A gas-slug model for basaltic Vulcanian eruptions at open-conduit volcanoes, constrained by textural characteristics and dynamics of the July 3rd, 2019, Stromboli eruption (Italy)

Stromboli is a unique open-conduit mafic volcano known for persistent Strombolian eruptions of highly porphyritic (HP) basalticshoshonite scoria. Stronger paroxysmal explosions occur once or twice per decade, ejecting low porphyritic (LP) golden pumice from deeper volatile-rich magma. The July 3rd, 2019, paroxysm showed features of a Vulcanian eruption—supersonic blast, ballistic ejection, and pyroclastic flows—despite Stromboli’s open-conduit basaltic nature. Textural analysis suggests that LP pyroclasts formed via rapid decompression, fragmentation, and quenching. This event likely resulted from shallow HP-filled conduit pressurization and failure triggered by a rising large gas slug. This caused top-down decompression, evacuating both HP and deeper LP magma. The proposed “basaltic Vulcanian” model better fits geophysical data than the traditional deep LP magma ascent model.

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Publication Details

Journal
Volcanica
Published
2026-02-11
DOI
https://doi.org/10.30909/vol/iajq5592
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
0.00

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article

A gas-slug model for basaltic Vulcanian eruptions at open-conduit volcanoes, constrained by textural characteristics and dynamics of the July 3rd, 2019, Stromboli eruption (Italy)

G. De Astis, Danilo Di Genova, Monica Piochi, Luca Caricchi et al.
Volcanica
Geological and Geochemical Analysis
article

A gas-slug model for basaltic Vulcanian eruptions at open-conduit volcanoes, constrained by textural characteristics and dynamics of the July 3rd, 2019, Stromboli eruption (Italy)

G. De Astis, Danilo Di Genova, Monica Piochi, Luca Caricchi, Marco Viccaro, Gerardo Carrasco-Núnez, Alessandro Frontoni, Laura Calabrò, Alessandro Vona, Teresa Oreade Grillo, Giuseppe La Spina, Guido Giordano, Riccardo Russo, Alessandro Aiuppa
article en

Abstract

Stromboli is a unique open-conduit mafic volcano known for persistent Strombolian eruptions of highly porphyritic (HP) basalticshoshonite scoria. Stronger paroxysmal explosions occur once or twice per decade, ejecting low porphyritic (LP) golden pumice from deeper volatile-rich magma. The July 3rd, 2019, paroxysm showed features of a Vulcanian eruption—supersonic blast, ballistic ejection, and pyroclastic flows—despite Stromboli’s open-conduit basaltic nature. Textural analysis suggests that LP pyroclasts formed via rapid decompression, fragmentation, and quenching. This event likely resulted from shallow HP-filled conduit pressurization and failure triggered by a rising large gas slug. This caused top-down decompression, evacuating both HP and deeper LP magma. The proposed “basaltic Vulcanian” model better fits geophysical data than the traditional deep LP magma ascent model.

VolcanicaVol. 9(1)
University of Geneva (CH), Roma Tre University (IT), Istituto Nazionale di Geofisica e Vulcanologia (IT), University of Catania (IT), Institute of Science and Technology for Ceramics (IT), Universidad Nacional Autónoma de México (MX), University of Palermo (IT)
Università degli Studi Roma Tre, Dipartimenti di Eccellenza, European Commission, Deutsche Forschungsgemeinschaft, Ministero dell’Istruzione, dell’Università e della Ricerca, Istituto Nazionale di Geofisica e Vulcanologia, HORIZON EUROPE Framework Programme
Openalex Percentile: Top 47%
Geological and Geochemical Analysis
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