Articles | Volume 9, issue 4
https://doi.org/10.5194/esurf-9-795-2021
https://doi.org/10.5194/esurf-9-795-2021
Research article
 | 
29 Jul 2021
Research article |  | 29 Jul 2021

Tectonically and climatically driven mountain-hopping erosion in central Guatemala from detrital 10Be and river profile analysis

Gilles Brocard, Jane Kathrin Willenbring, Tristan Salles, Michael Cosca, Axel Guttiérez-Orrego, Noé Cacao Chiquín, Sergio Morán-Ical, and Christian Teyssier

Viewed

Total article views: 2,564 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,858 651 55 2,564 206 46 49
  • HTML: 1,858
  • PDF: 651
  • XML: 55
  • Total: 2,564
  • Supplement: 206
  • BibTeX: 46
  • EndNote: 49
Views and downloads (calculated since 09 Nov 2020)
Cumulative views and downloads (calculated since 09 Nov 2020)

Viewed (geographical distribution)

Total article views: 2,564 (including HTML, PDF, and XML) Thereof 2,256 with geography defined and 308 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Dec 2024
Download
Short summary
The rise of a mountain affects the circulation of water, both in the atmosphere and over the land surface, thereby affecting the erosion of the land surface. We document how the rise of a mountain in central Guatemala has affected the erosion of an older range nearby. The new range intercepts precipitation formerly delivered to the older range. River response to the uplift of the new range has decreased incision across the older one. Both have reduced hillslope erosion over the old range.