Search results for "Explosive eruption"

showing 4 items of 24 documents

Phase petrology reveals shallow magma storage prior to large explosive silicic eruptions at Hekla volcano, Iceland

2017

Abstract Understanding the conditions that culminate in explosive eruptions of silicic magma is of great importance for volcanic hazard assessment and crisis mitigation. However, geological records of active volcanoes typically show a wide range of eruptive behavior and magnitude, which can vary dramatically for individual eruptive centers. In order to evaluate possible future scenarios of eruption precursors, magmatic system variables for different eruption types need to be constrained. Here we use petrological experiments and microanalysis of crystals to clarify the P – T – x state under which rhyodacitic melts accumulated prior to the H3 eruption; the largest Holocene Plinian eruption of…

geographyVulcanian eruptionExplosive eruptiongeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySilicicMagma chamber010502 geochemistry & geophysics01 natural sciencesGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyPumiceMagmaddc:550Earth and Planetary Sciences (miscellaneous)PhenocrystPetrologyGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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Explosive eruptions with little warning: Experimental petrology and volcano monitoring observations from the 2014 eruption of Kelud, Indonesia

2019

Explosive eruptions that occur with little or no precursory unrest (less than a month) pose the greatest hazards from volcanoes to nearby populations. Here we focus on the preeruptive conditions for these explosive events, their triggers and how these eruptions evolve. We concentrate on Kelud volcano, where we have conducted a set of petrological experiments to understand preeruptive storage conditions for several recent eruptions. For the 2014 explosive eruption, we combine this with an analysis of interferometric synthetic aperture radar measured deformation. Our data suggest that both explosive and effusive eruptions at Kelud are sourced from a magma storage system at 2-4 km. However, ex…

geographygeography.geographical_feature_categoryExplosive eruption010504 meteorology & atmospheric sciencesExplosive materialmagmaexplosive eruptionsUnrest010502 geochemistry & geophysics01 natural sciencespetrologyOverpressureInSARGeophysicsEffusive eruptionvolcanoVolcanoGeochemistry and PetrologyMagmaInterferometric synthetic aperture radarunrestPetrologyGeologySciences exactes et naturelles0105 earth and related environmental sciences
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Long-term changes in explosive and effusive behaviour at andesitic arc volcanoes: Chronostratigraphy of the Centre Hills Volcano, Montserrat

2017

Volcanism on Montserrat (Lesser Antilles arc) has migrated southwards since the formation of the Silver Hills ~ 2.5 Ma, and has formed three successively active volcanic centres. The Centre Hills volcano was the focus of volcanism from ~ 1–0.4 Ma, before activity commenced at the currently active Soufrière Hills volcano. The history of activity at these two volcanoes provides an opportunity to investigate the pattern of volcano behaviour on an andesitic arc island over the lifetime of individual volcanoes. Here, we describe the pyroclastic stratigraphy of subaerial exposures around central Montserrat; identifying 11 thick (> 1 m) pumiceous units derived from sustained explosive eruptions…

geographygeography.geographical_feature_categoryExplosive eruption010504 meteorology & atmospheric sciencesLavaGeochemistryPyroclastic rock010502 geochemistry & geophysics01 natural sciencesVolcanic rockGeophysicsEffusive eruptionVolcanoGeochemistry and PetrologyMagmaTephraGeologySeismology0105 earth and related environmental sciences
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New Inferences on Magma Dynamics in Melilitite-Carbonatite Volcanoes: The Case Study of Mt. Vulture (Southern Italy)

2022

This study provides the first micro-thermometric data of fluid inclusions (FIs) in mafic loose (disaggregated) xenocrysts and ultramafic xenoliths in explosive products of the melilitite-carbonatite Mt. Vulture volcano (southern Italy). Pure CO2 late stage FIs hosted in rock-forming minerals of wehrlite xenoliths and clinopyroxene xenocrysts were trapped at the local crust-mantle boundary (32 km). In contrast, trapping pressures within the loose olivine xenocrysts are from 3.2 to 4.5 kbar (8–13 km). Considering the ongoing degassing of mantle-derived CO2 rich gases, together with seismic evidences of the presence of low amount of melts at depth, and the tectonic control of the past volcanic…

micro-thermometryfluid inclusionsGeophysicsexplosive eruptionSettore GEO/07 - Petrologia E PetrografiaGeneral Earth and Planetary SciencesMt. Vulture volcanocarbonatite volcanoeSettore GEO/08 - Geochimica E Vulcanologia
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