Articles | Volume 17, issue 2
https://doi.org/10.5194/se-17-311-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-17-311-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The role of fault network geometry on the complexity of seismic cycles in the Apennines
Constanza Rodriguez Piceda
CORRESPONDING AUTHOR
University of Plymouth, School of Geography, Earth and Environmental Sciences, Plymouth, PL4 8AA, United Kingdom
GFZ Helmholtz Centre for Geosciences, Potsdam, 14473, Germany
Zoë K. Mildon
University of Plymouth, School of Geography, Earth and Environmental Sciences, Plymouth, PL4 8AA, United Kingdom
Billy J. Andrews
University of Plymouth, School of Geography, Earth and Environmental Sciences, Plymouth, PL4 8AA, United Kingdom
Yifan Yin
MIT Department of Earth, Atmospheric and Planetary Science, Cambridge, MA 02139, United States
Jean-Paul Ampuero
Université Côte d'Azur, Observatoire de la Côte d'Azur, IRD, CNRS, Géo azur, Valbonne, 06905, France
Martijn van den Ende
Université Côte d'Azur, Observatoire de la Côte d'Azur, IRD, CNRS, Géo azur, Valbonne, 06905, France
Claudia Sgambato
Birkbeck University of London, London, WC1E 7HX, United Kingdom
Percy Galvez
Everest Group, Zürich, 8001, Switzerland
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Short summary
Short summary
On 2 October 2020, the French Maritime Alps were struck by an extreme rainfall event caused by Storm Alex. Here, we show that seismic data provide the timing and velocity of the propagation of flash-flood waves along the Vésubie River. We also detect 114 small local earthquakes triggered by the rainwater weight and/or its infiltration into the ground. This study paves the way for future works that can reveal further details of the impact of Storm Alex on the Earth’s surface and subsurface.
Martijn P. A. van den Ende and Jean-Paul Ampuero
Solid Earth, 12, 915–934, https://doi.org/10.5194/se-12-915-2021, https://doi.org/10.5194/se-12-915-2021, 2021
Short summary
Short summary
Distributed acoustic sensing (DAS) is an emerging technology that measures stretching of an optical-fibre cable. This technology can be used to record the ground shaking of earthquakes, which offers a cost-efficient alternative to conventional seismometers. Since DAS is relatively new, we need to verify that existing seismological methods can be applied to this new data type. In this study, we reveal several issues by comparing DAS with conventional seismometer data for earthquake localisation.
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Short summary
We investigate how the spatial arrangement of normal faults in the Italian Apennines affects earthquake timing and size. Computer-based models show that wide networks with faults offset across-strike produce more irregular and variable earthquakes, while narrow networks with fewer across-strike faults lead to more regular events. Faster-moving faults are more sensitive to nearby positive stress interactions, highlighting the need to consider fault geometry in seismic hazard assessments.
We investigate how the spatial arrangement of normal faults in the Italian Apennines affects...