Articles | Volume 12, issue 4
https://doi.org/10.5194/se-12-801-2021
© Author(s) 2021. 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-12-801-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Apr 2021
Research article |
| 13 Apr 2021
| 13 Apr 2021
Mapping and evaluating kinematics and the stress and strain field at active faults and fissures: a comparison between field and drone data at the NE rift, Mt Etna (Italy)
Alessandro Tibaldi
CORRESPONDING AUTHOR
Department of Earth and Environmental Sciences, University of Milan-Bicocca, Milan, Italy
CRUST – Interuniversity Center for 3D Seismotectonics with Territorial Applications, Chieti, Italy
Noemi Corti
Department of Earth and Environmental Sciences, University of Milan-Bicocca, Milan, Italy
Emanuela De Beni
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
Fabio Luca Bonali
Department of Earth and Environmental Sciences, University of Milan-Bicocca, Milan, Italy
CRUST – Interuniversity Center for 3D Seismotectonics with Territorial Applications, Chieti, Italy
Susanna Falsaperla
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
Horst Langer
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
Marco Neri
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
Massimo Cantarero
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
Danilo Reitano
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Sezione di Catania, Catania, Italy
Luca Fallati
Department of Earth and Environmental Sciences, University of Milan-Bicocca, Milan, Italy
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Short summary
The Northeast Rift of Mt Etna is affected by ground deformation linked to gravity sliding of the volcano flank and dike injection. Drone surveys show that the rift is affected by NE-striking extensional fractures and normal faults. Given an age of 1614 CE for the offset lavas, we obtained an extension rate of 1.9 cm yr−1 for the last 406 years. The stress field is characterised by a NW–SE σHmin. Drone surveys allow us to quickly collect data with a resolution of 2–3 cm.
The Northeast Rift of Mt Etna is affected by ground deformation linked to gravity sliding of the...
