Earth Surface Dynamics
Earth Surface Dynamics
ESurf
Articles | Volume 11, issue 5
Articles | Volume 11, issue 5
https://doi.org/10.5194/esurf-11-995-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-11-995-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 11, issue 5
Research article
 | 
09 Oct 2023
Research article |  | 09 Oct 2023

Building a bimodal landscape: bedrock lithology and bed thickness controls on the morphology of Last Chance Canyon, New Mexico, USA

Sam Anderson, Nicole Gasparini, and Joel Johnson

Viewed

Total article views: 1,510 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,167 288 55 1,510 34 39
  • HTML: 1,167
  • PDF: 288
  • XML: 55
  • Total: 1,510
  • BibTeX: 34
  • EndNote: 39
Views and downloads (calculated since 05 Dec 2022)
Cumulative views and downloads (calculated since 05 Dec 2022)

Viewed (geographical distribution)

Total article views: 1,510 (including HTML, PDF, and XML) Thereof 1,459 with geography defined and 51 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 20 Nov 2024
Download
Short summary
We measured rock strength and amount of fracturing in the two different rock types, sandstones and carbonates, in Last Chance Canyon, New Mexico, USA. Where there is more carbonate bedrock, hills and channels steepen in Last Chance Canyon. This is because the carbonate-type bedrock tends to be more thickly bedded, is less fractured, and is stronger. The carbonate bedrock produces larger boulders than the sandstone bedrock, which can protect the more fractured sandstone bedrock from erosion.
Read more