Articles | Volume 18, issue 5
https://doi.org/10.5194/tc-18-2277-2024
https://doi.org/10.5194/tc-18-2277-2024
Research article
 | 
07 May 2024
Research article |  | 07 May 2024

Extensive palaeo-surfaces beneath the Evans–Rutford region of the West Antarctic Ice Sheet control modern and past ice flow

Charlotte M. Carter, Michael J. Bentley, Stewart S. R. Jamieson, Guy J. G. Paxman, Tom A. Jordan, Julien A. Bodart, Neil Ross, and Felipe Napoleoni

Viewed

Total article views: 1,265 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
944 267 54 1,265 39 39
  • HTML: 944
  • PDF: 267
  • XML: 54
  • Total: 1,265
  • BibTeX: 39
  • EndNote: 39
Views and downloads (calculated since 02 Nov 2023)
Cumulative views and downloads (calculated since 02 Nov 2023)

Viewed (geographical distribution)

Total article views: 1,265 (including HTML, PDF, and XML) Thereof 1,221 with geography defined and 44 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
We use radio-echo sounding data to investigate the presence of flat surfaces beneath the Evans–Rutford region in West Antarctica. These surfaces may be what remains of laterally continuous surfaces, formed before the inception of the West Antarctic Ice Sheet, and we assess two hypotheses for their formation. Tectonic structures in the region may have also had a control on the growth of the ice sheet by focusing ice flow into troughs adjoining these surfaces.