Uncovering the eruptive patterns of the 2019 double paroxysm eruption crisis of Stromboli volcano

In 2019, Stromboli volcano experienced one of the most violent eruptive crises in the last hundred years. Two paroxysmal explosions interrupted the ‘normal’ mild explosive activity during the tourist season. Here we integrate visual and field observations, textural and chemical data of eruptive prod...

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Veröffentlicht in:Nature communications 2021-07, Vol.12 (1), p.4213-4213, Article 4213
Hauptverfasser: Andronico, Daniele, Del Bello, Elisabetta, D’Oriano, Claudia, Landi, Patrizia, Pardini, Federica, Scarlato, Piergiorgio, de’ Michieli Vitturi, Mattia, Taddeucci, Jacopo, Cristaldi, Antonino, Ciancitto, Francesco, Pennacchia, Francesco, Ricci, Tullio, Valentini, Federico
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Sprache:eng
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Zusammenfassung:In 2019, Stromboli volcano experienced one of the most violent eruptive crises in the last hundred years. Two paroxysmal explosions interrupted the ‘normal’ mild explosive activity during the tourist season. Here we integrate visual and field observations, textural and chemical data of eruptive products, and numerical simulations to analyze the eruptive patterns leading to the paroxysmal explosions. Heralded by 24 days of intensified normal activity and 45 min of lava outpouring, on 3 July a paroxysm ejected ~6 × 10 7  kg of bombs, lapilli and ash up to 6 km high, damaging the monitoring network and falling towards SW on the inhabited areas. Intensified activity continued until the less energetic, 28 August paroxysm, which dispersed tephra mainly towards NE. We argue that all paroxysms at Stromboli share a common pre-eruptive weeks-to months-long unrest phase, marking the perturbation of the magmatic system. Our analysis points to an urgent implementation of volcanic monitoring at Stromboli to detect such long-term precursors. Integrated field and laboratory investigations, and numerical simulations of the 2019 paroxysmal explosions at Stromboli volcano revealed that they were anticipated by a week-to-month-long destabilization in the normal volcanic activity, a pattern common to all paroxysms.
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-021-24420-1