Search results for "LCA"

showing 10 items of 1995 documents

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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Ash-plume dynamics and eruption source parameters by infrasound and thermal imagery: The 2010 Eyjafjallajökull eruption

2013

During operational ash-cloud forecasting, prediction of ash concentration and total erupted mass directly depends on the determination of mass eruption rate (MER), which is typically inferred from plume height. Uncertainties for plume heights are large, especially for bent-over plumes in which the ascent dynamics are strongly affected by the surrounding wind field. Here we show how uncertainties can be reduced if MER is derived directly from geophysical observations of source dynamics. The combination of infrasound measurements and thermal camera imagery allows for the infrasonic type of source to be constrained (a dipole in this case) and for the plume exit velocity to be calculated (54–14…

010504 meteorology & atmospheric sciencesMeteorologyInfrasound Thermal cameras Volcanic Plume dynamicsInfrasoundPlume heightInfrasound010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesGeochemistry and PetrologyThermalEarth and Planetary Sciences (miscellaneous)ddc:5500105 earth and related environmental sciencesPlume heightLead (sea ice)Escape velocityPlumeGeophysics13. Climate actionSpace and Planetary ScienceParticle-size distributionEruption rateAsh eruptionsMass eruption rateGeology
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Active tectonics along the south east offshore margin of Mt. Etna: New insights from high-resolution seismic profiles

2018

The offshore margin of Mt. Etna has been shaped by Middle Pleistocene to Holocene shortening and extension and, more recently, by gravity-related sliding of the volcanic edifice. These processes have acted contemporaneously although the gravitational component largely prevails over the tectonic one. In order to investigate this issue, we focused on the main role of active tectonics along the south-eastern offshore of Mt. Etna by means of marine high-resolution seismic data. Seismic profiles revealed post-220 ka sedimentary deposits unconformably overlaying the Lower-Middle Pleistocene Etnean clayey substratum and volcanics of the Basal Tholeiitic phase and the Timpe phase. Offshore Aci Trez…

010504 meteorology & atmospheric sciencesPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturaleactive tectonics010502 geochemistry & geophysics01 natural sciencesSicilian thrust-beltPaleontologyActive tectonicActive tectonics; Ionian Sea; Mt. Etna; Seismic investigation; Sicilian thrust-belt; Earth and Planetary Sciences (all)Seismic investigationHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryContinental shelfMt. Etnalcsh:QE1-996.5Fold (geology)Ionian SeaMt. Etna; seismic investigation; active tectonics; Sicilian thrust-belt; Ionian SeaSeafloor spreadingVolcanic rocklcsh:GeologyTectonicsGeneral Earth and Planetary SciencesSedimentary rockEarth and Planetary Sciences (all)Geology
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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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The Graham Bank (Sicily Channel, central Mediterranean Sea). Seafloor signatures of volcanic and tectonic controls

2018

Abstract Graham Bank is a dominant physiographic element of the NW Sicily Channel (central Mediterranean Sea), affected in the last 100 years by numerous well-documented volcanic eruptions. We present the first results of a geomorphological study where the Graham Bank region in the depth interval 7–350 m was mapped for the first time with multi-beam echosounder and high-resolution seismic and multi-channel seismic reflection profiles. We describe in high resolution the detailed geomorphological features of Graham Bank, and how the superficial expression of different process and dynamics occurring in the sub-seafloor evidence volcanic and tectonic controls on seafloor morphology across a rel…

010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSeamount010502 geochemistry & geophysics01 natural sciencesFluid seepagePaleontologyMediterranean seaEcho soundingSlope instability14. Life underwater0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyFluid seepage; Graham Bank; Slope instability; Volcanic seamountgeography.geographical_feature_categoryVolcanic seamountFluid seepage Slope instability Volcanic seamount Graham BankGraham BankSeafloor spreadingTectonicsVolcanoSedimentary rockChannel (geography)Geology
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