Articles | Volume 6, issue 3
https://doi.org/10.5194/esurf-6-743-2018
https://doi.org/10.5194/esurf-6-743-2018
Research article
 | Highlight paper
 | 
04 Sep 2018
Research article | Highlight paper |  | 04 Sep 2018

Clast imbrication in coarse-grained mountain streams and stratigraphic archives as indicator of deposition in upper flow regime conditions

Fritz Schlunegger and Philippos Garefalakis

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
AR by Fritz Schlunegger on behalf of the Authors (01 Aug 2018)  Author's response   Manuscript 
ED: Publish as is (12 Aug 2018) by Sebastien Castelltort
ED: Publish subject to technical corrections (13 Aug 2018) by Niels Hovius (Editor)
AR by Fritz Schlunegger on behalf of the Authors (22 Aug 2018)  Author's response   Manuscript 
Download
Short summary
Clast imbrication, which is a depositional fabric where clasts overlap each other similar to a run of toppled dominoes, is one of the most conspicuous sedimentary structures in coarse-grained fluvial deposits. However, the conditions leading to this fabric have been contested. Here, we calculate the hydrological conditions for various stream gradients. We find that clast imbrication most likely forms where channel gradients exceed a threshold and where upper flow regime conditions prevail.