Articles | Volume 13, issue 1
https://doi.org/10.5194/esurf-13-41-2025
https://doi.org/10.5194/esurf-13-41-2025
Research article
 | 
16 Jan 2025
Research article |  | 16 Jan 2025

Massive permafrost rock slide under a warming polythermal glacier deciphered through mechanical modeling (Bliggspitze, Austria)

Felix Pfluger, Samuel Weber, Joseph Steinhauser, Christian Zangerl, Christine Fey, Johannes Fürst, and Michael Krautblatter

Viewed

Total article views: 8,368 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
4,521 1,984 1,863 8,368 355 125 211
  • HTML: 4,521
  • PDF: 1,984
  • XML: 1,863
  • Total: 8,368
  • Supplement: 355
  • BibTeX: 125
  • EndNote: 211
Views and downloads (calculated since 22 Aug 2024)
Cumulative views and downloads (calculated since 22 Aug 2024)

Viewed (geographical distribution)

Total article views: 8,368 (including HTML, PDF, and XML) Thereof 8,302 with geography defined and 66 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 13 Jun 2026
Download
Short summary
Our study explores permafrost–glacier interactions with a focus on their implications for preparing or triggering high-volume rock slope failures. Using the Bliggspitze rock slide as a case study, we demonstrate a new type of rock slope failure mechanism triggered by the uplift of the cold–warm dividing line in polythermal alpine glaciers, a widespread and currently under-explored phenomenon in alpine environments worldwide.
Share