Articles | Volume 20, issue 4
https://doi.org/10.5194/cp-20-891-2024
https://doi.org/10.5194/cp-20-891-2024
Research article
 | 
10 Apr 2024
Research article |  | 10 Apr 2024

Spatial variability of marine-terminating ice sheet retreat in the Puget Lowland

Marion A. McKenzie, Lauren E. Miller, Allison P. Lepp, and Regina DeWitt

Viewed

Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.

Total article views: 712 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
603 82 27 712 27 19 24
  • HTML: 603
  • PDF: 82
  • XML: 27
  • Total: 712
  • Supplement: 27
  • BibTeX: 19
  • EndNote: 24
Views and downloads (calculated since 17 Nov 2023)
Cumulative views and downloads (calculated since 17 Nov 2023)

Viewed (geographical distribution)

Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.

Total article views: 712 (including HTML, PDF, and XML) Thereof 693 with geography defined and 19 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 17 Jul 2024
Download
Short summary
Records of the interaction between land and glacial ice movement in the Puget Lowland of Washington State are used to interpret that solid Earth movement provided stability to this marine-terminating glacial ice for at least 500 years. These results are significant because this landscape is similar to parts of the Greenland Ice Sheet and the Antarctic Peninsula, indicating that the interactions seen in this area are applicable to modern glaciated regions.