Earth Surface Dynamics
Earth Surface Dynamics
ESurf
Articles | Volume 11, issue 6
Articles | Volume 11, issue 6
https://doi.org/10.5194/esurf-11-1251-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-11-1251-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 11, issue 6
Research article
 | Highlight paper
 | 
08 Dec 2023
Research article | Highlight paper |  | 08 Dec 2023

Alpine hillslope failure in the western US: insights from the Chaos Canyon landslide, Rocky Mountain National Park, USA

Matthew C. Morriss, Benjamin Lehmann, Benjamin Campforts, George Brencher, Brianna Rick, Leif S. Anderson, Alexander L. Handwerger, Irina Overeem, and Jeffrey Moore

Viewed

Total article views: 1,761 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,455 259 47 1,761 68 24 31
  • HTML: 1,455
  • PDF: 259
  • XML: 47
  • Total: 1,761
  • Supplement: 68
  • BibTeX: 24
  • EndNote: 31
Views and downloads (calculated since 05 May 2023)
Cumulative views and downloads (calculated since 05 May 2023)

Viewed (geographical distribution)

Total article views: 1,761 (including HTML, PDF, and XML) Thereof 1,722 with geography defined and 39 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 08 May 2024
Download
Editor
Multiple techniques are used to monitor the collapse of an Alpine landslide in the United States. It is shown that the landslide was moving rapidly pre-failure. Given that the frequency of extreme events is likely to increase with future climate change, additional monitoring of Alpine regions is essential to limit hazards from future Alpine mass movements.
Read more
Short summary
In this paper, we investigate the 28 June 2022 collapse of the Chaos Canyon landslide in Rocky Mountain National Park, Colorado, USA. We find that the landslide was moving prior to its collapse and took place at peak spring snowmelt; temperature modeling indicates the potential presence of permafrost.  We hypothesize that this landslide could be part of the broader landscape evolution changes to alpine terrain caused by a warming climate, leading to thawing alpine permafrost.
Read more