Tsunami risk management for crustal earthquakes and non-seismic sources in Italy

J Selva, A Amato, A Armigliato, R Basili… - La Rivista del Nuovo …, 2021 - Springer
Destructive tsunamis are most often generated by large earthquakes occurring at subduction
interfaces, but also other “atypical” sources—defined as crustal earthquakes and non …

[HTML][HTML] A guide to recognising slow-moving subaqueous landslides in seismic and bathymetry datasets

B Couvin, A Georgiopoulou, LA Amy - Earth-Science Reviews, 2024 - Elsevier
Slow-moving subaqueous landslides (SMSL) have been recognised in many studies from
seafloor bathymetric and seismic data, based on shared morphological characteristics with …

Gravitational collapse of Mount Etna's southeastern flank

M Urlaub, F Petersen, F Gross, A Bonforte, G Puglisi… - Science …, 2018 - science.org
The southeastern flank of Etna volcano slides into the Ionian Sea at rates of centimeters per
year. The prevailing understanding is that pressurization of the magmatic system, and not …

[HTML][HTML] Evidence of the Zanclean megaflood in the eastern Mediterranean Basin

A Micallef, A Camerlenghi, D Garcia-Castellanos… - Scientific Reports, 2018 - nature.com
The Messinian salinity crisis (MSC)-the most abrupt, global-scale environmental change
since the end of the Cretaceous–is widely associated with partial desiccation of the …

Crustal structure of the Ionian basin and eastern Sicily margin: Results from a wide‐angle seismic survey

D Dellong, F Klingelhoefer, H Kopp… - Journal of …, 2018 - Wiley Online Library
Abstract In the Ionian Sea (central Mediterranean) the slow convergence between Africa and
Eurasia results in the formation of a narrow subduction zone. The nature of the crust of the …

Sentinel-1 Interferometry and UAV Aerial Survey for Mapping Coseismic Ruptures: Mts. Sibillini vs. Mt. Etna Volcano

M Menichetti, M Roccheggiani, G De Guidi… - Remote Sensing, 2023 - mdpi.com
The survey and structural analysis of surface coseismic ruptures are essential tools for
characterizing seismogenic structures. In this work, a procedure to survey coseismic …

The spectrum of persistent volcanic flank instability: A review and proposed framework based on Kīlauea, Piton de la Fournaise, and Etna

MP Poland, A Peltier, A Bonforte, G Puglisi - Journal of Volcanology and …, 2017 - Elsevier
Persistent motion of the south flank of Kīlauea Volcano, Hawai'i, has been known for several
decades, but has only recently been identified at other large basaltic volcanoes—namely …

Deformation pattern of the northern sector of the Malta escarpment (Offshore SE Sicily, Italy): fault dimension, slip prediction, and seismotectonic implications

S Gambino, G Barreca, F Gross, C Monaco… - Frontiers in Earth …, 2021 - frontiersin.org
Marine seismic reflection data coupled with on-land structural measurements improve our
knowledge about the active deformation pattern of the northern sector of the Malta …

Slow slip events and flank instability at Mt. Etna volcano (Italy)

M Palano, F Sparacino, P Gambino, N D'Agostino… - Tectonophysics, 2022 - Elsevier
We analyzed a set of 11 slow slip events occurred during the 2006–2016 period and
affecting the GNSS (Global Navigation Satellite System) stations of the unstable flank of Mt …

Fault rupture and aseismic creep accompanying the December 26, 2018, Mw 4.9 Fleri earthquake (Mt. Etna, Italy): Factors affecting the surface faulting in a volcano …

G Tringali, D Bella, F Livio, MF Ferrario… - Quaternary …, 2023 - Elsevier
Abstract On December 26, 2018 (2: 19 UTC), during a volcanic eruption on the Mt. Etna
eastern flank (Sicily, southern Italy), the largest instrumental earthquake ever recorded in the …