Articles | Volume 11, issue 3
https://doi.org/10.5194/tc-11-1265-2017
https://doi.org/10.5194/tc-11-1265-2017
Research article
 | 
30 May 2017
Research article |  | 30 May 2017

Cryostratigraphy, sedimentology, and the late Quaternary evolution of the Zackenberg River delta, northeast Greenland

Graham L. Gilbert, Stefanie Cable, Christine Thiel, Hanne H. Christiansen, and Bo Elberling

Viewed

Total article views: 3,932 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,971 1,685 276 3,932 137 207
  • HTML: 1,971
  • PDF: 1,685
  • XML: 276
  • Total: 3,932
  • BibTeX: 137
  • EndNote: 207
Views and downloads (calculated since 17 Jan 2017)
Cumulative views and downloads (calculated since 17 Jan 2017)

Viewed (geographical distribution)

Total article views: 3,932 (including HTML, PDF, and XML) Thereof 3,614 with geography defined and 318 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
We reconstruct the Holocene development of the Zackenberg River delta (northeast Greenland) using a combination of sedimentology, cryostratigraphy, and geochronology. We distinguish four major depositional environments and identify three cryofacies. We apply the principles of cryostratigraphy to infer the aggradational history of permafrost. This paper contains an archive of ground ice in epigenetic permafrost in northeast Greenland.