Articles | Volume 21, issue 10
Nat. Hazards Earth Syst. Sci., 21, 3015–3029, 2021
https://doi.org/10.5194/nhess-21-3015-2021
Nat. Hazards Earth Syst. Sci., 21, 3015–3029, 2021
https://doi.org/10.5194/nhess-21-3015-2021

Research article 08 Oct 2021

Research article | 08 Oct 2021

Debris flow event on Osorno volcano, Chile, during summer 2017: new interpretations for chain processes in the southern Andes

Ivo Janos Fustos-Toribio et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2021-74', Roberto J. Marin, 18 Apr 2021
    • AC1: 'Reply on RC1', Ivo Fustos, 03 Aug 2021
  • RC2: 'Comment on nhess-2021-74', Anonymous Referee #2, 11 Jul 2021
    • AC2: 'Reply on RC2', Ivo Fustos, 03 Aug 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (16 Aug 2021) by Giovanni Macedonio
AR by Ivo Fustos on behalf of the Authors (20 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (08 Sep 2021) by Giovanni Macedonio
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Short summary
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.
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