Volcano

A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.[2][5][6] Large eruptions can affect atmospheric temperature as ash and droplets of sulfuric acid obscure the Sun and cool Earth's troposphere.[14] At the mid-ocean ridges, two tectonic plates diverge from one another as hot mantle rock creeps upwards beneath the thinned oceanic crust.[16][2] Hotspots are volcanic areas thought to be formed by mantle plumes, which are hypothesized to be columns of hot material rising from the core-mantle boundary.Volcanic fissure vents are generally found at diverging plate boundaries, they are flat, linear fractures through which basaltic lava emerges.Most cinder cones erupt only once and some may be found in monogenetic volcanic fields that may include other features that form when magma comes into contact with water such as maar explosion craters and tuff rings.Based on satellite images, it has been suggested that cinder cones might occur on other terrestrial bodies in the Solar system too; on the surface of Mars and the Moon.[28][29][30][31] Stratovolcanoes are tall conical mountains composed of lava flows and tephra in alternate layers, the strata that gives rise to the name.The combination is deadly, promoting explosive eruptions that produce great quantities of ash, as well as pyroclastic surges like the one that destroyed the city of Saint-Pierre in Martinique in 1902.[33] A supervolcano is defined as a volcano that has experienced one or more eruptions that produced over 1,000 cubic kilometres (240 cu mi) of volcanic deposits in a single explosive event.A supervolcano can produce devastation on a continental scale, and severely cool global temperatures for many years after the eruption due to the huge volumes of sulfur and ash released into the atmosphere.Pillow lava is a common eruptive product of submarine volcanoes and is characterized by thick sequences of discontinuous pillow-shaped masses which form underwater.Over time, the formations created by submarine volcanoes may become so large that they break the ocean surface as new islands or floating pumice rafts.An oceanographic research campaign in May 2019 showed that the previously mysterious humming noises were caused by the formation of a submarine volcano off the coast of Mayotte.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.[69] Through natural processes, mainly erosion, so much of the solidified erupted material that makes up the mantle of a volcano may be stripped away that its inner anatomy becomes apparent.[84] Vesuvius was described by Roman writers as having been covered with gardens and vineyards before its unexpected eruption of 79 CE, which destroyed the towns of Herculaneum and Pompeii.To help prevent people 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.Volcanic gases can reach the stratosphere, where they form sulfuric acid aerosols that can reflect solar radiation and lower surface temperatures significantly.[93] The 1815 eruption of Mount Tambora created global climate anomalies that became known as the "Year Without a Summer" because of the effect on North American and European weather.[99] Volcanic ash and weathered basalt produce some of the most fertile soil in the world, rich in nutrients such as iron, magnesium, potassium, calcium, and phosphorus.[101] Many volcanoes near human settlements are heavily monitored with the aim of providing adequate advance warnings of imminent eruptions to nearby populations.[102] The diversity of volcanoes and their complexities mean that eruption forecasts for the foreseeable future will be based on probability, and the application of risk management.[101] Citizens who may be concerned about their own exposure to risk from nearby volcanic activity should familiarize themselves with the types of, and quality of, volcano monitoring and public notification procedures being employed by governmental authorities in their areas.[105] Earth's Moon has no large volcanoes and no current volcanic activity, although recent evidence suggests it may still possess a partially molten core.However, radar sounding by the Magellan probe revealed evidence for comparatively recent volcanic activity at Venus's highest volcano Maat Mons, in the form of ash flows near the summit and on the northern flank.[119] Volcanoes are not distributed evenly over the Earth's surface but active ones with significant impact were encountered early in human history, evidenced by footprints of hominina found in East African volcanic ash dated at 3.66 million years old.Examples are: (1) the stories in the Athabascan subcultures about humans living inside mountains and a woman who uses fire to escape from a mountain,[121]: 135  (2) Pele's migration through the Hawarian island chain, ability to destroy forests and manifestations of the god's temper,[122] and (3) the association in Javanese folklore of a king resident in Mount Merapi volcano and a queen resident at a beach 50 km (31 mi) away on what is now known to be an earthquake fault that interacts with that volcano.[125] By 65 CE, Seneca the Younger proposed combustion as the cause,[125] an idea also adopted by the Jesuit Athanasius Kircher (1602–1680), who witnessed eruptions of Mount Etna and Stromboli, then visited the crater of Vesuvius and published his view of an Earth in Mundus Subterraneus with a central fire connected to numerous others depicting volcanoes as a type of safety valve.[127][better source needed] In 1650, René Descartes proposed the core of Earth was incandescent and, by 1785, the works of Decartes and others were synthesized into geology by James Hutton in his writings about igneous intrusions of magma.
Augustine Volcano (Alaska) during its eruptive phase on January 24, 2006
Map showing the divergent plate boundaries (oceanic spreading ridges) and recent sub-aerial volcanoes (mostly at convergent boundaries)
Video of lava agitating and bubbling in the volcanic eruption of Litli-Hrútur ( Fagradalsfjall ), Iceland, 2023
Lakagigar fissure vent in Iceland , the source of the major world climate alteration of 1783–84 , has a chain of volcanic cones along its length.
Skjaldbreiður , a shield volcano whose name means "broad shield"
East dome, a lava dome located on the lower east flank of St. Helens, part of the Sugar Bowl Eruptive Period (1800 YA).
Izalco volcano , the youngest volcano in El Salvador. Izalco erupted almost continuously from 1770 (when it formed) to 1958, earning it the nickname of "Lighthouse of the Pacific".
Cross-section through a stratovolcano (vertical scale is exaggerated) :
  1. Large magma chamber
  2. Bedrock
  3. Conduit (pipe)
  4. Base
  5. Sill
  6. Dike
  7. Layers of ash emitted by the volcano
  8. Flank
  9. Layers of lava emitted by the volcano
  10. Throat
  11. Parasitic cone
  12. Lava flow
  13. Vent
  14. Crater
  15. Ash cloud
Mt. Vesuvius, a stratovolcano, Gulf of Naples .
Lake Taupō, a volcanogenic lake in the caldera of Taupō supervolcano , New Zealand.
Crater lake, a volcanic lake in Oregon .
Satellite images of the January 15, 2022, eruption of Hunga Tonga-Hunga Haʻapai
Mud volcano at Gobustan
Castle geyser eruption, Yellowstone National Park .
Timelapse of San Miguel (volcano) degassing in 2022. El Salvador is home to 20 Holocene volcanoes, 3 of which have erupted in last 100yrs [ 49 ]
Pāhoehoe lava flow on Hawaii . The picture shows overflows of a main lava channel .
Litli-Hrútur ( Fagradalsfjall ) eruption 2023. View from an aeroplane
The Stromboli stratovolcano off the coast of Sicily has erupted continuously for thousands of years, giving rise to its nickname "Lighthouse of the Mediterranean".
Light-microscope image of tuff as seen in thin section (long dimension is several mm): the curved shapes of altered glass shards (ash fragments) are well preserved, although the glass is partly altered. The shapes were formed around bubbles of expanding, water-rich gas.
Schematic of volcano injection of aerosols and gases
Narcondam Island , India, is classified as a dormant volcano by the Geological Survey of India .
Solar radiation graph 1958–2008, showing how the radiation is reduced after major volcanic eruptions
Sulfur dioxide concentration over the Sierra Negra Volcano , Galapagos Islands , during an eruption in October 2005
Comparison of major United States prehistoric eruptions ( VEI 7 and 8 ) with major historical volcanic eruptions in the 19th and 20th century (VEI 5, 6 and 7). From left to right: Yellowstone 2.1 Ma, Yellowstone 1.3 Ma, Long Valley 6.26 Ma, Yellowstone 0.64 Ma . 19th century eruptions: Tambora 1815, Krakatoa 1883. 20th century eruptions: Novarupta 1912, St. Helens 1980, Pinatubo 1991.
The Tvashtar volcano erupts a plume 330 km (205 mi) above the surface of Jupiter 's moon Io .
Olympus Mons ( Latin , "Mount Olympus"), located on the planet Mars, is the tallest known mountain in the Solar System .
Volcano (disambiguation)Volcanic (disambiguation)Augustine Volcanoplanetary-mass objectvolcanic ashmagma chambertectonic platesdivergingconvergingmid-ocean ridgeMid-Atlantic RidgeRing of FireEast African RiftWells Gray-Clearwater volcanic fieldRio Grande riftdiapirscore–mantle boundarymantle plumeshotspot volcanismvolcanic islandHawaiian hotspottransform tectonic boundariesactivesulfuric acidtropospherevolcanic winterscryovolcanismcryovolcanoAeolian IslandsVulcanRoman mythologyvolcanismvolcanologyPlate tectonicslithosphereconvectionmantlepolygeneticmonogeneticDivergent boundarymid-ocean ridgesoceanic crustadiabaticpartial meltingdivergent plate boundariesseafloorBlack smokersIcelandConvergent boundarySubductionflux meltingviscoussilicacools and solidifies at depthvolcanic arcsCascade VolcanoesJapanese ArchipelagoIndonesiaHotspot (geology)HotspotsHawaiian IslandsSnake River PlainYellowstone CalderaYellowstone hotspotflood basaltsaulacogenalkali lavacarbonatitesTypes of volcanoesFagradalsfjallconicalcraterlava domeslandscapeplateauslandformPuʻu ʻŌʻōKīlaueaVolcanic cratersLake Taupōmud volcanoescryovolcanoesJupiterSaturnNeptuneigneousFissure ventLakagigarVolcanic fissure ventsdiverging plate boundariesbasaltic lavalava plateauShield volcanoSkjaldbreiðureffusive eruptionsOlympus MonsSolar SystemLava domerhyoliteMount St. HelensLassen Peak1980 eruption of Mount St. Helensvolcanic coneCinder coneIzalco volcanoscoriapyroclasticsmonogenetic volcanic fieldstuff ringsflank ventsParícutinSunset CraterArizonaNew MexicoCaja del Riovolcanic fieldstratovolcanotephrastratalaccolithsparasitic conesMount FujiMayon VolcanoMount VesuviusStromboliGulf of Naplesexplosive eruptionhistoricallyexplosive eruptionspyroclastic surgeslaharsvolcanic bombsTaupō supervolcanoSupervolcanoList of largest volcanic eruptionscalderasulfurgeologic mappingYellowstone National ParkValles CalderaLake TobaSumatraNgorongoro CraterOregonVolcanogenic lakesSubmarine volcanoSubaqueous volcanoHunga Tonga-Hunga HaʻapaiHolocenehydrophonesvolcanic gasesPillow lavaHydrothermal ventssome support peculiar ecosystemschemotrophspumice raftsseismicearthquakeoceanographicMayotteSubglacial volcanoice capspalagoniteBritish ColumbiaTuya ButteTuya RiverTuya RangeTuya Mountains Provincial ParkTuya LakeJennings RiverYukon Territorygeysersfumarolesmud poolshot springsGobustanMud volcanoBaratangBalochistanFumaroleGeyserpressureSan Miguel (volcano)El SalvadorHawaiilava channelSicilyvolcanic eruptioncarbon dioxidesulfur dioxidehydrogen sulfideVolcanic gasWater vapourhydrogen chloridehydrogen fluoridehydrogencarbon monoxidehalocarbonsvolatileLava flowMount RinjaniLombokfelsicdacitesrhyolitesPyroclastic flowsignimbritesAlaskaValley of Ten Thousand SmokesNovaruptaKatmaiEarth's atmosphereeruption columnstratospherefractional crystallizationintermediate compositionandesiticconvergent boundariesmagnesiumbasalticShield volcanoesMauna LoaKilaueaoceaniccontinental crustultramafickomatiitesProterozoicpāhoehoeHawaiianRhyoliticobsidianthin sectionwhen it flows to the surfacesand-sizedvolcaniclasticserosionbiological anatomyCinder HillMount BirdRoss IslandAntarcticaMount KaimonKyūshūDevils TowerTypes of volcanic eruptionsvolcanic explosivity indexHawaiian eruptionslava fountainsHawaiian volcanoesStrombolian eruptionsgas slugVulcanian eruptionsVulcanoPeléan eruptionsMount PeléePlinian eruptionsPliny the Youngereruption of Mount Vesuvius in 79pumiceash-fallMt. MazamaPhreatomagmatic eruptionsgroundwatersuperheatedPhreatic eruptionscountry rockFrescoBacchusAgathodaemonPompeiiHouse of the CentenarySmithsonian InstitutionGlobal Volcanism ProgramActive volcanoearthquake swarmsNarcondam IslandGeological Survey of IndiaMount EdgecumbeAlaska Volcano ObservatoryChaitén volcanoYellowstoneVesuviuseruption of 79 CEHerculaneumPinatuboSoufrière HillsMontserratPlymouthghost townFourpeaked MountainCapulin Volcano National MonumentHawaiian–Emperor seamount chainHohentwielGermanyShiprockCapulinZuidwal volcanoNetherlandsMonte VultureEdinburgh CastleCastle RockcalderasKoryakskyPetropavlovsk-KamchatskyKamchatka PeninsulaRussiaLists of volcanoesDecade VolcanoesInternational Association of Volcanology and Chemistry of the Earth's InteriorInternational Decade for Natural Disaster ReductionAvachinskyKamchatkaNevado de ColimaJaliscoColimaMount EtnaGalerasNariñoMount MerapiCentral JavaMount NyiragongoMount RainierWashingtonSakurajimaKagoshima PrefectureSanta Maria/SantiaguitoSantoriniCycladesTaal VolcanoUlawunNew BritainMount UnzenNagasaki PrefectureNaplesDeep Earth Carbon Degassing ProjectDeep Carbon ObservatoryMulti-Component Gas Analyzer Systemprediction of volcanic activitySierra Negra VolcanoGalapagos IslandsVolcanic hazardbasaltsector collapsesvolcanic gas emissionsmud potsHuaynaputinaRussian famine of 1601–1603ozone layeracid rainlivestockExplosive volcanic eruptionscarbonbiogeochemical cyclesjet aircraftturbineVEI 7 and 8volcanic wintersupereruptionpopulation bottleneckEnd-OrdovicianPermian-TriassicLate Devonianmass extinctionsMount TamboraYear Without a SummerfamineVolcanogenic massive sulfide ore depositGeothermal powerRapa NuiEaster Islandprobabilityrisk managementMount PinatuboList of extraterrestrial volcanoesVolcanism on the MoonVolcanism on MarsVolcanism on IoVolcanism on VenusTvashtarrillesLava flowsMaat Monsash flowsArsia MonsAscraeus MonsHecates TholusPavonis MonsMars ExpresssilicateEuropaGalilean moonsVoyager 2TritonCassini–Huygensliquid nitrogenammoniamethaneSaturnianKuiper Belt ObjectQuaoarexoplanetCOROT-7btransittidal heatinghomininasupernaturaldemigodsÇatalhöyükHephaistosAnaxagorasSeneca the YoungerJesuitAthanasius KircherMundus SubterraneusJohannes KeplerRené DescartesJames Huttonigneous intrusionsLazzaro Spallanzani1886 eruption of Mount TaraweraphreatomagmatichydrothermalAlfred Lacroix1902 eruption of Mount PeléeArthur HolmesList of volcanoesList of volcanic eruptions by death tollList of volcanic landformsMaritime impacts of volcanic eruptionsTimeline of volcanism on EarthVolcano NumberVolcano observatoryGeological Society of AmericaDK Pub.British Geological SurveyBibcodeOxford University PressNational Park ServiceUnited States Geological SurveyAmerican Journal of ScienceElsevier Inc.public domainChisholm, HughEncyclopædia BritannicaJohn W. JuddUniversity of California PressJournal of Geophysical ResearchWayback MachineThorarinsson, SigurdurPrinceton University PressReviews in Mineralogy and GeochemistryEuropean Space AgencyNational Geographic SocietyKorean Air LineslandformsList of landformsMountainPlateauTablelandValleyIce sheetSteppeTundraFluvialAlluvial fanCanyonChannelFloodplainislandMeanderRapidsStraitWaterfallGlacialArêteCirqueGlacierIce fieldTunnel valleyOceanic and coastal landformsContinental shelfCoral reefEstuaryIsthmusLagoonOceanic trenchPeninsulaSeamountLava fieldVolcanic craterVolcanic crater lakeVolcanic damVolcanic plateauVolcanic plugWall rockAeolianDesertDry lakeSandhillArtificial islandArtificial reefBridgeBuildingLand reclamationPolderQuarryReservoirTunnelGeographical featureVolcanic Seven SummitsExtraterrestrial volcanoesLarge volume volcanic eruptions in the Basin and Range ProvinceLarge volcanic eruptionsLargest volcanic eruptionsEarth timelineQuaternary volcanic eruptionsVolcanic eruption deathsComplex volcanoCryptovolcanic structureParasitic conePyroclastic conePyroclastic shieldRootless coneSomma volcanoTossolHarmonic tremorVolcanic rocksAgglomerateAndesiteBasaltic andesiteBenmoreiteBlairmoriteCinderDaciteFelsiteIgnimbriteKomatiiteLapilliLatiteLeucititeNephelinitePhonolitePhonotephriteRhyodaciteTephriphonoliteTrachyandesiteTrachybasaltTrachytePyroclastic fallPyroclastic flowHotspotEruptions by death tollVolcanic arcVolcanic belt