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Onset of sediment transport is a continuous transition driven by fluid shear and granular creep.A bottom-up control on fresh-bedrock topography under landscapes.Path selection in the growth of rivers.Global drainage patterns and the origins of topographic relief on Earth, Mars, and Titan.Ageing dynamics of ion bombardment induced self-organization processes.Dynamic reorganization of river basins.GEOMORPHOLOGY. Experimental evidence for hillslope control of landscape scale.GEOMORPHOLOGY. Landscapes in the lab.A lattice grain model of hillslope evolutionDeveloping, choosing and using landscape evolution models to inform field-based landscape reconstruction studiesOrogen-scale drainage network evolution and response to erodibility changes: insights from numerical experimentsThe influence of bedrock orientation on the landscape evolution, surface morphology and denudation (10Be) at the Niesen, SwitzerlandInfluence of mantle flow on the drainage of eastern Australia since the Jurassic PeriodControls on valley spacing in landscapes subject to rapid base-level fallThe root of branching river networks
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P2860
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в Nature в липні 2009
@uk
name
Formation of evenly spaced ridges and valleys
@en
Formation of evenly spaced ridges and valleys
@nl
type
label
Formation of evenly spaced ridges and valleys
@en
Formation of evenly spaced ridges and valleys
@nl
prefLabel
Formation of evenly spaced ridges and valleys
@en
Formation of evenly spaced ridges and valleys
@nl
P2093
P356
P1433
P1476
Formation of evenly spaced ridges and valleys
@en
P2093
J. Taylor Perron
James W. Kirchner
William E. Dietrich
P2888
P304
P356
10.1038/NATURE08174
P407
P577
2009-07-01T00:00:00Z
P6179
1037122098