EconPapers    
Economics at your fingertips  
 

Geomorphic thresholds for cascading hazards of debris flows and natural dam formation caused by large landslides

Hefryan Sukma Kharismalatri, Takashi Gomi () and Roy C. Sidle
Additional contact information
Hefryan Sukma Kharismalatri: Tokyo University of Agriculture and Technology
Takashi Gomi: Nagoya University
Roy C. Sidle: University of Central Asia

Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, 2025, vol. 121, issue 13, No 19, 15537-15552

Abstract: Abstract This study investigates geomorphic thresholds that control cascading hazards initiated by large landslides (volume > 105 m3), particularly their potential to generate natural dams or transform into debris flows. These two outcomes represent primary pathways in which large landslide debris interacts with channel networks, triggering downstream or upstream hazards. Using a global dataset of 188 large landslides, we analyzed key geomorphic parameters including inflow angle (entry angle of landslide into channel), local relief, and channel gradient. Our findings reveal distinct geomorphic thresholds: natural dams tend to form when landslides enter channels at inflow angles > 60° and encounter channel gradients 10°. Power-law scaling exponents between landslide area and volume were lower for debris flows than for natural dam-forming landslides, reflecting differences in failure depth and mobility. While this study focuses on natural dam formation and debris flows as dominant hazard sequences, other outcomes such as channel infilling with sediment or partial blockage may occur depending on local topography and hydrological conditions. To avoid conflating past observations with future projections, we frame our results as empirical thresholds that help assess the potential for cascading impacts. These insights are particularly relevant for mountain communities in tectonically active regions where limited infrastructure, isolation, and steep terrain amplify hazard exposure. By identifying simple geomorphic thresholds associated with hazard transitions, this study provides a framework for improving risk assessment, early warning strategies, and land use planning to enhance hazard mitigation strategies and support evidence-based land use management.

Keywords: Landslides; Debris flows; Natural dams; Sediment dynamics; Confluence angle; Cascading effects (search for similar items in EconPapers)
Date: 2025
References: Add references at CitEc
Citations:

Downloads: (external link)
http://link.springer.com/10.1007/s11069-025-07402-0 Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:spr:nathaz:v:121:y:2025:i:13:d:10.1007_s11069-025-07402-0

Ordering information: This journal article can be ordered from
http://www.springer.com/economics/journal/11069

DOI: 10.1007/s11069-025-07402-0

Access Statistics for this article

Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards is currently edited by Thomas Glade, Tad S. Murty and Vladimír Schenk

More articles in Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards from Springer, International Society for the Prevention and Mitigation of Natural Hazards
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().

 
Page updated 2025-08-01
Handle: RePEc:spr:nathaz:v:121:y:2025:i:13:d:10.1007_s11069-025-07402-0