Articles | Volume 7, issue 3
https://doi.org/10.5194/esurf-7-755-2019
© Author(s) 2019. 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-7-755-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
26 Aug 2019
Research article |
| 26 Aug 2019
| 26 Aug 2019
Inferring the timing of abandonment of aggraded alluvial surfaces dated with cosmogenic nuclides
Mitch K. D'Arcy
CORRESPONDING AUTHOR
Institute of Geosciences, University of Potsdam,
Karl-Liebknecht-Strasse 24/25, 14476 Potsdam, Germany
GFZ German Research Centre for Geosciences, Telegrafenberg, 14473
Potsdam, Germany
Taylor F. Schildgen
GFZ German Research Centre for Geosciences, Telegrafenberg, 14473
Potsdam, Germany
Institute of Geosciences, University of Potsdam,
Karl-Liebknecht-Strasse 24/25, 14476 Potsdam, Germany
Jens M. Turowski
GFZ German Research Centre for Geosciences, Telegrafenberg, 14473
Potsdam, Germany
Pedro DiNezio
Institute for Geophysics, Jackson School of Geosciences, University of
Texas at Austin, J.J. Pickle Research Campus, Building 196 10100 Burnet Road
(R2200), Austin, TX 78758, USA
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Cited
15 citations as recorded by crossref.
- Holocene Depositional History Inferred From Single‐Grain Luminescence Ages in Southern California, North America S. Saha et al. 10.1029/2021GL092774
- Weathering under coastal hyperaridity – Late Quaternary development of spectral, textural, and gravelometric alluvial fan surface characteristics J. Walk et al. 10.1016/j.quascirev.2021.107339
- A tool for the ages: The Probabilistic Cosmogenic Age Analysis Tool (P-CAAT) J. Dortch et al. 10.1016/j.quageo.2022.101323
- The Transport History of Alluvial Fan Sediment Inferred From Multiple Geochronometers B. Goehring et al. 10.1029/2021JF006096
- Geomorphological Evidence of Active Faulting in Low Seismicity Regions—Examples From the Valley of Gobi Lakes, Southern Mongolia J. van der Wal et al. 10.3389/feart.2020.589814
- Landscape response to tectonic deformation and cyclic climate change since ca. 800 ka in the southern central Andes E. Orr et al. 10.5194/esurf-12-1391-2024
- Time‐Invariant Late Quaternary Slip Rates Along the Agua Blanca Fault, Northern Baja California, Mexico P. Gold et al. 10.1029/2019TC005788
- Seismo‐Tectonic Model for the Southern Pre‐Rif Border (Northern Morocco): Insights From Morphochronology K. Agharroud et al. 10.1029/2020TC006633
- Geomorphic Dating of Across‐Fault Gully Incision Reveals Time‐Invariant Late Quaternary Slip‐Rates at the Eastern Termination of the Altyn Tagh Fault N. Wieler et al. 10.1029/2021GL096933
- Late Quaternary Intraplate Deformation Defined by the Las Chacras Fault Zone, West‐Central Argentina J. Rimando et al. 10.1029/2020TC006509
- Quaternary landscape evolution in the Western Argentine Precordillera constrained by 10Be cosmogenic dating V. Peri et al. 10.1016/j.geomorph.2021.107984
- Tectonic geomorphology and Quaternary fault slip rates in the Tsambagarav Massif, Mongolian Altai S. Ha et al. 10.1002/esp.5558
- Postglacial outsize fan formation in the Upper Rhone valley, Switzerland – gradual or catastrophic? A. Schoch‐Baumann et al. 10.1002/esp.5301
- Pedogenesis at the coastal arid-hyperarid transition deduced from a Late Quaternary chronosequence at Paposo, Atacama Desert J. Walk et al. 10.1016/j.catena.2023.107171
- New developments in onshore paleoseismic methods, and their impact on Quaternary tectonic studies J. McCalpin et al. 10.1016/j.quaint.2023.03.008
15 citations as recorded by crossref.
- Holocene Depositional History Inferred From Single‐Grain Luminescence Ages in Southern California, North America S. Saha et al. 10.1029/2021GL092774
- Weathering under coastal hyperaridity – Late Quaternary development of spectral, textural, and gravelometric alluvial fan surface characteristics J. Walk et al. 10.1016/j.quascirev.2021.107339
- A tool for the ages: The Probabilistic Cosmogenic Age Analysis Tool (P-CAAT) J. Dortch et al. 10.1016/j.quageo.2022.101323
- The Transport History of Alluvial Fan Sediment Inferred From Multiple Geochronometers B. Goehring et al. 10.1029/2021JF006096
- Geomorphological Evidence of Active Faulting in Low Seismicity Regions—Examples From the Valley of Gobi Lakes, Southern Mongolia J. van der Wal et al. 10.3389/feart.2020.589814
- Landscape response to tectonic deformation and cyclic climate change since ca. 800 ka in the southern central Andes E. Orr et al. 10.5194/esurf-12-1391-2024
- Time‐Invariant Late Quaternary Slip Rates Along the Agua Blanca Fault, Northern Baja California, Mexico P. Gold et al. 10.1029/2019TC005788
- Seismo‐Tectonic Model for the Southern Pre‐Rif Border (Northern Morocco): Insights From Morphochronology K. Agharroud et al. 10.1029/2020TC006633
- Geomorphic Dating of Across‐Fault Gully Incision Reveals Time‐Invariant Late Quaternary Slip‐Rates at the Eastern Termination of the Altyn Tagh Fault N. Wieler et al. 10.1029/2021GL096933
- Late Quaternary Intraplate Deformation Defined by the Las Chacras Fault Zone, West‐Central Argentina J. Rimando et al. 10.1029/2020TC006509
- Quaternary landscape evolution in the Western Argentine Precordillera constrained by 10Be cosmogenic dating V. Peri et al. 10.1016/j.geomorph.2021.107984
- Tectonic geomorphology and Quaternary fault slip rates in the Tsambagarav Massif, Mongolian Altai S. Ha et al. 10.1002/esp.5558
- Postglacial outsize fan formation in the Upper Rhone valley, Switzerland – gradual or catastrophic? A. Schoch‐Baumann et al. 10.1002/esp.5301
- Pedogenesis at the coastal arid-hyperarid transition deduced from a Late Quaternary chronosequence at Paposo, Atacama Desert J. Walk et al. 10.1016/j.catena.2023.107171
- New developments in onshore paleoseismic methods, and their impact on Quaternary tectonic studies J. McCalpin et al. 10.1016/j.quaint.2023.03.008
Latest update: 05 Jan 2025
Short summary
The age of formation of sedimentary deposits is often interpreted to record information about past environmental changes. Here, we show that the timing of abandonment of surfaces also provides valuable information. We derive a new set of equations that can be used to estimate when a sedimentary surface was abandoned based on what is known about its activity from surface dating. Estimates of abandonment age can benefit a variety of geomorphic analyses, which we illustrate with a case study.
The age of formation of sedimentary deposits is often interpreted to record information about...
