Articles | Volume 9, issue 2
https://doi.org/10.5194/esurf-9-167-2021
© Author(s) 2021. 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-9-167-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Mar 2021
Research article |
| 09 Mar 2021
| 09 Mar 2021
Growing topography due to contrasting rock types in a tectonically dead landscape
School of Geographical and Earth Sciences, University of Glasgow,
Glasgow, G12 8QQ, UK
CAPES Foundation, Ministry of Education of Brazil, Brasília, DF 70040-020, Brazil
Cristina Persano
School of Geographical and Earth Sciences, University of Glasgow,
Glasgow, G12 8QQ, UK
Martin D. Hurst
School of Geographical and Earth Sciences, University of Glasgow,
Glasgow, G12 8QQ, UK
Paul Bishop
School of Geographical and Earth Sciences, University of Glasgow,
Glasgow, G12 8QQ, UK
Derek Fabel
Scottish Universities Environmental Research Centre, East Kilbride,
G75 0QF, UK
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- 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
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- Constraints on what controls millennial-scale basin-wide denudation across mountain belts, Asia Y. Yang et al. 10.1007/s11430-024-1420-8
- Interactions between tectonics, bedrock inheritance and geomorphic responses of rivers in a post-rifting upland (Ponta Grossa Arch region, Brazil) M. Santos et al. 10.1590/2317-4889202220210002
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25 citations as recorded by crossref.
- Episodic kilometre-scale burial and exhumation and the importance of missing section P. Green et al. 10.1016/j.earscirev.2022.104226
- Eroding the Himalaya: Topographic and Climatic Control of Erosion Rates and Implications for Tectonics K. Whipple et al. 10.1086/731260
- Post-Miocene topographic rejuvenation in an elevated passive continental margin not characterized by a sharp escarpment (northern end of the Mantiqueira Range, Brazil) S. Calegari et al. 10.1016/j.geomorph.2021.107946
- Impact of tectonic topographic rejuvenation in landscapes with high bedrock/duricrust strength: Insights from geomorphic evidence in a post-rifted region (SE Brazil) D. Campos et al. 10.1016/j.geomorph.2023.108749
- Post-rift geomorphological evolution of a passive continental margin (Paraíba region, northeastern Brazil): Insights from river profile and drainage divide analysis F. Alves et al. 10.1016/j.geomorph.2022.108384
- The southeast Brazilian rifted continental margin is not a single, continuous upwarp: Variations in morphology and denudation patterns along the continental drainage divide T. Fonte-Boa et al. 10.1016/j.earscirev.2022.104091
- Lithological control on topographic relief evolution in a slow tectonic setting (Anti-Atlas, Morocco) R. Clementucci et al. 10.1016/j.epsl.2022.117788
- Transient response to changes in uplift rates in the northern Atlas-Meseta system (Morocco) R. Clementucci et al. 10.1016/j.geomorph.2023.108765
- Geomorphic complexity and the case for topographic rejuvenation of the Appalachian Mountains J. Spotila & P. Prince 10.1016/j.geomorph.2022.108449
- Identificação dos leques aluviais dissecados do Quadrilátero Ferrífero (MG) através de critérios espaciais e sedimentológicos F. Lopes et al. 10.26848/rbgf.v14.3.p1296-1311
- Erosional Response to Pleistocene Climate Changes in the Brazilian Highlands V. Godard et al. 10.1029/2024JF007671
- Transient and relict landforms in a lithologically heterogeneous post-orogenic landscape in the intertropical belt (Alto Paranaíba region, Brazil) K. Marques et al. 10.1016/j.geomorph.2021.107892
- Cosmogenic (un-)steadiness revealed by paired-nuclide catchment-wide denudation rates in the formerly half-glaciated Vosges Mountains (NE France) T. Jautzy et al. 10.1016/j.epsl.2023.118490
- 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
- Stream laws in analog tectonic-landscape models R. Reitano et al. 10.5194/esurf-11-731-2023
- Pedogenic processes in a chronosequence of very deeply weathered soils in southeastern Brazil S. Rezende et al. 10.1016/j.catena.2022.106362
- Tectonic advection of contacts enhances landscape transience N. Mitchell & A. Forte 10.1002/esp.5559
- Yardangs sculpted by erosion of heterogeneous material S. Boury et al. 10.1073/pnas.2322411121
- Impact of Changing Concavity Indices on Channel Steepness and Divide Migration Metrics B. Gailleton et al. 10.1029/2020JF006060
- The Erosional Signature of Drainage Divide Motion Along the Blue Ridge Escarpment M. Stokes et al. 10.1029/2022JF006757
- 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
- Paul Bishop: recalling an academic life C. Philo & J. Briggs 10.1080/14702541.2023.2273562
- Constraints on what controls millennial-scale basin-wide denudation across mountain belts, Asia Y. Yang et al. 10.1007/s11430-024-1420-8
- Interactions between tectonics, bedrock inheritance and geomorphic responses of rivers in a post-rifting upland (Ponta Grossa Arch region, Brazil) M. Santos et al. 10.1590/2317-4889202220210002
- Denudation history of the Great Escarpment in the southwestern flank of the Angola (Bié) Dome, Africa B. Silva et al. 10.1007/s00531-022-02267-1
Latest update: 22 Nov 2024
Short summary
Plate tectonics drive the formation of mountain ranges. Yet when tectonic forces cease, mountain ranges persist for hundreds of millions of years, forming major Earth surface features. This work presents denudation rate estimates from one such ancient mountain range that show that denudation is strongly tied to rock type. Resistant rocks denude more slowly despite having much steeper topography, and contrasts in rock type cause increasing relief in the absence of active tectonics.
Plate tectonics drive the formation of mountain ranges. Yet when tectonic forces cease, mountain...
