Articles | Volume 15, issue 4
https://doi.org/10.5194/tc-15-2057-2021
https://doi.org/10.5194/tc-15-2057-2021
Research article
 | 
26 Apr 2021
Research article |  | 26 Apr 2021

Deciphering the evolution of the Bleis Marscha rock glacier (Val d'Err, eastern Switzerland) with cosmogenic nuclide exposure dating, aerial image correlation, and finite element modeling

Dominik Amschwand, Susan Ivy-Ochs, Marcel Frehner, Olivia Steinemann, Marcus Christl, and Christof Vockenhuber

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (05 Dec 2020) by Andreas Vieli
AR by Dominik Amschwand on behalf of the Authors (21 Jan 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (03 Feb 2021) by Andreas Vieli
RR by Leif S. Anderson (23 Feb 2021)
ED: Publish subject to technical corrections (25 Feb 2021) by Andreas Vieli
AR by Dominik Amschwand on behalf of the Authors (10 Mar 2021)  Author's response    Manuscript
Download
Short summary
We reconstruct the Holocene history of the Bleis Marscha rock glacier (eastern Swiss Alps) by determining the surface residence time of boulders via their exposure to cosmic rays. We find that this stack of lobes formed in three phases over the last ~9000 years, controlled by the regional climate. This work adds to our understanding of how these permafrost landforms reacted in the past to climate oscillations and helps to put the current behavior of rock glaciers in a long-term perspective.