0000000000435305

AUTHOR

Mauro Rosi

showing 2 related works from this author

Ground deformation reveals the scale-invariant conduit dynamics driving explosive basaltic eruptions

2021

The mild activity of basaltic volcanoes is punctuated by violent explosive eruptions that occur without obvious precursors. Modelling the source processes of these sudden blasts is challenging. Here, we use two decades of ground deformation (tilt) records from Stromboli volcano to shed light, with unprecedented detail, on the short-term (minute-scale) conduit processes that drive such violent volcanic eruptions. We find that explosive eruptions, with source parameters spanning seven orders of magnitude, all share a common pre-blast ground inflation trend. We explain this exponential inflation using a model in which pressure build-up is caused by the rapid expansion of volatile-rich magma ri…

010504 meteorology & atmospheric sciencesExplosive materialScienceGeneral Physics and AstronomyMagnitude (mathematics)VolcanologyDeformation (meteorology)010502 geochemistry & geophysics01 natural sciencestiltGeneral Biochemistry Genetics and Molecular BiologyArticlePhysics::Geophysicsground deformationElectrical conduitOrders of magnitude (specific energy)ground deformation conduit dynamics early warningAstrophysics::Solar and Stellar AstrophysicsStromboli0105 earth and related environmental sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryExplosive eruptionQGeneral ChemistryGeophysicsVolcanoMagmaSeismologyGeologyNature Communications
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The 15 March 2007 explosive crisis at Stromboli Volcano, Italy: assessing physical parameters through a multidisciplinary approach

2011

Basaltic volcanoes are dominated by lava emission and mild explosive activity. Nevertheless, many basaltic systems exhibit, from time to time, poorly documented and little-understood violent explosions. A short-lived, multiblast explosive crisis (paroxysmal explosion) occurred on 15 March 2007 during an effusive eruptive crisis at Stromboli (Italy). The explosive crisis, which started at 20:38:14 UT, had a total duration of ∼5 min. The combined use of multiparametric data collected by the permanent instrumental networks (seismic, acoustic, and thermal records) and a field survey carried out immediately after the event enabled us to constrain the eruptive dynamics and quantify physical param…

DYNAMICSAtmospheric ScienceExplosive materialLavaPyroclastic flowSoil SciencePyroclastic rockAquatic ScienceOceanographyGeophysical monitoringEffusive eruptionImpact craterDEFORMATIONGeochemistry and Petrologyddc:550SR ISOTOPE EVIDENCE; EFFUSIVE ERUPTION; PAROXYSMAL EXPLOSION; PLUMBING SYSTEM; DYNAMICS; DEFORMATION; INSIGHTS; EVENT; TIME; CRYSTALLIZATIONEarth and Planetary Sciences (miscellaneous)StromboliParoxysmTephraEarth-Surface ProcessesWater Science and TechnologySR ISOTOPE EVIDENCEgeographygeography.geographical_feature_categoryEcologyTephra depositPLUMBING SYSTEMEFFUSIVE ERUPTIONPaleontologyForestryBallistic ejectionPAROXYSMAL EXPLOSIONVOLCANOLOGY INFRASOUND FALL-OUTTIMEINSIGHTSGeophysicsEVENTVolcanoSpace and Planetary ScienceCRYSTALLIZATIONScoriaGeologySeismology
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