0000000000154181

AUTHOR

A. Amigo

showing 3 related works from this author

Sustaining persistent lava lakes: Observations from high-resolution gas measurements at Villarrica volcano, Chile

2016

International audience; Active lava lakes – as the exposed upper part of magmatic columns – are prime locations to investigate the conduit flow processes operating at active, degassing volcanoes. Persistent lava lakes require a constant influx of heat to sustain a molten state at the Earth's surface. Several mechanisms have been proposed to explain how such heat transfer can operate efficiently. These models make contrasting predictions with respect to the flow dynamics in volcanic conduits and should result in dissimilar volatile emissions at the surface. Here we look at high-frequency SO2 fluxes, plume composition, thermal emissions and aerial video footage from the Villarrica lava lake i…

010504 meteorology & atmospheric sciencesLavaEarth scienceUAVUV camera010502 geochemistry & geophysics01 natural sciencesElectrical conduitFlux (metallurgy)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeophysic0105 earth and related environmental sciencesgeographyTrail By Firegeography.geographical_feature_categoryTrail ByLava domeFireconduit dynamicPlumeGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGas slugMagmavolcanic degassingGeologyMulti-GAS
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Unrest at the Nevados de Chillán volcanic complex: a failed or yet to unfold magmatic eruption?

2018

Resuming erupting activity at volcanoes that have been long quiescent poses a significant challenge to hazard assessment, as it require assessment of whether the change in activity is an isolated event or the beginning of a new eruptive sequence. Such inception is often poorly characterised as quiescent volcanoes tend to be poorly equipped and not extensively monitored, especially with respect to gas geochemistry. Here, we report gas composition and flux measurements from a newly opened vent at the very onset of eruptive activity at the Nevados de Chillán volcanic complex (Chile) in January-February 2016. The molar proportions of H2O, CO2, SO2, H2S and H2 gases are found to be 98.4, 0.97, 0…

event.disaster_typeBasaltTrail By FireQE1-996.5geographygeography.geographical_feature_categoryAndesiteGeochemistryUV cameraGeologyEruption triggerDaciteVolcanic GasesBasaltic andesiteLithic fragmentVolcanoVolcanic unrestMagma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanologyevent[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentVolcanic gasesMulti-GASGeology
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Extraordinary sediment delivery and rapid geomorphic response following the 2008-2009 eruption of Chaitén Volcano, Chile

2016

U.S. Geological Survey Volcano Science Center SERNAGEOMIN's Programa de Riesgos Volcanicos Conicyt Fondecyt grants 1110609 1141064 11130671 Conicyt Fondap 15090013 Vamos Research Centre

HydrologySediment yieldgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesSediment010502 geochemistry & geophysics01 natural sciencesVolcanoHyperconcentrated flowResearch centreGeological surveySuspended loadGeomorphologyGeology0105 earth and related environmental sciencesWater Science and TechnologyWater Resources Research
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