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. 2019 Dec 6;9:18542. doi: 10.1038/s41598-019-54949-7

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© The Author(s) 2019, corrected publication 2021

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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(a) Hillshading of Stromboli topo-bathymetric grid with the locations and shape of the simulated landslides based on Fig. 9 showed in Chiocci et al.³³. PDC (Punta Dei Corvi) and PLB (Punta LaBronzo) are the locations of the monitoring gauges managed by the Laboratory of Experimental Geophysics of the Department of Earth Sciences of the University of Florence (http://lgs.geo.unifi.it/). White square shows the location of trenches described in Rosi et al.⁴. The inset shows the vertical cross section of the triggering slide (after Ma et al.¹²). Map was generated using Quantum GIS 2.8.1 software (https://www.qgis.org).