Articles | Volume 5, issue 1
https://doi.org/10.5194/esurf-5-85-2017
© Author(s) 2017. 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-5-85-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 Jan 2017
Research article |
| 30 Jan 2017
Steady state, erosional continuity, and the topography of landscapes developed in layered rocks
Matija Perne
Department of Geosciences, University of Arkansas, Fayetteville, Arkansas, USA
Jožef Stefan Institute, Ljubljana, Slovenia
Department of Geosciences, University of Arkansas, Fayetteville, Arkansas, USA
Evan A. Thaler
Department of Geosciences, University of Arkansas, Fayetteville, Arkansas, USA
Joseph M. Myre
Department of Geosciences, University of Arkansas, Fayetteville, Arkansas, USA
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- Uncovering the Controls on Fluvial Bedrock Erodibility and Knickpoint Expression: A High‐Resolution Comparison of Bedrock Properties Between Knickpoints and Non‐Knickpoint Reaches K. Chilton & J. Spotila 10.1029/2021JF006511
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42 citations as recorded by crossref.
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- Lateral bedrock erosion and valley formation in a heterogeneously layered landscape, Northeast Kansas A. Marcotte et al. 10.1002/esp.5172
- Migrating Transverse Escarpments in Strike Valleys on the Colorado Plateau C. Sheehan & D. Ward 10.1029/2019JF005260
- Preservation of Valley and Ridge topography via delivery of resistant, ridge-sourced boulders to hillslopes and channels, Southern Appalachian Mountains, U.S.A. K. Chilton & J. Spotila 10.1016/j.geomorph.2020.107263
- Spatially Variable Increase in Rock Uplift in the Northern U.S. Cordillera Recorded in the Distribution of River Knickpoints and Incision Depths N. Mitchell & B. Yanites 10.1029/2018JF004880
- Magnitude and timing of transient incision resulting from large‐scale drainage capture, Sutlej River, Northwest Himalaya B. Penserini et al. 10.1002/esp.5705
- Lithologic Effects on Landscape Response to Base Level Changes: A Modeling Study in the Context of the Eastern Jura Mountains, Switzerland B. Yanites et al. 10.1002/2016JF004101
- Isolating Lithologic Versus Tectonic Signals of River Profiles to Test Orogenic Models for the Eastern and Southeastern Carpathians B. Gailleton et al. 10.1029/2020JF005970
- Ongoing landscape transience in the eastern Amazon Craton consistent with lithologic control of base level C. Fadul et al. 10.1002/esp.5447
- The Erosional Signature of Drainage Divide Motion Along the Blue Ridge Escarpment M. Stokes et al. 10.1029/2022JF006757
- Rock strength and structural controls on fluvial erodibility: Implications for drainage divide mobility in a collisional mountain belt J. Zondervan et al. 10.1016/j.epsl.2020.116221
- Exhumation of the southern transpressive Bucaramanga fault, eastern Cordillera of Colombia: Insights from detrital, quantitative thermochronology and geomorphology M. Bermúdez et al. 10.1016/j.jsames.2020.103057
- Yardangs sculpted by erosion of heterogeneous material S. Boury et al. 10.1073/pnas.2322411121
- Dip, layer spacing, and incision rate controls on the formation of strike valleys, cuestas, and cliffbands in heterogeneous stratigraphy D. Ward 10.1130/L1056.1
- Impacts of Spontaneous Waterfall Development on Bedrock River Longitudinal Profile Morphology S. Rothman et al. 10.1029/2022JF007057
- Uplift and exhumation events and thermochronological constraints at the end of Triassic in southwestern Ordos Basin W. JianQiang et al. 10.18654/1000-0569/2020.04.14
- Criteria and tools for determining drainage divide stability A. Forte & K. Whipple 10.1016/j.epsl.2018.04.026
- An Autogenic Cycle of Fluvial Transience in Dipping, Layered Rocks C. Sheehan & D. Ward 10.1029/2020GL090246
- Erosion of heterogeneous rock drives diversification of Appalachian fishes M. Stokes et al. 10.1126/science.add9791
- New constraints on bedrock erodibility and landscape response times upstream of an active fault J. Zondervan et al. 10.1016/j.geomorph.2019.106937
- Quantifying the competing influences of lithology and throw rate on bedrock river incision E. Kent et al. 10.1130/B35783.1
- Growing topography due to contrasting rock types in a tectonically dead landscape D. Peifer et al. 10.5194/esurf-9-167-2021
- Bedload‐Bedrock Contrasts Form Enigmatic Low‐Relief Surfaces of the Pyrenees M. Fox et al. 10.1029/2022GL101995
- Uplift and exhumation events and thermochronological constraints at the end of Triassic in southwestern Ordos Basin W. JianQiang et al. 10.18654/1000-0569/2020.04.14
- Bedrock river erosion through dipping layered rocks: quantifying erodibility through kinematic wave speed N. Mitchell & B. Yanites 10.5194/esurf-9-723-2021
- Geomorphic complexity and the case for topographic rejuvenation of the Appalachian Mountains J. Spotila & P. Prince 10.1016/j.geomorph.2022.108449
- Tectonic advection of contacts enhances landscape transience N. Mitchell & A. Forte 10.1002/esp.5559
- Geometric disequilibrium of river basins produces long-lived transient landscapes H. Beeson et al. 10.1016/j.epsl.2017.07.010
- Lithology: A Landlab submodule for spatially variable rock properties K. Barnhart et al. 10.21105/joss.00979
- Resistant rock layers amplify cosmogenically‐determined erosion rates A. Darling et al. 10.1002/esp.4730
- Building a bimodal landscape: bedrock lithology and bed thickness controls on the morphology of Last Chance Canyon, New Mexico, USA S. Anderson et al. 10.5194/esurf-11-995-2023
- Complex erosional response to uplift and rock strength contrasts in transient river systems crossing an active normal fault revealed by 10Be and 26Al cosmogenic nuclide analyses S. Boulton et al. 10.1002/esp.5778
- Quasi‐Steady Evolution of Hillslopes in Layered Landscapes: An Analytic Approach R. Glade & R. Anderson 10.1002/2017JF004466
- River profile evolution by plucking in lithologically heterogeneous landscapes: Uniform uplift vs. tilting E. Gabet 10.1002/esp.4832
- Response of transient rock uplift and base level knickpoints to erosional efficiency contrasts in bedrock streams J. Wolpert & A. Forte 10.1002/esp.5146
- The Dynamics of Channel Slope, Width, and Sediment in Actively Eroding Bedrock River Systems B. Yanites 10.1029/2017JF004405
- Uncovering the Controls on Fluvial Bedrock Erodibility and Knickpoint Expression: A High‐Resolution Comparison of Bedrock Properties Between Knickpoints and Non‐Knickpoint Reaches K. Chilton & J. Spotila 10.1029/2021JF006511
- Himalayan valley-floor widths controlled by tectonically driven exhumation F. Clubb et al. 10.1038/s41561-023-01238-8
- Stratigraphic control of landscape response to base-level fall, Young Womans Creek, Pennsylvania, USA R. DiBiase et al. 10.1016/j.epsl.2018.10.005
- Estimating the disequilibrium in denudation rates due to divide migration at the scale of river basins T. Sassolas-Serrayet et al. 10.5194/esurf-7-1041-2019
- River system reformed by the Eastern Kunlun Fault: Implications from geomorphological features in the Eastern Kunlun Mountains, Northern Tibetan Plateau X. Yu et al. 10.1016/j.geomorph.2019.106876
- Amphitheatre‐headed canyons of Southern Utah: Stratigraphic control of canyon morphology A. Ryan & K. Whipple 10.1002/esp.4987
Latest update: 20 Nov 2024
Short summary
Concepts of landscape equilibrium often enable the interpretation of landscape response to various forces. However, we demonstrate that standard conceptions of landscape equilibrium do not apply in layered rocks. We develop a more general mathematical description of steady state based on a constraint of land surface continuity. In the case of rock layers that are nearly horizontal, this continuity steady state makes substantially different predictions about the nature of equilibrium landscapes.
Concepts of landscape equilibrium often enable the interpretation of landscape response to...
