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

Author

Listed:
  • Daniele Andronico

    (Istituto Nazionale di Geofisica e Vulcanologia-Osservatorio Etneo, Sezione di Catania)

  • Elisabetta Bello

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Roma 1)

  • Claudia D’Oriano

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Pisa)

  • Patrizia Landi

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Pisa)

  • Federica Pardini

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Pisa)

  • Piergiorgio Scarlato

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Roma 1)

  • Mattia de’ Michieli Vitturi

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Pisa
    University at Buffalo)

  • Jacopo Taddeucci

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Roma 1)

  • Antonino Cristaldi

    (Istituto Nazionale di Geofisica e Vulcanologia-Osservatorio Etneo, Sezione di Catania)

  • Francesco Ciancitto

    (Istituto Nazionale di Geofisica e Vulcanologia-Osservatorio Etneo, Sezione di Catania)

  • Francesco Pennacchia

    (Università di Roma Tre)

  • Tullio Ricci

    (Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Roma 1)

  • Federico Valentini

    (Piazza Santa Maria Ausiliatrice, 10)

Abstract

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 × 107 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.

Suggested Citation

  • Daniele Andronico & Elisabetta Bello & Claudia D’Oriano & Patrizia Landi & Federica Pardini & Piergiorgio Scarlato & Mattia de’ Michieli Vitturi & Jacopo Taddeucci & Antonino Cristaldi & Francesco Cia, 2021. "Uncovering the eruptive patterns of the 2019 double paroxysm eruption crisis of Stromboli volcano," Nature Communications, Nature, vol. 12(1), pages 1-14, December.
  • Handle: RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-24420-1
    DOI: 10.1038/s41467-021-24420-1
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    Cited by:

    1. Chiara Maria Petrone & Silvio Mollo & Ralf Gertisser & Yannick Buret & Piergiorgio Scarlato & Elisabetta Bello & Daniele Andronico & Ben Ellis & Alessio Pontesilli & Gianfilippo Astis & Pier Paolo Gia, 2022. "Magma recharge and mush rejuvenation drive paroxysmal activity at Stromboli volcano," Nature Communications, Nature, vol. 13(1), pages 1-17, December.

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