and is the typical texture of viscous lava flows. However, even basaltic or mafic flows

can be erupted asaa flows, particularly if the eruption rate is high and the slope is steep.

Phoehoe is characterized by its smooth and often ropey or wrinkly surface and is generally formed

from more fluid lava flows. Usually, only mafic flows will erupt as phoehoe, since they often erupt at

higher temperatures or have the proper chemical make-up to allow them to flow with greater fluidity.

Volcanic activity

Fresco with Mount VesuviusbehindBacchus andAgathodaimon, as seen inPompeii'sHouse of the Centenary

Popular classification of volcanoes

Active

A popular way of classifying magmatic volcanoes is by their frequency oferuption, with those that

erupt regularly called active, those that have erupted in historical times but are now quiet

called dormant, and those that have not erupted in historical times called extinct. However, these

popular classificationsextinct in particularare practically meaningless to scientists. They use

classifications which refer to a particular volcano's formative and eruptive processes and resulting

shapes, which was explained above.

There is no real consensus among volcanologists on how to define an "active" volcano. The lifespan of

a volcano can vary from months to several million years, making such a distinction sometimes

meaningless when compared to the lifespans of humans or even civilizations. For example, many of

Earth's volcanoes have erupted dozens of times in the past few thousand years but are not currently
http://en.wikipedia.org/wiki/Surfacehttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/P%C4%81hoehoehttp://en.wikipedia.org/wiki/P%C4%81hoehoehttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Hawaiian_languagehttp://en.wikipedia.org/wiki/Hawaiian_languagehttp://en.wikipedia.org/wiki/Frescohttp://en.wikipedia.org/wiki/Mount_Vesuviushttp://en.wikipedia.org/wiki/Bacchushttp://en.wikipedia.org/wiki/Bacchushttp://en.wikipedia.org/wiki/Agathodaimonhttp://en.wikipedia.org/wiki/Pompeiihttp://en.wikipedia.org/wiki/Pompeiihttp://en.wikipedia.org/wiki/House_of_the_Centenaryhttp://en.wikipedia.org/wiki/House_of_the_Centenaryhttp://en.wikipedia.org/wiki/Types_of_volcanic_eruptionshttp://en.wikipedia.org/wiki/Types_of_volcanic_eruptionshttp://en.wikipedia.org/wiki/File:Pompeii_-_Casa_del_Centenario_-_MAN.jpghttp://en.wikipedia.org/wiki/File:Pompeii_-_Casa_del_Centenario_-_MAN.jpghttp://en.wikipedia.org/wiki/Surfacehttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/P%C4%81hoehoehttp://en.wikipedia.org/wiki/Wikipedia:IPA_for_Hawaiianhttp://en.wikipedia.org/wiki/Hawaiian_languagehttp://en.wikipedia.org/wiki/Frescohttp://en.wikipedia.org/wiki/Mount_Vesuviushttp://en.wikipedia.org/wiki/Bacchushttp://en.wikipedia.org/wiki/Agathodaimonhttp://en.wikipedia.org/wiki/Pompeiihttp://en.wikipedia.org/wiki/House_of_the_Centenaryhttp://en.wikipedia.org/wiki/Types_of_volcanic_eruptions


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showing signs of eruption. Given the long lifespan of such volcanoes, they are very active. By human

lifespans, however, they are not.

Scientists usually consider a volcano to be erupting orlikely to erupt if it is currently erupting, or

showing signs of unrest such as unusual earthquake activity or significant new gas emissions. Most

scientists consider a volcano active if it has erupted in holocenetimes. Historic times is another

timeframe foractive.[4]But it is important to note that the span of recorded history differs from region to

region. InChina and theMediterranean, recorded history reaches back more than 3,000 years but in

the Pacific Northwest of theUnited Statesand Canada, it reaches back less than 300 years, and

in Hawaii and New Zealand, only around 200 years.[5] The Smithsonian Global Volcanism Program's

definition ofactive is having erupted within the last 10,000 years (the 'holocene' period).

Presently there are about 500 active volcanoes in the world the majority following along the Pacific

'Ring of Fire' and around 50 of these erupt each year.[6]The United States is home to 50 active

volcanoes.[7]There are more than 1,500 potentially active volcanoes. [8]An estimated 500 million people

live near active volcanoes.[9]

Extinct

Fourpeaked volcano,Alaska, in September 2007, after being thought extinct for over 10,000 years.

Extinct volcanoes are those that scientists consider unlikely to erupt again, because the volcano no

longer has a lava supply. Examples of extinct volcanoes are many volcanoes on the Hawaiian

Emperor seamount chain in the Pacific Ocean,Hohentwiel, Shiprock and the Zuidwal volcano in

the Netherlands.Edinburgh Castlein Scotland is famously located atop an extinct volcano. Otherwise,

whether a volcano is truly extinct is often difficult to determine. Since "supervolcano"calderas can have

eruptive lifespans sometimes measured in millions of years, a caldera that has not produced an

eruption in tens of thousands of years is likely to be considered dormant instead of extinct.

Dormant

It is difficult to distinguish an extinct volcano from a dormant one. Volcanoes are often considered to

be extinct if there are no written records of its activity. Nevertheless, volcanoes may remain dormant
http://en.wikipedia.org/wiki/Holocenehttp://en.wikipedia.org/wiki/Holocenehttp://en.wikipedia.org/wiki/Volcano#cite_note-3http://en.wikipedia.org/wiki/Volcano#cite_note-3http://en.wikipedia.org/wiki/Chinahttp://en.wikipedia.org/wiki/Chinahttp://en.wikipedia.org/wiki/Mediterraneanhttp://en.wikipedia.org/wiki/United_Stateshttp://en.wikipedia.org/wiki/United_Stateshttp://en.wikipedia.org/wiki/United_Stateshttp://en.wikipedia.org/wiki/Canadahttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/New_Zealandhttp://en.wikipedia.org/wiki/Volcano#cite_note-4http://en.wikipedia.org/wiki/Volcano#cite_note-4http://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Volcano#cite_note-5http://en.wikipedia.org/wiki/Volcano#cite_note-5http://en.wikipedia.org/wiki/Volcano#cite_note-6http://en.wikipedia.org/wiki/Volcano#cite_note-6http://en.wikipedia.org/wiki/Volcano#cite_note-6http://en.wikipedia.org/wiki/Volcano#cite_note-7http://en.wikipedia.org/wiki/Volcano#cite_note-7http://en.wikipedia.org/wiki/Volcano#cite_note-8http://en.wikipedia.org/wiki/Volcano#cite_note-8http://en.wikipedia.org/wiki/Fourpeaked_Mountainhttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Hawaiian_%E2%80%93_Emperor_seamount_chainhttp://en.wikipedia.org/wiki/Hawaiian_%E2%80%93_Emperor_seamount_chainhttp://en.wikipedia.org/wiki/Pacific_Oceanhttp://en.wikipedia.org/wiki/Pacific_Oceanhttp://en.wikipedia.org/wiki/Hohentwielhttp://en.wikipedia.org/wiki/Hohentwielhttp://en.wikipedia.org/wiki/Shiprockhttp://en.wikipedia.org/wiki/Zuidwal_volcanohttp://en.wikipedia.org/wiki/Netherlandshttp://en.wikipedia.org/wiki/Edinburgh_Castlehttp://en.wikipedia.org/wiki/Edinburgh_Castlehttp://en.wikipedia.org/wiki/Edinburgh_Castlehttp://en.wikipedia.org/wiki/Scotlandhttp://en.wikipedia.org/wiki/Calderahttp://en.wikipedia.org/wiki/File:Fourpeaked-fumaroles-cyrus-read1.JPGhttp://en.wikipedia.org/wiki/File:Fourpeaked-fumaroles-cyrus-read1.JPGhttp://en.wikipedia.org/wiki/Holocenehttp://en.wikipedia.org/wiki/Volcano#cite_note-3http://en.wikipedia.org/wiki/Chinahttp://en.wikipedia.org/wiki/Mediterraneanhttp://en.wikipedia.org/wiki/United_Stateshttp://en.wikipedia.org/wiki/Canadahttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/New_Zealandhttp://en.wikipedia.org/wiki/Volcano#cite_note-4http://en.wikipedia.org/wiki/Pacific_Ring_of_Firehttp://en.wikipedia.org/wiki/Volcano#cite_note-5http://en.wikipedia.org/wiki/Volcano#cite_note-6http://en.wikipedia.org/wiki/Volcano#cite_note-7http://en.wikipedia.org/wiki/Volcano#cite_note-8http://en.wikipedia.org/wiki/Fourpeaked_Mountainhttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Hawaiian_%E2%80%93_Emperor_seamount_chainhttp://en.wikipedia.org/wiki/Hawaiian_%E2%80%93_Emperor_seamount_chainhttp://en.wikipedia.org/wiki/Pacific_Oceanhttp://en.wikipedia.org/wiki/Hohentwielhttp://en.wikipedia.org/wiki/Shiprockhttp://en.wikipedia.org/wiki/Zuidwal_volcanohttp://en.wikipedia.org/wiki/Netherlandshttp://en.wikipedia.org/wiki/Edinburgh_Castlehttp://en.wikipedia.org/wiki/Scotlandhttp://en.wikipedia.org/wiki/Caldera


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for a long period of time. For example, Yellowstonehas a repose/recharge period of around 700 ka,

andToba of around 380 ka.[10]Vesuvius was described by Roman writers as having been covered with

gardens and vineyards before its famous eruption of AD 79, which destroyed the towns

ofHerculaneum andPompeii. Before its catastrophic eruption of 1991,Pinatubo was an inconspicuous

volcano, unknown to most people in the surrounding areas. Two other examples are the long-

dormantSoufrire Hills volcano on the island ofMontserrat, thought to be extinct before activity

resumed in 1995 and Fourpeaked MountaininAlaska, which, before its September 2006 eruption, had

not erupted since before 8000 BC and had long been thought to be extinct.

Technical classification of volcanoes

Volcanic-alert level

The three common popular classifications of volcanoes can be subjective and some volcanoes thought

to have been extinct have announced to the world they were just pretending. [11]To help prevent

citizens from falsely believing they are not at risk when living on or near a volcano, countries have

adopted new classifications to describe the various levels and stages of volcanic activity.[12] Some alert

systems use different numbers or colors to designate the different stages. Other systems use colors

and words. Some systems use a combination of both.

Volcano warning schemes of the United States

The United States Geological Survey (USGS) has adopted a common system nationwide for

characterizing the level of unrest and eruptive activity at volcanoes. The new volcano alert-level

system classifies volcanoes now as being in a normal, advisory, watch or warning stage. Additionally,

colors are used to denote the amount of ash produced. Details of the US system can be found

atVolcano warning schemes of the United States.

Notable volcanoes

Koryakskyvolcano towering overPetropavlovsk-Kamchatsky on Kamchatka Peninsula, Far Eastern Russia.

Main articles:Lists of volcanoes andDecade Volcanoes
http://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Kiloannumhttp://en.wikipedia.org/wiki/Toba_Lakehttp://en.wikipedia.org/wiki/Toba_Lakehttp://en.wikipedia.org/wiki/Volcano#cite_note-chesner1991-9http://en.wikipedia.org/wiki/Vesuviushttp://en.wikipedia.org/wiki/Herculaneumhttp://en.wikipedia.org/wiki/Herculaneumhttp://en.wikipedia.org/wiki/Pompeiihttp://en.wikipedia.org/wiki/Pompeiihttp://en.wikipedia.org/wiki/Pinatubohttp://en.wikipedia.org/wiki/Pinatubohttp://en.wikipedia.org/wiki/Soufri%C3%A8re_Hillshttp://en.wikipedia.org/wiki/Soufri%C3%A8re_Hillshttp://en.wikipedia.org/wiki/Montserrathttp://en.wikipedia.org/wiki/Montserrathttp://en.wikipedia.org/wiki/Fourpeaked_Mountainhttp://en.wikipedia.org/wiki/Fourpeaked_Mountainhttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Volcano#cite_note-10http://en.wikipedia.org/wiki/Volcano#cite_note-10http://en.wikipedia.org/wiki/Volcano#cite_note-11http://en.wikipedia.org/wiki/Volcano_warning_schemes_of_the_United_Stateshttp://en.wikipedia.org/wiki/Volcano_warning_schemes_of_the_United_Stateshttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Petropavlovsk-Kamchatskyhttp://en.wikipedia.org/wiki/Kamchatka_Peninsulahttp://en.wikipedia.org/wiki/Kamchatka_Peninsulahttp://en.wikipedia.org/wiki/Russiahttp://en.wikipedia.org/wiki/Russiahttp://en.wikipedia.org/wiki/Lists_of_volcanoeshttp://en.wikipedia.org/wiki/Lists_of_volcanoeshttp://en.wikipedia.org/wiki/Decade_Volcanoeshttp://en.wikipedia.org/wiki/Decade_Volcanoeshttp://en.wikipedia.org/wiki/File:Avacha_volcano_Petropavlovsk-Kamchatsky_oct-2005.jpghttp://en.wikipedia.org/wiki/File:Avacha_volcano_Petropavlovsk-Kamchatsky_oct-2005.jpghttp://en.wikipedia.org/wiki/Yellowstone_Calderahttp://en.wikipedia.org/wiki/Kiloannumhttp://en.wikipedia.org/wiki/Toba_Lakehttp://en.wikipedia.org/wiki/Volcano#cite_note-chesner1991-9http://en.wikipedia.org/wiki/Vesuviushttp://en.wikipedia.org/wiki/Herculaneumhttp://en.wikipedia.org/wiki/Pompeiihttp://en.wikipedia.org/wiki/Pinatubohttp://en.wikipedia.org/wiki/Soufri%C3%A8re_Hillshttp://en.wikipedia.org/wiki/Montserrathttp://en.wikipedia.org/wiki/Fourpeaked_Mountainhttp://en.wikipedia.org/wiki/Alaskahttp://en.wikipedia.org/wiki/Volcano#cite_note-10http://en.wikipedia.org/wiki/Volcano#cite_note-11http://en.wikipedia.org/wiki/Volcano_warning_schemes_of_the_United_Stateshttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Petropavlovsk-Kamchatskyhttp://en.wikipedia.org/wiki/Kamchatka_Peninsulahttp://en.wikipedia.org/wiki/Russiahttp://en.wikipedia.org/wiki/Lists_of_volcanoeshttp://en.wikipedia.org/wiki/Decade_Volcanoes


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The Decade Volcanoes are 16 volcanoes identified by theInternational Association of Volcanology

and Chemistry of the Earth's Interior(IAVCEI) as being worthy of particular study in light of their history

of large, destructive eruptions and proximity to populated areas. They are named Decade Volcanoes

because the project was initiated as part of theUnited Nations-sponsored International Decade for

Natural Disaster Reduction. The 16 current Decade Volcanoes are

Avachinsky-Koryaksky,Kamchatka,

Russia

Nevado de

Colima,Jaliscoand Colima,Mexico

Mount Etna, Sicily,Italy

Galeras,Nario, Colombia

Mauna Loa,Hawaii,USA

Mount Merapi,Central Java,Indonesia

Mount Nyiragongo,Democratic

Republic of the Congo

Mount Rainier, Washington,USA

Sakurajima, Kagoshima

Prefecture, Japan

Santa Maria/Santiaguito,Guatemala

Santorini,Cyclades, Greece

Taal Volcano, Luzon,Philippines

Teide,Canary Islands, Spain

Ulawun,New Britain,Papua New

Guinea

Mount Unzen,Nagasaki

Prefecture, Japan

Vesuvius,Naples, Italy

Effects of volcanoes

Schematic of volcano injection of aerosols and gases.
http://en.wikipedia.org/wiki/Decade_Volcanoeshttp://en.wikipedia.org/wiki/International_Association_of_Volcanology_and_Chemistry_of_the_Earth's_Interiorhttp://en.wikipedia.org/wiki/International_Association_of_Volcanology_and_Chemistry_of_the_Earth's_Interiorhttp://en.wikipedia.org/wiki/International_Association_of_Volcanology_and_Chemistry_of_the_Earth's_Interiorhttp://en.wikipedia.org/wiki/United_Nationshttp://en.wikipedia.org/wiki/United_Nationshttp://en.wikipedia.org/wiki/International_Decade_for_Natural_Disaster_Reductionhttp://en.wikipedia.org/wiki/International_Decade_for_Natural_Disaster_Reductionhttp://en.wikipedia.org/wiki/International_Decade_for_Natural_Disaster_Reductionhttp://en.wikipedia.org/wiki/Avachinskyhttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Kamchatka_Peninsulahttp://en.wikipedia.org/wiki/Kamchatka_Peninsulahttp://en.wikipedia.org/wiki/Colima_(volcano)http://en.wikipedia.org/wiki/Colima_(volcano)http://en.wikipedia.org/wiki/Jaliscohttp://en.wikipedia.org/wiki/Jaliscohttp://en.wikipedia.org/wiki/Jaliscohttp://en.wikipedia.org/wiki/Colimahttp://en.wikipedia.org/wiki/Colimahttp://en.wikipedia.org/wiki/Mexicohttp://en.wikipedia.org/wiki/Mount_Etnahttp://en.wikipedia.org/wiki/Sicilyhttp://en.wikipedia.org/wiki/Sicilyhttp://en.wikipedia.org/wiki/Italyhttp://en.wikipedia.org/wiki/Italyhttp://en.wikipedia.org/wiki/Galerashttp://en.wikipedia.org/wiki/Nari%C3%B1ohttp://en.wikipedia.org/wiki/Colombiahttp://en.wikipedia.org/wiki/Mauna_Loahttp://en.wikipedia.org/wiki/Mauna_Loahttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/USAhttp://en.wikipedia.org/wiki/USAhttp://en.wikipedia.org/wiki/Mount_Merapihttp://en.wikipedia.org/wiki/Mount_Merapihttp://en.wikipedia.org/wiki/Central_Javahttp://en.wikipedia.org/wiki/Central_Javahttp://en.wikipedia.org/wiki/Central_Javahttp://en.wikipedia.org/wiki/Indonesiahttp://en.wikipedia.org/wiki/Indonesiahttp://en.wikipedia.org/wiki/Mount_Nyiragongohttp://en.wikipedia.org/wiki/Mount_Nyiragongohttp://en.wikipedia.org/wiki/Democratic_Republic_of_the_Congohttp://en.wikipedia.org/wiki/Democratic_Republic_of_the_Congohttp://en.wikipedia.org/wiki/Democratic_Republic_of_the_Congohttp://en.wikipedia.org/wiki/Mount_Rainierhttp://en.wikipedia.org/wiki/Washington_(U.S._state)http://en.wikipedia.org/wiki/Washington_(U.S._state)http://en.wikipedia.org/wiki/USAhttp://en.wikipedia.org/wiki/USAhttp://en.wikipedia.org/wiki/Sakurajimahttp://en.wikipedia.org/wiki/Kagoshima_Prefecturehttp://en.wikipedia.org/wiki/Kagoshima_Prefecturehttp://en.wikipedia.org/wiki/Japanhttp://en.wikipedia.org/wiki/Santa_Mar%C3%ADa_(volcano)http://en.wikipedia.org/wiki/Santa_Mar%C3%ADa_(volcano)http://en.wikipedia.org/wiki/Guatemalahttp://en.wikipedia.org/wiki/Guatemalahttp://en.wikipedia.org/wiki/Santorinihttp://en.wikipedia.org/wiki/Santorinihttp://en.wikipedia.org/wiki/Cycladeshttp://en.wikipedia.org/wiki/Cycladeshttp://en.wikipedia.org/wiki/Greecehttp://en.wikipedia.org/wiki/Taal_Volcanohttp://en.wikipedia.org/wiki/Luzonhttp://en.wikipedia.org/wiki/Luzonhttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Teidehttp://en.wikipedia.org/wiki/Teidehttp://en.wikipedia.org/wiki/Canary_Islandshttp://en.wikipedia.org/wiki/Canary_Islandshttp://en.wikipedia.org/wiki/Spainhttp://en.wikipedia.org/wiki/Ulawunhttp://en.wikipedia.org/wiki/Ulawunhttp://en.wikipedia.org/wiki/New_Britainhttp://en.wikipedia.org/wiki/New_Britainhttp://en.wikipedia.org/wiki/New_Britainhttp://en.wikipedia.org/wiki/Papua_New_Guineahttp://en.wikipedia.org/wiki/Papua_New_Guineahttp://en.wikipedia.org/wiki/Papua_New_Guineahttp://en.wikipedia.org/wiki/Mount_Unzenhttp://en.wikipedia.org/wiki/Nagasaki_Prefecturehttp://en.wikipedia.org/wiki/Nagasaki_Prefecturehttp://en.wikipedia.org/wiki/Japanhttp://en.wikipedia.org/wiki/Vesuviushttp://en.wikipedia.org/wiki/Province_of_Napleshttp://en.wikipedia.org/wiki/Italyhttp://en.wikipedia.org/wiki/File:Mauna_Loa_atmospheric_transmission.pnghttp://en.wikipedia.org/wiki/File:Mauna_Loa_atmospheric_transmission.pnghttp://en.wikipedia.org/wiki/File:Volcanic_injection.svghttp://en.wikipedia.org/wiki/File:Volcanic_injection.svghttp://en.wikipedia.org/wiki/International_Association_of_Volcanology_and_Chemistry_of_the_Earth's_Interiorhttp://en.wikipedia.org/wiki/International_Association_of_Volcanology_and_Chemistry_of_the_Earth's_Interiorhttp://en.wikipedia.org/wiki/United_Nationshttp://en.wikipedia.org/wiki/International_Decade_for_Natural_Disaster_Reductionhttp://en.wikipedia.org/wiki/International_Decade_for_Natural_Disaster_Reductionhttp://en.wikipedia.org/wiki/Avachinskyhttp://en.wikipedia.org/wiki/Koryakskyhttp://en.wikipedia.org/wiki/Kamchatka_Peninsulahttp://en.wikipedia.org/wiki/Colima_(volcano)http://en.wikipedia.org/wiki/Colima_(volcano)http://en.wikipedia.org/wiki/Jaliscohttp://en.wikipedia.org/wiki/Colimahttp://en.wikipedia.org/wiki/Mexicohttp://en.wikipedia.org/wiki/Mount_Etnahttp://en.wikipedia.org/wiki/Sicilyhttp://en.wikipedia.org/wiki/Italyhttp://en.wikipedia.org/wiki/Galerashttp://en.wikipedia.org/wiki/Nari%C3%B1ohttp://en.wikipedia.org/wiki/Colombiahttp://en.wikipedia.org/wiki/Mauna_Loahttp://en.wikipedia.org/wiki/Hawaiihttp://en.wikipedia.org/wiki/USAhttp://en.wikipedia.org/wiki/Mount_Merapihttp://en.wikipedia.org/wiki/Central_Javahttp://en.wikipedia.org/wiki/Indonesiahttp://en.wikipedia.org/wiki/Mount_Nyiragongohttp://en.wikipedia.org/wiki/Democratic_Republic_of_the_Congohttp://en.wikipedia.org/wiki/Democratic_Republic_of_the_Congohttp://en.wikipedia.org/wiki/Mount_Rainierhttp://en.wikipedia.org/wiki/Washington_(U.S._state)http://en.wikipedia.org/wiki/USAhttp://en.wikipedia.org/wiki/Sakurajimahttp://en.wikipedia.org/wiki/Kagoshima_Prefecturehttp://en.wikipedia.org/wiki/Kagoshima_Prefecturehttp://en.wikipedia.org/wiki/Japanhttp://en.wikipedia.org/wiki/Santa_Mar%C3%ADa_(volcano)http://en.wikipedia.org/wiki/Guatemalahttp://en.wikipedia.org/wiki/Santorinihttp://en.wikipedia.org/wiki/Cycladeshttp://en.wikipedia.org/wiki/Greecehttp://en.wikipedia.org/wiki/Taal_Volcanohttp://en.wikipedia.org/wiki/Luzonhttp://en.wikipedia.org/wiki/Philippineshttp://en.wikipedia.org/wiki/Teidehttp://en.wikipedia.org/wiki/Canary_Islandshttp://en.wikipedia.org/wiki/Spainhttp://en.wikipedia.org/wiki/Ulawunhttp://en.wikipedia.org/wiki/New_Britainhttp://en.wikipedia.org/wiki/Papua_New_Guineahttp://en.wikipedia.org/wiki/Papua_New_Guineahttp://en.wikipedia.org/wiki/Mount_Unzenhttp://en.wikipedia.org/wiki/Nagasaki_Prefecturehttp://en.wikipedia.org/wiki/Nagasaki_Prefecturehttp://en.wikipedia.org/wiki/Japanhttp://en.wikipedia.org/wiki/Vesuviushttp://en.wikipedia.org/wiki/Province_of_Napleshttp://en.wikipedia.org/wiki/Italy


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Solar radiation graph 1958-2008, showing how the radiation is reduced after major volcanic eruptions.

Sulfur dioxideconcentration over theSierra Negra Volcano,Galapagos Islandsduring an eruption in October

2005

There are many different types of volcanic eruptions and associated activity:phreatic

eruptions(steam-generated eruptions), explosive eruption of high-silicalava (e.g.,rhyolite),

effusive eruption of low-silica lava (e.g., basalt),pyroclastic flows, lahars (debris flow) andcarbon

dioxideemission. All of these activities can pose a hazard to humans. Earthquakes,hot

springs,fumaroles,mud pots and geysers often accompany volcanic activity.

The concentrations of different volcanic gasescan vary considerably from one volcano to the

next.Water vaporis typically the most abundant volcanic gas, followed bycarbon

dioxideandsulfur dioxide. Other principal volcanic gases include hydrogen sulfide,hydrogen

chloride, andhydrogen fluoride. A large number of minor and trace gases are also found in

volcanic emissions, for example hydrogen, carbon monoxide, halocarbons, organic compounds,

and volatile metal chlorides.

Large, explosive volcanic eruptions inject water vapor (H2O), carbon dioxide (CO2), sulfur dioxide

(SO2), hydrogen chloride (HCl), hydrogen fluoride (HF) and ash (pulverized rock andpumice) into

the stratosphere to heights of 1632 kilometres (1020 mi) above the Earth's surface. The most

significant impacts from these injections come from the conversion of sulfur dioxide to sulfuric

acid(H2SO4), which condenses rapidly in the stratosphere to form finesulfateaerosols. The

aerosols increase the Earth's albedoits reflection of radiation from theSunback into space

and thus cool the Earth's lower atmosphere or troposphere; however, they also absorb heat

radiated up from the Earth, thereby warming thestratosphere. Several eruptions during the past

century have caused a decline in the average temperature at the Earth's surface of up to half a

degree (Fahrenheit scale) for periods of one to three years sulfur dioxide from the eruption

ofHuaynaputina probably caused the Russian famine of 16011603.[13]
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One proposed volcanic winterhappened c. 70,000 years ago following thesupereruption ofLake

Toba on Sumatra island in Indonesia.[14] According to the Toba catastrophe theory to which some

anthropologists and archeologists subscribe, it had global consequences,[15]killing most humans

then alive and creating apopulation bottleneckthat affected the genetic inheritance of all humans

today.[16]The 1815 eruption ofMount Tamboracreated global climate anomalies that became

known as the "Year Without a Summer" because of the effect on North American and European

weather.[17] Agricultural crops failed and livestock died in much of the Northern Hemisphere,

resulting in one of the worst famines of the 19th century.[18]The freezing winter of 174041, which

led to widespreadfamine in northern Europe, may also owe its origins to a volcanic eruption.[19]

It has been suggested that volcanic activity caused or contributed to the End-

Ordovician, Permian-Triassic,Late Devonianmass extinctions, and possibly others. The massive

eruptive event which formed theSiberian Traps, one of the largest known volcanic events of the

last 500 million years ofEarth's geological history, continued for a million years and is considered

to be the likely cause of the "Great Dying" about 250 million years ago,[20] which is estimated to

have killed 90% of species existing at the time. [21]

The sulfate aerosols also promote complex chemicalreactions on their surfaces that alter chlorine

and nitrogen chemical species in the stratosphere. This effect, together with increased

stratosphericchlorinelevels from chlorofluorocarbonpollution, generates chlorine monoxide

(ClO), which destroysozone(O3). As the aerosols grow and coagulate, they settle down into the

upper troposphere where they serve as nuclei forcirrus clouds and further modify the

Earth's radiation balance. Most of the hydrogen chloride (HCl) and hydrogen fluoride (HF) aredissolved in water droplets in the eruption cloud and quickly fall to the ground asacid rain. The

injected ash also falls rapidly from the stratosphere; most of it is removed within several days to a

few weeks. Finally, explosive volcanic eruptions release the greenhouse gas carbon dioxide and

thus provide a deep source ofcarbon for biogeochemical cycles.

Gas emissions from volcanoes are a natural contributor to acid rain. Volcanic activity releases

about 130 to 230teragrams (145 million to 255 millionshort tons) ofcarbon dioxideeach year.

[22]Volcanic eruptions may inject aerosols into the Earth's atmosphere. Large injections may cause

visual effects such as unusually colorful sunsets and affect global climate mainly by cooling it.Volcanic eruptions also provide the benefit of adding nutrients to soil through

the weatheringprocess of volcanic rocks. These fertile soils assist the growth of plants and

various crops. Volcanic eruptions can also create new islands, as the magma cools and solidifies

upon contact with the water.
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t_tonhttp://en.wikipedia.org/wiki/Carbon_dioxidehttp://en.wikipedia.org/wiki/Volcano#cite_note-21http://en.wikipedia.org/wiki/Particulatehttp://en.wikipedia.org/wiki/Earth's_atmospherehttp://en.wikipedia.org/wiki/Climatehttp://en.wikipedia.org/wiki/Soilhttp://en.wikipedia.org/wiki/Weathering


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Ash thrown into the air by eruptions can present a hazard to aircraft, especiallyjet aircraft where

the particles can be melted by the high operating temperature. Dangerous encounters in 1982

after the eruption ofGalunggung in Indonesia, and 1989 after the eruption ofMount Redoubtin

Alaska raised awareness of this phenomenon. NineVolcanic Ash Advisory Centers were

established by theInternational Civil Aviation Organizationto monitor ash clouds and advise pilots

accordingly. The2010 eruptions of Eyjafjallajkullcaused major disruptions to air travel in Europe.

Volcanoes on other planetary bodies

TheTvashtarvolcano erupts a plume 330 km (205 mi) above the surface ofJupiter's moonIo.
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Olympus Mons (Latin, "Mount Olympus") is the tallest knownmountainin oursolar system, located on

theplanetMars.

Main articles: Geology of the Moon,Geology of Mars,Volcanism on Io, andVolcanism on Venus

The Earth's Moon has no large volcanoes and no current volcanic activity, although recent

evidence suggests it may still possess a partially molten core. [23] However, the Moon

volcanic e

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