Articles | Volume 4, issue 1
https://doi.org/10.5194/esurf-4-147-2016
© Author(s) 2016. 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-4-147-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
02 Feb 2016
Research article |
| 02 Feb 2016
On the potential for regolith control of fluvial terrace formation in semi-arid escarpments
School of Geography, Environment and Earth Sciences, Victoria
University of Wellington, Wellington, New Zealand
F. Schlunegger
Institute of
Geological Sciences, University of Bern, Bern, Switzerland
C. Litty
Institute of
Geological Sciences, University of Bern, Bern, Switzerland
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Cited
15 citations as recorded by crossref.
- Fluvial activity in the Lomas de Lachay during the upper Pleistocene and Holocene T. Kalicki & P. Kalicki 10.1016/j.geomorph.2020.107087
- Late-Pleistocene catchment-wide denudation patterns across the European Alps R. Delunel et al. 10.1016/j.earscirev.2020.103407
- fluvial responses to external and internal forcing: Upper Holocene dynamics in a low latitude semi-arid region in South America K. Lima et al. 10.1016/j.jsames.2021.103545
- Chronology of alluvial terrace sediment accumulation and incision in the Pativilca Valley, western Peruvian Andes C. Litty et al. 10.1016/j.geomorph.2018.05.005
- A 121‐ka record of Western Andean fluvial response to suborbital climate cycles recorded by rhythmic grain size variations of the Lima fluvial fan W. Viveen et al. 10.1002/esp.5831
- Heinrich events and tectonic uplift as possible drivers for late Quaternary fluvial dynamics in the western Peruvian Andes W. Viveen et al. 10.1016/j.gloplacha.2022.103972
- Possible climatic controls on the accumulation of Peru's most prominent alluvial fan: The Lima Conglomerate C. Litty et al. 10.1002/esp.4548
- Stratigraphy and palaeoenvironmental interpretation of late Quaternary colluvial slope deposits in southern Africa J. Knight 10.25131/sajg.124.0031
- Climate changes and the formation of fluvial terraces in central Amazonia inferred from landscape evolution modeling A. do Prado et al. 10.5194/esurf-10-457-2022
- Alluvial channel response to environmental perturbations: fill-terrace formation and sediment-signal disruption S. Tofelde et al. 10.5194/esurf-7-609-2019
- Climate-controlled shifts in sediment provenance inferred from detrital zircon ages, western Peruvian Andes C. Litty et al. 10.1130/G38371.1
- Short communication: Field data reveal that the transport probability of clasts in Peruvian and Swiss streams mainly depends on the sorting of the grains F. Schlunegger et al. 10.5194/esurf-8-717-2020
- On the mechanisms resulting in the formation of the Quaternary staircase terrace systems in the valleys of the western Andean margin of Peru F. Schlunegger et al. 10.1016/j.geomorph.2023.108923
- Impact of climate on landscape form, sediment transfer and the sedimentary record R. Harries et al. 10.1002/esp.5075
- Fluvial archives, a valuable record of vertical crustal deformation A. Demoulin et al. 10.1016/j.quascirev.2016.11.011
14 citations as recorded by crossref.
- Fluvial activity in the Lomas de Lachay during the upper Pleistocene and Holocene T. Kalicki & P. Kalicki 10.1016/j.geomorph.2020.107087
- Late-Pleistocene catchment-wide denudation patterns across the European Alps R. Delunel et al. 10.1016/j.earscirev.2020.103407
- fluvial responses to external and internal forcing: Upper Holocene dynamics in a low latitude semi-arid region in South America K. Lima et al. 10.1016/j.jsames.2021.103545
- Chronology of alluvial terrace sediment accumulation and incision in the Pativilca Valley, western Peruvian Andes C. Litty et al. 10.1016/j.geomorph.2018.05.005
- A 121‐ka record of Western Andean fluvial response to suborbital climate cycles recorded by rhythmic grain size variations of the Lima fluvial fan W. Viveen et al. 10.1002/esp.5831
- Heinrich events and tectonic uplift as possible drivers for late Quaternary fluvial dynamics in the western Peruvian Andes W. Viveen et al. 10.1016/j.gloplacha.2022.103972
- Possible climatic controls on the accumulation of Peru's most prominent alluvial fan: The Lima Conglomerate C. Litty et al. 10.1002/esp.4548
- Stratigraphy and palaeoenvironmental interpretation of late Quaternary colluvial slope deposits in southern Africa J. Knight 10.25131/sajg.124.0031
- Climate changes and the formation of fluvial terraces in central Amazonia inferred from landscape evolution modeling A. do Prado et al. 10.5194/esurf-10-457-2022
- Alluvial channel response to environmental perturbations: fill-terrace formation and sediment-signal disruption S. Tofelde et al. 10.5194/esurf-7-609-2019
- Climate-controlled shifts in sediment provenance inferred from detrital zircon ages, western Peruvian Andes C. Litty et al. 10.1130/G38371.1
- Short communication: Field data reveal that the transport probability of clasts in Peruvian and Swiss streams mainly depends on the sorting of the grains F. Schlunegger et al. 10.5194/esurf-8-717-2020
- On the mechanisms resulting in the formation of the Quaternary staircase terrace systems in the valleys of the western Andean margin of Peru F. Schlunegger et al. 10.1016/j.geomorph.2023.108923
- Impact of climate on landscape form, sediment transfer and the sedimentary record R. Harries et al. 10.1002/esp.5075
1 citations as recorded by crossref.
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Discussed (final revised paper)
Latest update: 15 Jan 2025
Short summary
Cut-fill terraces are common landforms throughout the world. Their distribution both in space and time is not clear-cut, as they can arise from numerous processes. We apply a climate-dependent regolith production algorithm to determine potential sediment loads during climate shifts. When combined with transport capacity, our results suggest that the cut-fill terraces of western Peru can result from transient stripping of hillslope sediment but not steady-state hillslope erosion.
Cut-fill terraces are common landforms throughout the world. Their distribution both in space...
