Articles | Volume 25, issue 9
https://doi.org/10.5194/nhess-25-3559-2025
https://doi.org/10.5194/nhess-25-3559-2025
Research article
 | 
23 Sep 2025
Research article |  | 23 Sep 2025

The Parraguirre ice–rock avalanche 1987, semi-arid Andes, Chile – a holistic revision

Johannes J. Fürst, David Farías-Barahona, Thomas Bruckner, Lucia Scaff, Martin Mergili, Santiago Montserrat, and Humberto Peña

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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 egusphere-2024-3103', Anonymous Referee #1, 21 Apr 2025
    • AC1: 'Reply on RC1', Johannes J. Fürst, 27 May 2025
  • RC2: 'Comment on egusphere-2024-3103', Anonymous Referee #2, 24 Apr 2025
    • AC3: 'Reply on RC2', Johannes J. Fürst, 27 May 2025
  • RC3: 'Comment on egusphere-2024-3103', Anonymous Referee #3, 27 Apr 2025
    • AC2: 'Reply on RC3', Johannes J. Fürst, 27 May 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish as is (13 Jun 2025) by Bayes Ahmed
AR by Johannes J. Fürst on behalf of the Authors (23 Jun 2025)  Manuscript 
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Short summary
The 1987 Parraguirre ice–rock avalanche developed into a devastating debris flow, causing the loss of many lives and inflicting severe damage near Santiago, Chile. Here, we revise this event, combining various observational records with modelling techniques. In that year, important snow cover coincided with persistent warm periods in spring. We also put forward upward corrections for the trigger and flood volumes involved in this debris flow. Finally, temporary river damming was key for the flow ferocity.
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