The morphological response to the 13 May 2022 major explosive event at Stromboli volcano, Italy, characterised by high-resolution UAS surveys

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Markus Schmid
Ulrich Kueppers
https://orcid.org/0000-0003-2815-1444
Tullio Ricci
https://orcid.org/0000-0002-0553-5384
Riccardo Civico
https://orcid.org/0000-0002-5015-2155
Valeria Cigala
https://orcid.org/0000-0003-2410-136X
David Fee
https://orcid.org/0000-0002-0936-9977
Julia E. Gestrich
https://orcid.org/0000-0001-8663-1388
Alexandra M. Iezzi
https://orcid.org/0000-0002-6782-7681
Corrado Cimarelli
Caron E. J. Vossen
Richard M. Buzard
Maurizio Ripepe
Giorgio Lacanna
Donald B. Dingwell
https://orcid.org/0000-0002-3332-789X

Abstract

Since 2019, the frequency of major explosive eruptions at Stromboli volcano (Italy) has increased, heightening the exposure of population and scientists to the hazards posed by ejecta. Morphological changes can directly alter the hazard potential associated with these phenomena. Here, we present a quantitative morphological analysis of changes of the crater terrace area linked to the 13 May 2022 major explosive event. High resolution (2.5 cm pixel-1) aerial imagery was acquired by unoccupied aircraft systems 2 hours before and 19 hours after the event. The 13 May 2022 major explosive event consisted of a minimum of seven explosions from four vents located in the south-central crater area. The opportune timing of this campaign enabled the quantification of morphological changes at Stromboli related to a single major explosive event at high temporal and spatial resolution. A total of 12.7 × 103 m3 was excavated and 5.5 × 103 m3 deposited. Via the mapping and classification of bomb distributions we observe that angular blocks make up the largest fraction of ballistics >0.2 m, from which we infer a strong interaction with wall rock and/or fragmentation of solidified plugs in the shallow plumbing system. The morphological changes observed provide valuable constraints on how much material is displaced, and the shift in location and the number of active vents during major explosive events at Stromboli.

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How to Cite
Schmid, M., Kueppers, U., Ricci, T., Civico, R., Cigala, V., Fee, D., Gestrich, J. E., Iezzi, A. M., Cimarelli, C., Vossen, C. E. J., Buzard, R. M., Ripepe, M., Lacanna, G. and Dingwell, D. B. (2025) “The morphological response to the 13 May 2022 major explosive event at Stromboli volcano, Italy, characterised by high-resolution UAS surveys”, Volcanica, 8(2), pp. 387–397. doi: 10.30909/vol/crjj4989.
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Articles
Author Biographies

David Fee, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA

Secondary Affiliation:

 Alaska Volcano Observatory, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA

Julia E. Gestrich, Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, 80333 Munich, Germany

Secondary Affiliation: 

Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA

Alexandra M. Iezzi, U.S. Geological Survey, Volcano Science Center, Cascades Volcano Observatory, Vancouver, WA, USA

Second Affiliation: Department of Earth Science and Earth Research Institute, University of California, Santa Barbara, CA, USA

Richard M. Buzard, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA

Secondary Affiliation: 

U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA, USA

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Dates
Received 2024-05-22
Accepted 2025-05-25
Published 2025-08-26
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