Search results for "Volcano"

showing 10 items of 591 documents

Magmatic gas percolation through the old lava dome of El Misti volcano

2017

International audience; The proximity of the major city of Arequipa to El Misti has focused attention on the hazards posed by the active volcano. Since its last major eruption in the fifteenth century, El Misti has experienced a series of modest phreatic eruptions and fluctuating fumarolic activity. Here, we present the first measurements of the compositions of gas emitted from the lava dome in the summit crater. The gas composition is found to be fairly dry with a H2O/SO2 molar ratio of 32 ± 3, a CO2/SO2 molar ratio of 2.7 ± 0.2, a H2S/SO2 molar ratio of 0.23 ± 0.02 and a H2/SO2 molar ratio of 0.012 ± 0.002. This magmatic gas signature with minimal evidence of hydrothermal or wall rock int…

Volcanic hazardsImágenes ASTER010504 meteorology & atmospheric sciencesPoison control010502 geochemistry & geophysics01 natural sciencesASTERTrail by fireImpact craterGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGases volcánicos14. Life underwaterGas compositionPetrology0105 earth and related environmental sciencesWall rockgeographygeography.geographical_feature_categoryVolcanesOutgassingArequipaVolcanic hazardLava domeVolcán MistiPhreatic eruptionVolcano13. Climate action[SDU]Sciences of the Universe [physics]DesgasificaciónGeologySeismologyMulti-GASResearch Article
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Helium and CO2 soil gas emission from Santorini (Greece)

1994

Soil gas investigation is a useful tool to detect active faults. The sudden appearance of soil gas anomalies in zones of deep-reaching faults represents a promising potential precursor of earthquakes and volcanic eruptions. In volcanic areas the development of soil gas monitoring techniques is particularly important, as they can represent, together with remote sensing techniques, the only geochemical methods that can be safely applied during volcanic unrest, when it becomes impossible or too dangerous to sample crater fumaroles. A soil gas survey was carried out in June 1993 at the main island of Thera, in the Santorini volcanic complex. CO2 flux and CO2 and helium concentrations were measu…

Volcanic hazardsgeographygeography.geographical_feature_categorySoil gasGeochemistryActive faultFault (geology)FumaroleImpact craterVolcanoGeochemistry and PetrologyGeothermal gradientSeismologyGeologyBulletin of Volcanology
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Hot-spot detection and characterization of strombolian activity from MODIS infrared data

2014

Identifying and characterizing strombolian activity from space is a challenging task for satellite-based infrared systems. Stromboli volcano is a natural laboratory that offers a unique opportunity for refining thermal remote-sensing applications that involve transient phenomena and small to moderate hot-spots. A new simple and fast algorithm gave us the opportunity to revisit the MODIS-derived thermal output at Stromboli volcano over the last 13 years. The new algorithm includes both night-time and daytime data and shows high performance with the detection of small-amplitude thermal anomalies (  1000 MW). The ...

Volcano Remote SensingDaytimegeographygeography.geographical_feature_categoryInfraredHot spot (veterinary medicine)Fast algorithmStrombolian eruptionCharacterization (materials science)MODISVolcanohot spot; MODIS; Stromboli; infraredhot spot13. Climate actioninfraredGeneral Earth and Planetary SciencesSatelliteStromboliGeologyRemote sensingInternational Journal of Remote Sensing
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Practical Volcano-Independent Recognition of Seismic Events: VULCAN.ears Project

2021

Recognizing the mechanisms underlying seismic activity and tracking temporal and spatial patterns of earthquakes represent primary inputs to monitor active volcanoes and forecast eruptions. To quantify this seismicity, catalogs are established to summarize the history of the observed types and number of volcano-seismic events. In volcano observatories the detection and posterior classification or labeling of the events is manually performed by technicians, often suffering a lack of unified criteria and eventually resulting in poorly reliable labeled databases. State-of-the-art automatic Volcano-Seismic Recognition (VSR) systems allow real-time monitoring and consistent catalogs. VSR systems…

Volcano monitoring010504 meteorology & atmospheric sciencesComputer scienceVolcano-independent VSRInduced seismicity010502 geochemistry & geophysicscomputer.software_genre01 natural sciencesEruption forecastingvolcano-seismic recognitionMachine learningVolcano-seismic recognitionlcsh:ScienceData mining0105 earth and related environmental sciencesGraphical user interfacegeographygeography.geographical_feature_categorybusiness.industryvolcano monitoringdata miningVULCAN.earsmachine learningVolcano13. Climate actionVulcanGeneral Earth and Planetary Scienceslcsh:QData miningeruption forecastingSeismic recognitionbusinesscomputer
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In situ Volcano Monitoring: Present and Future

2015

During the last couple of decades, volcanology has evolved significantly, allowing for an improved understanding of volcanic processes preceding, accompanying and following eruptive events. Key elements to these achievements are the huge amounts of high quality data being collected by networks of increasingly sensitive instruments deployed at active volcanoes. The diffusion of continuous, precise measurements of: (1) wide-band ground displacement; (2) flux and chemistry of volatile emissions; and (3) the spatio-temporal variations of potential fields (e.g., gravity) now permit imaging the mechanism that controls mass transfer underneath volcanoes to an unprecedented level of detail. Joined …

Volcano monitoringArts and Humanities (all)Volcano seismologyGround deformationVolcanic SO2 fluxGravity methodVolcanic plume
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Diffuse soil CO2 degassing from Linosa island

2014

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Volcano monitoringLineamentGeochemistrysoil degassingfluid geochemistryCO2lcsh:QC851-999Instruments and techniques; Soil degassing; Volcano monitoring; GeophysicsSequential Gaussian simulationSoil co2 fluxFlux (metallurgy)Soil degassingGeomorphologygeographygeography.geographical_feature_categoryRiftlcsh:QC801-809Instruments and techniquesSettore GEO/08 - Geochimica E VulcanologiaTectonicslcsh:Geophysics. Cosmic physicsGeophysicsVolcanoLinosaSoil CO_2 fluxlcsh:Meteorology. ClimatologyGeologyChannel (geography)
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Gas emissions and crustal deformation from the Krýsuvík high temperature geothermal system, Iceland

2020

Abstract The Krýsuvik volcanic system is located on the oblique spreading Reykjanes Peninsula, SW Iceland. Since early 2009 the region has been undergoing episodes of localized ground uplift and subsidence. From April–November 2013, we operated near-real time monitoring of gas emissions in Krýsuvik, using a Multi-component Gas Analyzer System (Multi-GAS), collecting data on gas composition from a fumarole (H2O, CO2, SO2, H2S). The dataset in this study, comprises a near-continuous gas composition time series, the quantification of diffuse CO2 gas flux, analytical results for direct samples of dry gas, seismic records, and GPS data. Gas emissions from the Krýsuvik geothermal system were exam…

Volcano monitoringgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeothermal gaVolcanic gaMineralogySubsidence (atmosphere)FluxCrustal deformation010502 geochemistry & geophysicsInlet01 natural sciencesGas analyzerFumaroleKrýsuvíkVolcanic CO2 fluxGeophysicsVolcanoGeochemistry and PetrologyGas compositionGeophysicGeothermal gradientGeology0105 earth and related environmental sciences
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Plume composition and volatile flux from Nyamulagira volcano

2015

Nyamulagira, in the Virunga volcanic province (VVP), Democratic Republic of Congo, is one of the most active volcanoes in Africa. The volcano is located about 25 km north-northwest of Lake Kivu in the Western Branch of the East African Rift System (EARS). The activity is characterized by frequent eruptions (on average, one eruption every 2–4 years) which occur both from the summit crater and from the flanks (31 flank eruptions over the last 110 years). Due to the peculiar low viscosity of its lava and its location in the floor of the rift, Nyamulagira morphology is characterized by a wide lava field that covers over 1100 km2 and contains more than 100 flank cones. Indeed, Nyamulagira is a S…

Volcanoes degassing Virunga province gas chemistry flux
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Environmental impact of volcanic emissions at Nyiragongo (DRC)

2015

The large amount of trace elements emitted from volcanoes has a strong impact on the close surrounding areas. Nyiragongo Volcano (Democratic Republic of Congo) belongs to the Virunga volcanic chain and is one of the most active volcanoes in Africa. It is characterized by the presence of an active and permanent lava lake with a persistent degassing activity. During a field trip in October-November 2014, we investigated the impact of the volcanogenic deposition in the surrounding of the crater by using different sampling techniques. Rain-gauges were used to collect atmospheric bulk deposition. Active and passive biomonitoring techniques (moss-bags and leaves of endemic plants – Senecio spp. a…

Volcanoes atmomspheric deposition rainwaterSettore GEO/08 - Geochimica E Vulcanologia
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Research data supporting "Dynamics of outgassing and plume transport revealed by proximal Unmanned Aerial System (UAS) measurements at Volcán Villarr…

2018

Timeseries of volcanic gas concentrations obtained by a drone-mounted multi-GAS sensor payload at Villarrica Volcano, Chile (20 March 2018). All concentrations are expressed in ppmv. Data have been corrected for differences in sensor response time using Ratiocalc software.

Volcanology
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