The Cryosphere
The Cryosphere
TC
Articles | Volume 14, issue 1
Articles | Volume 14, issue 1
https://doi.org/10.5194/tc-14-1-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-1-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 14, issue 1
Research article
 | 
02 Jan 2020
Research article |  | 02 Jan 2020

Rock glacier characteristics serve as an indirect record of multiple alpine glacier advances in Taylor Valley, Antarctica

Kelsey Winsor, Kate M. Swanger, Esther Babcock, Rachel D. Valletta, and James L. Dickson

Viewed

Total article views: 3,713 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,507 1,102 104 3,713 243 110 112
  • HTML: 2,507
  • PDF: 1,102
  • XML: 104
  • Total: 3,713
  • Supplement: 243
  • BibTeX: 110
  • EndNote: 112
Views and downloads (calculated since 18 Jun 2019)
Cumulative views and downloads (calculated since 18 Jun 2019)

Viewed (geographical distribution)

Total article views: 3,713 (including HTML, PDF, and XML) Thereof 3,124 with geography defined and 589 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 02 Jul 2025
Download
Short summary
We studied an ice-cored rock glacier in Taylor Valley, Antarctica, coupling ground-penetrating radar analyses with stable isotope and major ion geochemistry of (a) surface ponds and (b) buried clean ice. These analyses indicate that the rock glacier ice is fed by a nearby alpine glacier, recording multiple Holocene to late Pleistocene glacial advances. We demonstrate the potential to use rock glaciers and buried ice, common throughout Antarctica, to map previous glacial extents.
Read more
Share