Search results for "Volcanism"

showing 10 items of 90 documents

A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop

2019

Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large-volume pyroclastic deposits and later-stage deformation related to post-caldera resurgence and volcanism. Unrest episodes are not always followed by an eruption; however, every eruption is preceded by unrest. The Campi Flegrei caldera (CFc), located along the eastern Tyrrhenian coastline in southern Italy, is close to the densely populated area of Naples. It is one of the most dangerous volcanoes on Earth and represents a key example of an acti…

010504 meteorology & atmospheric sciencesCalderasGeochemistryEnergy Engineering and Power TechnologyPyroclastic rockVolcanologyMagma chamberVolcanism010502 geochemistry & geophysics01 natural sciencesdrillingsouthern ItalycalderaCaldera14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMechanical Engineeringlcsh:QE1-996.5VolcanologyMagellanPlus workshopInternational Ocean Discovery Programlcsh:GeologyCampi Flegrei calderaVolcanoItaly13. Climate actionEruptionMagmacaldera Campi Flegrei monitopring system hydrothermal system IODPCampi FlegreiGeology
researchProduct

Linking tephrochronology and soil characteristics in the Sila and Nebrodi mountains, Italy

2017

Recent studies have demonstrated that soils formed on pyroclastic ash deposits are much more common in the Mediterranean area than previously assumed. These soils are an important key to understanding past volcanic events and landscape evolution. Chronological information in soils of Quaternary volcanic events, however, remains still poorly understood in southern Italy. Using a multi-method forensic approach, we explore the origin and age of volcanic deposits (soils) in Sicily and Calabria. The geochemical signature of the soil was compared to the chemical fingerprint of the magmas of potential source areas of southern Italian volcanoes. The results indicate that the investigated soils on t…

010504 meteorology & atmospheric sciencesEarth science1904 Earth-Surface ProcessesGeo-forensicPyroclastic rockWeatheringVolcanism010502 geochemistry & geophysics01 natural scienceslaw.inventionQuaternarylawVolcanic sedimentRadiocarbon dating910 Geography & travel0105 earth and related environmental sciencesEarth-Surface ProcessesgeographySoil evolutiongeography.geographical_feature_categoryBedrockEarth15. Life on land10122 Institute of GeographySurface ProcessesVolcanoSettore AGR/14 - PedologiaClastic rockDatingTephrochronologyGeologyCATENA
researchProduct

Oligo-Miocene lacustrine microbial and metazoan buildups from the Limagne Basin (French Massif Central)

2018

The Limagne Basin (French Massif Central) is an extensive continental lacustrine system accommodating microbial and metazoan buildups from Chattian to Aquitanian age. A description of these buildups and their associated biotic components in Grand Gandaillat and Crechy quarries provides insights into their spatio-temporal distribution patterns. Flats, cauliflowers, domes, cones and coalescent columnar morphologies have been identified with a main laminated mesofabric and laminated, columnar, filamentous and caddisfly-coated microfabrics. Two low-gradient margin models emerged based on the changes in the distribution, morphology and size of the microbial and metazoan-rich deposits through tim…

010504 meteorology & atmospheric sciencesGeochemistryCarbonatesVolcanismEcological successionStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesVolcanismMarlCycle ClimateEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryPaleontologyMassif15. Life on landTectonicTectonicsVolcanoSedimentary rockLacustrine/palustrine[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
researchProduct

Explosive eruptive history of Pantelleria, Italy: Repeated caldera collapse and ignimbrite emplacement at a peralkaline volcano

2018

A new, pre-Green Tuff (46 ka) volcanic stratigraphy is presented for the peralkaline Pantelleria Volcano, Italy. New 40Ar/39Ar and paleomagnetic data are combined with detailed field studies to develop a comprehensive stratigraphic reconstruction of the island.We find that the pre-46 ka succession is characterised by eight silicarich peralkaline (trachyte to pantellerite) ignimbrites,many ofwhich blanketed the entire island. The ignimbrites are typically welded to rheomorphic, and are commonly associated with lithic breccias and/or pumice deposits. They record sustained radial pyroclastic density currents fed by lowpyroclastic fountains. The onset of ignimbrite emplacement is typically prec…

010504 meteorology & atmospheric sciencesGeochemistryPyroclastic rockTrachyte010502 geochemistry & geophysics01 natural sciencesPeralkaline rock40Ar/39Ar datingEffusive eruptionGeochemistry and PetrologyPumiceBreccia[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderaEruptive history0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryIgnimbritesPeralkaline volcanismSettore GEO/07 - Petrologia E PetrografiaSettore GEO/08 - Geochimica E VulcanologiaCaldera collapsePeralkaline volcanism Pantelleria Ignimbrites Caldera collapse Eruptive history 40Ar/39Ar datingGeophysicsVolcano13. Climate actionSeismologyGeologyPantelleria
researchProduct

Reaction path models of magmatic gas scrubbing

2016

Gas-water-rock reactions taking place within volcano-hosted hydrothermal systems scrub reactive, water-soluble species (sulfur, halogens) from the magmatic gas phase, and as such play a major control on the composition of surface gas manifestations. A number of quantitative models of magmatic gas scrubbing have been proposed in the past, but no systematic comparison of model results with observations from natural systems has been carried out, to date. Here, we present the results of novel numerical simulations, in which we initialized models of hydrothermal gas-water-rock at conditions relevant to Icelandic volcanism. We focus on Iceland as an example of a "wet" volcanic region where scrubb…

010504 meteorology & atmospheric sciencesIcelandMineralogychemistry.chemical_elementVolcanism010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationGas phaseHydrothermal systemGeochemistry and PetrologyReaction path0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryEQ3/6GeologyGas emissionsGas-water-rock interactionSulfurMagmatic gas scrubbing; Gas-water-rock interaction; EQ3/6; Hydrothermal systems; IcelandMagmatic gas scrubbingSettore GEO/08 - Geochimica E VulcanologiachemistryVolcano13. Climate actionGeologyData scrubbing
researchProduct

Changes in SO2 Flux Regime at Mt. Etna Captured by Automatically Processed Ultraviolet Camera Data

2019

We used a one-year long SO2 flux record, which was obtained using a novel algorithm for real-time automatic processing of ultraviolet (UV) camera data, to characterize changes in degassing dynamics at the Mt. Etna volcano in 2016. These SO2 flux records, when combined with independent thermal and seismic evidence, allowed for capturing switches in activity from paroxysmal explosive eruptions to quiescent degassing. We found SO2 fluxes 1.5−2 times higher than the 2016 average (1588 tons/day) during the Etna’s May 16−25 eruptive paroxysmal activity, and mild but detectable SO2 flux increases more than one month before its onset. The SO2 flux typically peaked during a lava fo…

010504 meteorology & atmospheric sciencesLava2SO<sub>2</sub> fluxesAutomatic processing010502 geochemistry & geophysicsAtmospheric sciencesmedicine.disease_causeUV Camerafluxe01 natural sciencesFlux (metallurgy)Thermalmedicinelcsh:Scienceexplosive basaltic volcanism0105 earth and related environmental sciencesSOExplosive eruptionEtna VolcanofluxesEtna volcanoGeneral Earth and Planetary Scienceslcsh:QEtna volcano; Explosive basaltic volcanism; SO; 2; fluxes; UV cameraGeologyUltravioletRemote Sensing
researchProduct

Antisana volcano: A representative andesitic volcano of the eastern cordillera of Ecuador: Petrography, chemistry, tephra and glacial stratigraphy

2017

Antisana volcano is representative of many active andesitic strato-volcanoes of Pleistocene age in Ecuador's Eastern Cordillera. This study represents the first modern geological and volcanological investigation of Antisana since the late 1890's; it also summarizes the present geochemical understanding of its genesis. The volcano's development includes the formation and destruction of two older edifices (Antisana I and II) during some 400 + ka. Antisana II suffered a sector collapse about 15,000 years ago which was followed by the birth and growth of Antisana III. During its short life Antisana III has generated >= 50 eruptions of small to medium intensity, often associated with andesitic t…

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesLong-lived evolving andesitic volcanism[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPlagioclaseTephra0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyAndesitesAndesiteNorthern Volcanic ZoneGeologybiology.organism_classificationVolcano13. Climate actionAntisanaMagmaengineeringPhenocrystGeologyJournal of South American Earth Sciences
researchProduct

Thematic vent opening probability maps and hazard assessment of small-scale pyroclastic density currents in the San Salvador volcanic complex (El Sal…

2021

The San Salvador volcanic complex (El Salvador) and Nejapa-Chiltepe volcanic complex (Nicaragua) have been characterized by a significant variability in eruption style and vent location. Densely inhabited cities are built on them and their surroundings, including the metropolitan areas of San Salvador (∼2.4 million people) and Managua (∼1.4 million people), respectively. In this study we present novel vent opening probability maps for these volcanic complexes, which are based on a multi-model approach that relies on kernel density estimators. In particular, we present thematic vent opening maps, i.e., we consider different hazardous phenomena separately, including lava emission, small-scale…

010504 meteorology & atmospheric sciencesLavaPyroclastic rockVolcanismHazard analysis010502 geochemistry & geophysicsHazard mapvolcanic hazard mapping01 natural sciencesEnvironmental technology. Sanitary engineeringGPhreatomagmatic eruptionGeography. Anthropology. Recreation[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGE1-350TD1-10660105 earth and related environmental sciencesgeographyQE1-996.5geography.geographical_feature_categoryGeologyEnvironmental sciencesThematic mapVolcano13. Climate actionGeneral Earth and Planetary Sciencesvent opening hazard map San Salvador volcano Nejapa-Chiltepe volcanic zoneGeologySeismology
researchProduct

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
researchProduct

Submarine morphology of the Comoros volcanic archipelago

2021

co-auteur étranger; International audience; A detailed morpho-bathymetric study of the Comoros archipelago, based on mostly unpublished bathymetric data, provides a first glimpse into the submarine section of these islands. It offers a complete view of the distribution of volcanic structures around the archipelago, allowing to discuss the origin and evolution of this volcanism. Numerous volcanic cones and erosional-depositional features have been recognized throughout the archipelago. The magmatic supply is focused below one or several volcanoes for each island, but is also controlled by lithospheric fractures evidenced by volcanic ridges, oriented along the supposed Lwandle-Somali plate bo…

010504 meteorology & atmospheric sciencesVolcanic ridges[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographySubmarine volcanismVolcanism010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyComoros archipelagoGeochemistry and PetrologyLithosphereComoros archipelago Mass slope instabilities Morpho-bathymetry Mounds Submarine volcanism Volcanic cones Volcanic ridges[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyVolcanic conesMass slope instabilitiesBathymetry14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMorpho-bathymetrySubmarineGeologyPlate tectonicsVolcanoArchipelagoMoundsVolcanic coneGeology
researchProduct