The Cryosphere
The Cryosphere
TC
Articles | Volume 19, issue 10
Articles | Volume 19, issue 10
https://doi.org/10.5194/tc-19-5095-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-19-5095-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 10
Research article
 | 
27 Oct 2025
Research article |  | 27 Oct 2025

Folding due to anisotropy in ice, from drill-core-scale cloudy bands to km-scale internal reflection horizons

Paul D. Bons, Yuanbang Hu, M.-Gema Llorens, Steven Franke, Nicolas Stoll, Ilka Weikusat, Julien Westhoff, and Yu Zhang

Viewed

Total article views: 2,727 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,768 842 117 2,727 148 97 112
  • HTML: 1,768
  • PDF: 842
  • XML: 117
  • Total: 2,727
  • Supplement: 148
  • BibTeX: 97
  • EndNote: 112
Views and downloads (calculated since 27 Jan 2025)
Cumulative views and downloads (calculated since 27 Jan 2025)

Viewed (geographical distribution)

Total article views: 2,727 (including HTML, PDF, and XML) Thereof 2,686 with geography defined and 41 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 03 May 2026
Download
Short summary
What causes folds in ice layers from the km scale down to the scale visible in the drill core: buckle folding due to variations in viscosity between layers, or the effect of mechanical anisotropy of ice due to an alignment of the crystal-lattice planes? Power spectra of folds in ice, a biotite schist, and numerical simulations show that folding in ice is due to the anisotropy, as the folds are self-similar, meaning that there is no characteristic fold scale that would result from buckle folding.
Read more
Share