Articles | Volume 5, issue 2
https://doi.org/10.5194/esurf-5-239-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-5-239-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
08 May 2017
Research article |
| 08 May 2017
Self-similar growth of a bimodal laboratory fan
Pauline Delorme
CORRESPONDING AUTHOR
Institut de Physique du Globe de Paris, Paris – Sorbonne Paris Cité, Université Paris Diderot, Paris, France
Vaughan Voller
Saint Anthony Falls Laboratory, University of Minnesota, Minneapolis, Minnesota, USA
Chris Paola
Saint Anthony Falls Laboratory, University of Minnesota, Minneapolis, Minnesota, USA
Olivier Devauchelle
Institut de Physique du Globe de Paris, Paris – Sorbonne Paris Cité, Université Paris Diderot, Paris, France
Éric Lajeunesse
Institut de Physique du Globe de Paris, Paris – Sorbonne Paris Cité, Université Paris Diderot, Paris, France
Laurie Barrier
Institut de Physique du Globe de Paris, Paris – Sorbonne Paris Cité, Université Paris Diderot, Paris, France
François Métivier
Institut de Physique du Globe de Paris, Paris – Sorbonne Paris Cité, Université Paris Diderot, Paris, France
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Cited
16 citations as recorded by crossref.
- Interaction between driftwood deposition patterns and debris flow fan development Y. Chiu et al. 10.1007/s10346-023-02116-5
- Fossilized autogenic responses of grain‐size transition to sediment supply and water discharge: Alluvial fan experiments H. Shin et al. 10.1111/sed.13173
- Growth and shape of a laboratory alluvial fan P. Delorme et al. 10.1103/PhysRevE.98.012907
- The thin blue line: A review of shoreline dynamics across time scales and environments V. Voller et al. 10.1002/esp.4705
- Episodic sediment supply to alluvial fans: implications for fan incision and morphometry A. Leenman & B. Eaton 10.5194/esurf-10-1097-2022
- Experimental evidence for bifurcation angles control on abandoned channel fill geometry L. Szewczyk et al. 10.5194/esurf-8-275-2020
- Coupling threshold theory and satellite-derived channel width to estimate the formative discharge of Himalayan foreland rivers K. Gaurav et al. 10.5194/esurf-9-47-2021
- Floods on Alluvial Fans: Implications for Reworking Rates, Morphology and Fan Hazards A. Leenman et al. 10.1029/2021JF006367
- Remote sensing of laboratory rivers A. Leenman & B. Eaton 10.1002/esp.5577
- Mechanisms for avulsion on alluvial fans: Insights from high‐frequency topographic data A. Leenman & B. Eaton 10.1002/esp.5059
- Temporal evolution of backward erosion piping in small-scale experiments J. Pol et al. 10.1007/s11440-022-01545-1
- Quaternary alluvial fan dynamics of the Jaldhaka basin A. Raha & M. Biswas 10.1007/s11629-021-7005-y
- Stabilising large grains in self-forming steep channels W. Booker & B. Eaton 10.5194/esurf-8-51-2020
- Application of a plate model to reproduce surface deformations observed at Uturuncu volcano, Bolivia A. Morand et al. 10.1016/j.jvolgeores.2021.107241
- A New Efficient Method to Solve the Stream Power Law Model Taking Into Account Sediment Deposition X. Yuan et al. 10.1029/2018JF004867
- The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan W. Feng et al. 10.1007/s12517-019-4468-z
16 citations as recorded by crossref.
- Interaction between driftwood deposition patterns and debris flow fan development Y. Chiu et al. 10.1007/s10346-023-02116-5
- Fossilized autogenic responses of grain‐size transition to sediment supply and water discharge: Alluvial fan experiments H. Shin et al. 10.1111/sed.13173
- Growth and shape of a laboratory alluvial fan P. Delorme et al. 10.1103/PhysRevE.98.012907
- The thin blue line: A review of shoreline dynamics across time scales and environments V. Voller et al. 10.1002/esp.4705
- Episodic sediment supply to alluvial fans: implications for fan incision and morphometry A. Leenman & B. Eaton 10.5194/esurf-10-1097-2022
- Experimental evidence for bifurcation angles control on abandoned channel fill geometry L. Szewczyk et al. 10.5194/esurf-8-275-2020
- Coupling threshold theory and satellite-derived channel width to estimate the formative discharge of Himalayan foreland rivers K. Gaurav et al. 10.5194/esurf-9-47-2021
- Floods on Alluvial Fans: Implications for Reworking Rates, Morphology and Fan Hazards A. Leenman et al. 10.1029/2021JF006367
- Remote sensing of laboratory rivers A. Leenman & B. Eaton 10.1002/esp.5577
- Mechanisms for avulsion on alluvial fans: Insights from high‐frequency topographic data A. Leenman & B. Eaton 10.1002/esp.5059
- Temporal evolution of backward erosion piping in small-scale experiments J. Pol et al. 10.1007/s11440-022-01545-1
- Quaternary alluvial fan dynamics of the Jaldhaka basin A. Raha & M. Biswas 10.1007/s11629-021-7005-y
- Stabilising large grains in self-forming steep channels W. Booker & B. Eaton 10.5194/esurf-8-51-2020
- Application of a plate model to reproduce surface deformations observed at Uturuncu volcano, Bolivia A. Morand et al. 10.1016/j.jvolgeores.2021.107241
- A New Efficient Method to Solve the Stream Power Law Model Taking Into Account Sediment Deposition X. Yuan et al. 10.1029/2018JF004867
- The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan W. Feng et al. 10.1007/s12517-019-4468-z
Latest update: 14 Dec 2024
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.
Alluvial fans are sedimentary deposits that take place at the outlet of mountain range. This...
