Articles | Volume 4, issue 1
Research article
10 Mar 2016
Research article |  | 10 Mar 2016

Modelling sediment clasts transport during landscape evolution

Sébastien Carretier, Pierre Martinod, Martin Reich, and Yves Godderis

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Cited articles

Anderson, R., Anderson, S., and Tucker, G.: Rock damage and regolith transport by frost: an example of climate modulation of the geomorphology of the critical zone, Earth Surf. Proc. Land., 38, 299–316,, 2013.
Anderson, R. S.: Particle trajectories on hillslopes: Implications for particle age and Be-10 structure, J. Geophys. Res.-Earth, 120, 1626–1644,, 2015.
Anderson, S., Anderson, R., and Tucker, G.: Landscape scale linkages in critical zone evolution, C. R. Geosci., 344, 586–596, 2012.
Andreotti, B., Claudin, P., and Pouliquen, O.: Measurements of the aeolian sand transport saturation length, Geomorphology, 123, 343–348,, 2010.
Andrews, D. J. and Hanks, T. C.: Scarp degraded by linear diffusion: Inverse solution for age, J. Geophys. Res., 90, 10193–10208, 1985.
Short summary
We introduce moving clasts (grains, minerals, cobbles) in a landscape evolution model. This coupling has many potential applications, such as sediment provenance or the tracing of weathered material. It fills a gap between long-term landscape dynamics, which are difficult to tackle, and sediment clast populations studied in the field.