Articles | Volume 24, issue 10
https://doi.org/10.5194/nhess-24-3401-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-24-3401-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Co- and postseismic subaquatic evidence for prehistoric fault activity near Coyhaique, Aysén Region, Chile
Renard Centre of Marine Geology (RCMG), Department of Geology, Ghent University, 9000 Ghent, Belgium
Katleen Wils
Renard Centre of Marine Geology (RCMG), Department of Geology, Ghent University, 9000 Ghent, Belgium
Kris Vanneste
Royal Observatory of Belgium, 1180 Brussels, Belgium
Roberto Urrutia
Centro EULA, Universidad de Concepción, Casilla 160-C, Concepción, Chile
Mario Pino
Instituto de Ciencias de la Tierra, Universidad Austral de Chile, Casilla 567, Valdivia, Chile
Catherine Kissel
Laboratoire des Sciences du Climat et de l'Environnement/IPSL, CEA/CNRS/UVSQ, Université Paris-Saclay, 91198 Gif-sur-Yvette, France
Marc De Batist
Renard Centre of Marine Geology (RCMG), Department of Geology, Ghent University, 9000 Ghent, Belgium
Maarten Van Daele
Renard Centre of Marine Geology (RCMG), Department of Geology, Ghent University, 9000 Ghent, Belgium
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Short summary
This study identifies a prehistoric earthquake around 4400 years ago near the city of Coyhaique (Aysén Region, Chilean Patagonia) and illustrates the potential seismic hazard in the region. We found deposits in lakes and a fjord that can be related to subaquatic and onshore landslides, all with a similar age, indicating that they were most likely caused by an earthquake. Through modeling we found that this was an earthquake of magnitude 6.3 to 7.0 on a fault near the city of Coyhaique.
This study identifies a prehistoric earthquake around 4400 years ago near the city of Coyhaique...
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