Search results for "Volcano"

showing 10 items of 591 documents

Forecasting Effusive Dynamics and Decompression Rates by Magmastatic Model at Open-vent Volcanoes

2017

AbstractEffusive eruptions at open-conduit volcanoes are interpreted as reactions to a disequilibrium induced by the increase in magma supply. By comparing four of the most recent effusive eruptions at Stromboli volcano (Italy), we show how the volumes of lava discharged during each eruption are linearly correlated to the topographic positions of the effusive vents. This correlation cannot be explained by an excess of pressure within a deep magma chamber and raises questions about the actual contributions of deep magma dynamics. We derive a general model based on the discharge of a shallow reservoir and the magmastatic crustal load above the vent, to explain the linear link. In addition, we…

010504 meteorology & atmospheric sciencesLavaScienceHawaiian eruptionVolcanologyStromboli; effusion rate; lava flowMagma chamberStromboli effusion rate lava flow010502 geochemistry & geophysics01 natural sciencesArticleeffusion rateEffusive eruptionStratovolcanoEffusive EruptionsStromboliPetrology0105 earth and related environmental sciencesgeographyMultidisciplinaryExplosive eruptiongeography.geographical_feature_categoryQRVolcanology; Effusive EruptionsVolcanoMagmaMedicinelava flowGeology
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Shallow vent architecture during hybrid explosive-effusive activity at Cordón Caulle (Chile, 2011-12): Evidence from direct observations and pyroclas…

2013

International audience; In June 2011, an eruption of rhyolite magma began at the Puyehue-Cordón Caulle volcanic complex, southern Chile. By January 2012, explosive activity had declined from sustained pyroclastic (Plinian to sub-Plinian) fountaining to mixed gas and ash jetting punctuated by Vulcanian blasts. This explosive activity was accompanied by synchronous effusion of obsidian lava in a hybrid explosive-effusive eruption. Fortuitous climatic conditions permitted ground-based observation and video recording of transient vent dynamics as well as real-time collection of proximal juvenile ash as it sedimented from the active plume. The main eruptive vent complex and site of lava effusion…

010504 meteorology & atmospheric sciencesLava[SDE.MCG]Environmental Sciences/Global ChangesSilicicPyroclastic rockMineralogyrhyolite010502 geochemistry & geophysics01 natural sciencestube pumiceobsidianGeochemistry and PetrologyPuyehue-Cordón CaulleRhyolite[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyTephraPetrology0105 earth and related environmental sciencesgeographyVulcanian eruptiongeography.geographical_feature_categoryPeléan eruptionexplosive-effusive transitionGeophysicsVolcanopermeabilityGeologyVulcanian
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Shallow system rejuvenation and magma discharge trends at Piton de la Fournaise volcano (La Réunion Island)

2017

International audience; Basaltic magma chambers are often characterized by emptying and refilling cycles that influence their evolution in space and time, and the associated eruptive activity. During April 2007, the largest historical eruption of Piton de la Fournaise (Île de La Réunion, France) drained the shallow plumbing system (>240×106 m3>240×106 m3) and resulted in collapse of the 1-km-wide summit crater. Following these major events, Piton de la Fournaise entered a seven-year long period of near-continuous deflation interrupted, in June 2014, by a new phase of significant inflation. By integrating multiple datasets (lava discharge rates, deformation, seismicity, gas flux, gas composi…

010504 meteorology & atmospheric sciencesLavaeffusive paroxysmMagma chamber010502 geochemistry & geophysicseffusive trend01 natural sciencesEffusive eruptionImpact crater[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryeffusive paroxysm; effusive trends; Piton de la Fournaise; shallow plumbing system; unloading; Geophysics; Geochemistry and Petrology; Earth and Planetary Sciences (miscellaneous); Space and Planetary ScienceGeochemistry and Petrologyunloading[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyEarth and Planetary Sciences (miscellaneous)Petrology0105 earth and related environmental sciencesBasaltgeographygeography.geographical_feature_categoryeffusive trendsFumarolePiton de la FournaiseGeophysicsVolcanoshallow plumbing systemSpace and Planetary ScienceMagmaGeologySeismology
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Dynamic Triggering of Mud Volcano Eruptions During the 2016-2017 Central Italy Seismic Sequence

2017

On 24 August 2016 a seismic event (Mw 6.0) was the first of the long Central Italy sequence (ongoing at the end of 2017) of medium-to-high magnitude earthquakes, with nine Mw ≥5 up to October 2017, and with about 74.000 seismic events registered after one year. The largest was the Mw 6.5 30 October 2016 event near Norcia. After the major seismic events, seventeen mud volcanoes erupted around Monteleone di Fermo village (Marche region). Mud volcano eruptions generally occurred a few hours to a few days after the main earthquakes, suggesting a seismic triggering. We analyzed the peak ground velocities (PGV) and dynamic stresses during the three largest earthquakes. We also evaluated the stati…

010504 meteorology & atmospheric sciencesMagnitude (mathematics)010502 geochemistry & geophysics01 natural sciencesSequence (geology)GeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Static stressSeismologyGeology0105 earth and related environmental sciencesDynamic stressMud volcanoJournal of Geophysical Research: Solid Earth
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An expanded model and application of the combined effect of crystal-size distribution and crystal shape on the relative viscosity of magmas

2018

International audience; This study examines the combined effect of crystal-size distributions (CSD) and crystal shape on the rheology of vesicle free magmatic suspensions and provides the first practical application of an empirical model to estimate the relative effect of crystal content and CSD's on the viscosity of magma directly from textural image analysis of natural rock samples in the form of a user-friendly texture-rheology spreadsheet calculator. We extend and apply established relationships between the maximum packing fraction ϕm of a crystal bearing suspension and both its rheological properties and the polydispersity γ of a CSD. By using analogue rotational rheometric experiments…

010504 meteorology & atmospheric sciencesRelative viscosityDispersityThermodynamicsMagma rheologyCrystal size distribution010502 geochemistry & geophysicsAtomic packing factor01 natural sciencesCrystalViscosityGeophysicsRheologyGeochemistry and PetrologyMagma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologySuspension (vehicle)GeologyCrystal shape0105 earth and related environmental sciences
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Validation of a novel Multi-Gas sensor for volcanic HCl alongside H2S and SO2 at Mt. Etna

2017

Erratum to: Bull Volcanol (2017) 79: 36DOI 10.1007/s00445-017-1114-zDuring the steps of corrections, the publisher inadvertently changed the author affiliations so that they were no longer correct. The correct information is given below. The publisher regrets this mistake.; International audience; Volcanic gas emission measurements inform predictions of hazard and atmospheric impacts. For these measurements, Multi-Gas sensors provide low-cost in situ monitoring of gas composition but to date have lacked the ability to detect halogens. Here, two Multi-Gas instruments characterized passive outgassing emissions from Mt. Etna’s (Italy) three summit craters, Voragine (VOR), North-east Crater (NE…

010504 meteorology & atmospheric sciencesResponse modelPoison controlMineralogyOpen-system volcanic degassing010502 geochemistry & geophysics01 natural sciencesElectronic noseImpact craterGeochemistry and PetrologyCalibrationGas compositionVolcanic outgassing0105 earth and related environmental sciencesMulti-Gas instrumentgeographygeography.geographical_feature_categoryE-noseOutgassingVolcano13. Climate action[SDU]Sciences of the Universe [physics]HalogenMagmaChlorineGeology
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Magmas near the critical degassing pressure drive volcanic unrest towards a critical state

2016

During the reawaking of a volcano, magmas migrating through the shallow crust have to pass through hydrothermal fluids and rocks. The resulting magma–hydrothermal interactions are still poorly understood, which impairs the ability to interpret volcano monitoring signals and perform hazard assessments. Here we use the results of physical and volatile saturation models to demonstrate that magmatic volatiles released by decompressing magmas at a critical degassing pressure (CDP) can drive volcanic unrest towards a critical state. We show that, at the CDP, the abrupt and voluminous release of H2O-rich magmatic gases can heat hydrothermal fluids and rocks, triggering an accelerating deformation …

010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyPoison control010502 geochemistry & geophysics01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyHydrothermal circulationArticlePhysics and Astronomy (all)PetrologyVolcanic unrest0105 earth and related environmental sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryBiochemistry Genetics and Molecular Biology (all)QChemistry (all)CrustGeneral ChemistryPhysics and Astronomy (all) Volcano Eruption Unrest Campi FlegreiVolcano13. Climate actionMagmaRock failureGeologyPressure.drive
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Combined ground and aerial measurements resolve vent-specific gas fluxes from a multi-vent volcano

2020

Volcanoes with multiple summit vents present a methodological challenge for determining vent-specific gas emissions. Here, using a novel approach combining multiple ultraviolet cameras with synchronous aerial measurements, we calculate vent-specific gas compositions and fluxes for Stromboli volcano. Emissions from vent areas are spatially heterogeneous in composition and emission rate, with the central vent area dominating passive emissions, despite exhibiting the least explosive behaviour. Vents exhibiting Strombolian explosions emit low to negligible passive fluxes and are CO2-dominated, even during passive degassing. We propose a model for the conduit system based on contrasting rheologi…

010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyVolcanology010502 geochemistry & geophysics01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyArticleStromboliPetrologylcsh:Science0105 earth and related environmental sciencesExplosive behaviourgeographyMultidisciplinarygeography.geographical_feature_categoryQNatural hazardsGas emissionsGeneral ChemistryStrombolian eruptionPlumeOutgassingVolcanoConduit systemvolcanic gasesEnvironmental sciencelcsh:Q
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Editorial: Seismicity in Volcanic Areas

2021

International audience

010504 meteorology & atmospheric sciencesScienceQ010502 geochemistry & geophysics01 natural scienceseruptiontectonicvolcanoearthquake[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGeneral Earth and Planetary Sciencesseismicity volcanism swarmsdykeComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesmagma “mush”Frontiers in Earth Science
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Selenium mobilization in soils due to volcanic derived acid rain: An example from Mt Etna volcano, Sicily

2011

International audience; The significant amounts of selenium (Se) emitted by volcanoes may have important impact on human health due to the narrow range between nutrition requirement and toxic effects for living organisms upon Se exposure. Although soils play a key role in determining the level in food and water and thereby human health, little is known about the behaviour of Se in volcanic soils. In this work we evaluated the Se release during rainwater–soil interaction under controlled conditions using soils collected on the flanks of Etna volcano and synthetic rain. Selenium concentrations in soil leachate solutions displayed a spatial distribution, which cannot be explained by plume depo…

010504 meteorology & atmospheric sciencesSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; GroundwaterSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; Groundwaterchemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth SciencesVolcanoe010502 geochemistry & geophysics01 natural sciencesSelenateVolcanic soilchemistry.chemical_compoundSeleniumContaminationGeochemistry and PetrologySelenium acid rain soilsGeogenicChemical compositionGroundwater0105 earth and related environmental sciencesgeographyGroundwaterSeleniumgeography.geographical_feature_categoryGeologySettore GEO/08 - Geochimica E VulcanologiaDeposition (aerosol physics)chemistryVolcano13. Climate action[SDU]Sciences of the Universe [physics]Environmental chemistrySoil waterAcid rainGeologyGroundwaterSelenium
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