Articles | Volume 6, issue 2
https://doi.org/10.5194/esurf-6-505-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-6-505-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
How concave are river channels?
School of GeoSciences, University of Edinburgh, Drummond Street, Edinburgh EH8 9XP, UK
Fiona J. Clubb
Institute of Earth and Environmental Science, University of Potsdam, 14476 Potsdam, Germany
Boris Gailleton
School of GeoSciences, University of Edinburgh, Drummond Street, Edinburgh EH8 9XP, UK
Martin D. Hurst
School of Geographical and Earth Sciences, University of Glasgow, University Avenue, Glasgow G12 8QQ, UK
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- Lithological and structural controls on river profiles and networks in the northern Sierra Nevada (California, USA) E. Gabet 10.1130/B35128.1
- Morphotectonics of the northern Bogd fault and implications for Middle Pleistocene to modern uplift rates in southern Mongolia J. van der Wal et al. 10.1016/j.geomorph.2020.107330
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- Tracking Downstream Variability in Large Grain‐Size Distributions in the South‐Central Andes B. Purinton & B. Bookhagen 10.1029/2021JF006260
1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
Rivers can reveal information about erosion rates, tectonics, and climate. In order to make meaningful inferences about these influences, one must be able to compare headwaters to downstream parts of the river network. We describe new methods for normalizing river steepness for drainage area to better understand how rivers record erosion rates in eroding landscapes.
Rivers can reveal information about erosion rates, tectonics, and climate. In order to make...