Departamento de Obras Civiles y Geología, Facultad de
Ingeniería, Universidad Católica de Temuco, Rudecindo Ortega 02950,
Temuco, Chile
Department of Forest Sciences, Faculty of Agriculture and Forest
Sciences, Universidad de La Frontera, Av. Francisco Salazar 01145, Temuco,
4780000, Chile
Department of Forest Sciences, Faculty of Agriculture and Forest
Sciences, Universidad de La Frontera, Av. Francisco Salazar 01145, Temuco,
4780000, Chile
Butamallín Research Center for Global Change, University of La
Frontera, Av. Francisco Salazar 01145, Temuco, 4780000, Chile
Pablo Moreno-Yaeger
Department of Civil Engineering, University of La Frontera,
Francisco Salazar 1145, Temuco, Chile
Department of Geoscience, University of Wisconsin–Madison, 1215
West Dayton St., Madison, WI 53706, USA
Ramiro Muñoz-Ramirez
Departamento de Obras Civiles y Geología, Facultad de
Ingeniería, Universidad Católica de Temuco, Rudecindo Ortega 02950,
Temuco, Chile
Ines Rodriguez Araneda
Departamento de Obras Civiles y Geología, Facultad de
Ingeniería, Universidad Católica de Temuco, Rudecindo Ortega 02950,
Temuco, Chile
Ningsheng Chen
Key Laboratory of Mountain Hazards and Surface Processes, Institute
of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu
610041, China
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Cumulative views and downloads
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1,751
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Total article views: 3,607 (including HTML, PDF, and XML)
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Total article views: 1,111 (including HTML, PDF, and XML)
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Links between debris flow and volcanic evolution are an open question in the southern Andes. We modelled the catastrophic debris flow using field data, a geotechnical approach and numerical modelling of the Petrohué event (Chile, 2017). Our results indicated new debris-flow-prone zones. Finally, we propose considering connections between volcanoes and debris flow in the southern Andes.
Links between debris flow and volcanic evolution are an open question in the southern Andes. We...
