Articles | Volume 7, issue 3
https://doi.org/10.5194/esurf-7-879-2019
© 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-7-879-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Sep 2019
Research article |
| 20 Sep 2019
| 20 Sep 2019
River channel width controls blocking by slow-moving landslides in California's Franciscan mélange
Department of Earth and Planetary Sciences, UC Santa Cruz, Santa Cruz, CA 95064, USA
Kiara N. Broudy
Department of Earth and Planetary Sciences, UC Santa Cruz, Santa Cruz, CA 95064, USA
Alexander L. Nereson
Department of Earth and Planetary Sciences, UC Santa Cruz, Santa Cruz, CA 95064, USA
Joshua J. Roering
Department of Earth Sciences, University of Oregon, Eugene, OR
97403, USA
Alexander L. Handwerger
Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA 91109, USA
Georgina Bennett
School of Environmental Sciences, University of East Anglia, Norwich, Norfolk, NR4 7TJ, UK
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Cited
16 citations as recorded by crossref.
- Unsaturated Flow Processes and the Onset of Seasonal Deformation in Slow‐Moving Landslides N. Finnegan et al. 10.1029/2020JF005758
- Frictional Control on Accelerating Creep During the Slow‐To‐Fast Transition of Rainfall‐Induced Catastrophic Landslides K. Paul et al. 10.1029/2023JF007213
- How big is a boulder? The importance of boulder definition choice in earth science research and river management R. Mason & L. Polvi 10.1002/esp.5861
- Boulders as a lithologic control on river and landscape response to tectonic forcing at the Mendocino triple junction C. Shobe et al. 10.1130/B35385.1
- Influence of Rarely Mobile Boulders on Channel Width and Slope: Theory and Field Application R. Nativ et al. 10.1029/2021JF006537
- Disproportionate and chronic sediment delivery from a fluvially controlled, deep‐seated landslide in Aotearoa New Zealand S. McColl et al. 10.1002/esp.5358
- The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards C. Shobe et al. 10.1016/j.earscirev.2021.103717
- Scale dependent spatial structuring of mountain river large bed elements maximizes flow resistance J. Wiener & G. Pasternack 10.1016/j.geomorph.2022.108431
- A new type of sliding zone soil and its severe effect on the formation of giant landslides in the Jinsha River tectonic suture zone, China S. Ren et al. 10.1007/s11069-023-05931-0
- The influence of coarse particle abundance and spatial distribution on sediment transport and cluster evolution in steep channels under sediment-starved conditions W. Li et al. 10.1016/j.catena.2023.107199
- The Preservation of Climate‐Driven Landslide Dams in Western Oregon W. Struble et al. 10.1029/2020JF005908
- Multi-period formation and possible high-position hazards of Chada gully deposits on the eastern margin of Tibetan Plateau Y. Zhang et al. 10.1016/j.enggeo.2022.106712
- Life and death of slow-moving landslides P. Lacroix et al. 10.1038/s43017-020-0072-8
- Landslide Sensitivity and Response to Precipitation Changes in Wet and Dry Climates A. Handwerger et al. 10.1029/2022GL099499
- Boulders modulate hillslope-channel coupling in the northern Alaska Range A. Bender & R. Lease 10.1130/G52086.1
- Seismic cycles, earthquakes, landslides and sediment fluxes: Linking tectonics to surface processes using a reduced-complexity model T. Croissant et al. 10.1016/j.geomorph.2019.04.017
15 citations as recorded by crossref.
- Unsaturated Flow Processes and the Onset of Seasonal Deformation in Slow‐Moving Landslides N. Finnegan et al. 10.1029/2020JF005758
- Frictional Control on Accelerating Creep During the Slow‐To‐Fast Transition of Rainfall‐Induced Catastrophic Landslides K. Paul et al. 10.1029/2023JF007213
- How big is a boulder? The importance of boulder definition choice in earth science research and river management R. Mason & L. Polvi 10.1002/esp.5861
- Boulders as a lithologic control on river and landscape response to tectonic forcing at the Mendocino triple junction C. Shobe et al. 10.1130/B35385.1
- Influence of Rarely Mobile Boulders on Channel Width and Slope: Theory and Field Application R. Nativ et al. 10.1029/2021JF006537
- Disproportionate and chronic sediment delivery from a fluvially controlled, deep‐seated landslide in Aotearoa New Zealand S. McColl et al. 10.1002/esp.5358
- The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards C. Shobe et al. 10.1016/j.earscirev.2021.103717
- Scale dependent spatial structuring of mountain river large bed elements maximizes flow resistance J. Wiener & G. Pasternack 10.1016/j.geomorph.2022.108431
- A new type of sliding zone soil and its severe effect on the formation of giant landslides in the Jinsha River tectonic suture zone, China S. Ren et al. 10.1007/s11069-023-05931-0
- The influence of coarse particle abundance and spatial distribution on sediment transport and cluster evolution in steep channels under sediment-starved conditions W. Li et al. 10.1016/j.catena.2023.107199
- The Preservation of Climate‐Driven Landslide Dams in Western Oregon W. Struble et al. 10.1029/2020JF005908
- Multi-period formation and possible high-position hazards of Chada gully deposits on the eastern margin of Tibetan Plateau Y. Zhang et al. 10.1016/j.enggeo.2022.106712
- Life and death of slow-moving landslides P. Lacroix et al. 10.1038/s43017-020-0072-8
- Landslide Sensitivity and Response to Precipitation Changes in Wet and Dry Climates A. Handwerger et al. 10.1029/2022GL099499
- Boulders modulate hillslope-channel coupling in the northern Alaska Range A. Bender & R. Lease 10.1130/G52086.1
Latest update: 22 Nov 2024
Short summary
In some settings, landslides trigger valley blockages that impound huge volumes of sediment, often drastically changing river habitat and habitability. In other settings, landslides appear to have little effect on rivers. In this study, we explore what governs the different sensitivity of rivers to blocking from landslide debris. We accomplish this by comparing two sites in California with dramatic differences in blocking from otherwise similar slow-moving landslides.
In some settings, landslides trigger valley blockages that impound huge volumes of sediment,...
