Articles | Volume 5, issue 2
Research article
08 May 2017
Research article |  | 08 May 2017

Self-similar growth of a bimodal laboratory fan

Pauline Delorme, Vaughan Voller, Chris Paola, Olivier Devauchelle, Éric Lajeunesse, Laurie Barrier, and François Métivier


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Pauline Delorme on behalf of the Authors (20 Mar 2017)  Author's response   Manuscript 
ED: Publish as is (07 Apr 2017) by Patricia Wiberg
ED: Publish as is (11 Apr 2017) by Niels Hovius (Editor)
AR by Pauline Delorme on behalf of the Authors (13 Apr 2017)  Author's response   Manuscript 
Short summary
Alluvial fans are sedimentary deposits that take place at the outlet of mountain range. This location makes them the first sedimentary archive where sediments, eroded from mountains, are deposed. Their morphology is controlled by the water and sediment discharges and sediment characteristics. By using controlled laboratory experiments, we show that an alluvial fan composed of two distinct sediments has a characteristic shape; it can be decomposed into two fans made up of one sediment.