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Articles | Volume 16, issue 12
Articles | Volume 16, issue 12
https://doi.org/10.5194/se-16-1473-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-16-1473-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 12
Research article
 | 
02 Dec 2025
Research article |  | 02 Dec 2025

New paleoseismological and morphotectonic investigations along the 2018 surface ruptures of the Fiandaca Fault, eastern flank of Etna volcano (Italy)

Giorgio Tringali, Domenico Bella, Franz A. Livio, Anna Maria Blumetti, Gianluca Groppelli, Luca Guerrieri, Marco Neri, Vincenzo Adorno, Rosario Pettinato, Sara Trotta, and Alessandro M. Michetti

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Short summary
Trenches were excavated along the Fiandaca Fault providing data for relocating buildings damaged by the 2018 Mt. Etna earthquake. The paleoseismological results revealed 3 surface faulting events occurred in: 2018, 1894 and an unknown one in the Early Middle Ages. To verify a possible increase in seismicity, fault scarps were analysed conceptualizing a kinematic model and obtaining throw rate growth in the last 2 kyrs.
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