Articles | Volume 25, issue 12
https://doi.org/10.5194/nhess-25-4843-2025
https://doi.org/10.5194/nhess-25-4843-2025
Research article
 | 
05 Dec 2025
Research article |  | 05 Dec 2025

Controls over debris flow initiation in glacio-volcanic environments in the Southern Andes

Ivo Fustos-Toribio, Daniel Basualto, Ardy Gatica, Alvaro Bravo-Alarcón, José-Luis Palma, Gabriel Fuentealba, and Sergio A. Sepúlveda

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Cited articles

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Bogaard, T. A. and Greco, R.: Landslide hydrology: from hydrology to pore pressure, WIREs Water, 3, 439–459, https://doi.org/10.1002/wat2.1126, 2015. 
Bordoni, M., Vivaldi, V., Ciabatta, L., Brocca, L., and Meisina, C.: Temporal prediction of shallow landslides exploiting soil saturation degree derived by ERA5-Land products, B. Eng. Geol. Environ., 82, https://doi.org/10.1007/s10064-023-03304-2, 2023. 
Bovis, M. J. and Jakob, M.: The role of debris supply conditions in predicting debris flow activity, Earth Surf. Proc. Land., 24, 1039–1054, https://doi.org/10.1002/(SICI)1096-9837(199910)24:11<1039::AID-ESP29>3.0.CO;2-U, 1999. 
Bucher, J., del Papa, C., Hernando, I. R., and Almada, G.: Upper-flow-regime deposits related to glacio-volcanic interactions in Patagonia: Insights from the Pleistocene record in Southern Andes, Sedimentology, 71, 2314–2334, https://doi.org/10.1111/sed.13216, 2024. 
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Short summary
We investigated how volcanic soils and heavy rainfall trigger dangerous debris flows in the southern Andes. Our findings show saturated volcanic-soils above less permeable glacial deposits create ideal conditions for slope failures. Monitoring soil moisture and surface changes helps predict these events. This knowledge aids in protecting communities from debris flow hazards, increasingly important under climate change.
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