05 Dec 2022
05 Dec 2022
Status: this preprint is open for discussion.

Building a Bimodal Landscape with Varying Bed Thicknesses in Last Chance Canyon, New Mexico

Samuel Anderson1, Nicole Gasparini1, and Joel Johnson2 Samuel Anderson et al.
  • 1Earth and Environmental Science, Tulane University, New Orleans, 70118, USA
  • 2Jackson School of Geosciences, University of Texas at Austin, Austin, 78712, USA

Abstract. We explore how rock properties and channel morphology vary with rock type in Last Chance canyon, Guadalupe mountains, New Mexico, USA. The rocks here are composed of horizontally to near horizontally interbedded carbonate and sandstone. This study focuses on first and second order channel sections where the streams have a lower channel steepness index (ksn) upstream and transition to a higher ksn downstream. We hypothesize that differences in bed thickness and rock strength influence ksn values, both directly by influencing bulk bedrock strength but also indirectly through the production of coarse sediment. We collected discontinuity intensity data (the length of bedding planes and fractures per unit area), Schmidt hammer rebound measurements, and measured the largest boulder at every 40-foot elevation contour to test this hypothesis. Bedrock and boulder minerology was determined using a lab-based carbonate dissolution method. High resolution orthomosaics and DEMs were generated from drone photos. The orthomosaics were used to map channel sections with exposed bedrock. The high-resolution DEMs were used to measure channel slope and hillslope relief. We find that discontinuity intensity is negatively correlated with Schmidt hammer rebound values. Channel steepness is higher where reaches are primarily incising through more thickly bedded carbonate bedrock. Where there is more thinly bedded sandstone rock exposed, channel steepness tends to be lower. Furthermore, the effect that rock properties have on channel morphology is confounded by sediment input from hillslopes. Thickly bedded rock units on surrounding hillslopes contribute larger sized colluvial sediment to the channels, and these reaches have higher ksn. Larger and more competent carbonate sediment armors both the carbonate and the more erodible sandstone and dampens the negative effect sandstone bedrock has on channel steepness. We believe that in the relatively steep, high ksn downstream channel sections slope is primarily controlled by the coarse alluvial cover. We further posit that the upstream low ksn reaches have a baselevel that is essentially fixed by the steep downstream reaches, resulting in a stable configuration where channel slopes have adjusted to lithologic differences and/or sediment armor.

Samuel Anderson et al.

Status: open (extended)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-1285', Anonymous Referee #1, 24 Jan 2023 reply

Samuel Anderson et al.

Samuel Anderson et al.


Total article views: 174 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
127 39 8 174 2 2
  • HTML: 127
  • PDF: 39
  • XML: 8
  • Total: 174
  • BibTeX: 2
  • EndNote: 2
Views and downloads (calculated since 05 Dec 2022)
Cumulative views and downloads (calculated since 05 Dec 2022)

Viewed (geographical distribution)

Total article views: 176 (including HTML, PDF, and XML) Thereof 176 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
Latest update: 26 Jan 2023
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.