Articles | Volume 4, issue 1
https://doi.org/10.5194/esurf-4-1-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/esurf-4-1-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
15 Jan 2016
Research article |
| 15 Jan 2016
Tectonic geomorphology at small catchment sizes – extensions of the stream-power approach and the χ method
S. Hergarten
CORRESPONDING AUTHOR
Institut für Geo- und Umweltnaturwissenschaften, Albert-Ludwigs-Universität Freiburg, Freiburg im Breisgau, Germany
Institut für Geographie und Geologie, Universität Salzburg, Salzburg, Austria
Institut für Erdwissenschaften, NAWI Graz, Karl-Franzens-Universität Graz, Graz, Austria
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37 citations as recorded by crossref.
- Drivers of landscape evolution in eastern Tibet L. Yan et al. 10.1016/j.geomorph.2022.108478
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- The topography of a continental indenter: The interplay between crustal deformation, erosion, and base level changes in the eastern Southern Alps J. Robl et al. 10.1002/2016JF003884
- Detection of channel-hillslope coupling along a tectonic gradient M. Hurst et al. 10.1016/j.epsl.2019.06.018
- Combining geomorphometry, feature extraction techniques and Earth-surface processes research: The way forward G. Sofia 10.1016/j.geomorph.2020.107055
- Debris‐Flow Process Controls on Steepland Morphology in the San Gabriel Mountains, California W. Struble et al. 10.1029/2022JF007017
- Short communication: Forward and inverse analytic models relating river long profile to tectonic uplift history, assuming a nonlinear slope–erosion dependency Y. Wang et al. 10.5194/esurf-10-833-2022
- Clustering River Profiles to Classify Geomorphic Domains F. Clubb et al. 10.1029/2019JF005025
- A Robust Channel Head Extraction Method Based on High‐Resolution Topographic Convergence, Suitable for Both Slowly and Fastly Eroding Landscapes A. Lurin et al. 10.1029/2022JF006999
- Evidence for pre-Pleistocene landforms in the Eastern Alps: Geomorphological constraints from the Gurktal Alps T. Bartosch & K. Stüwe 10.17738/ajes.2019.0006
- Isolating climatic, tectonic, and lithologic controls on mountain landscape evolution J. Leonard et al. 10.1126/sciadv.add8915
- Old orogen – young topography: Evidence for relief rejuvenation in the Bohemian Massif K. Wetzlinger et al. 10.17738/ajes.2023.0002
- 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
- Fault activity in the San Gabriel Mountains, southern California, USA: Insights from landscape morphometrics, erosion rates, and fault-slip rates A. Mere & D. McPhillips 10.1130/B37218.1
- 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
- Progressive evolution of thrust fold topography in the frontal Himalaya D. Wahyudi et al. 10.1016/j.geomorph.2021.107717
- Rectangular drainage pattern evolution controlled by pipe cave collapse along clastic dikes, the Dead Sea Basin, Israel M. Hamawi et al. 10.1002/esp.5295
- Northeastward expansion of the Tibetan Plateau: Topographic evidence from the North Qinling Mts.–Weihe Graben Coupling system, Central China M. Duan et al. 10.1016/j.palaeo.2023.111612
- Geomorphic signature of segmented relief rejuvenation in the Sierra Morena, Betic forebulge, Spain I. Expósito et al. 10.5194/esurf-10-1017-2022
- The topographic state of fluvially conditioned mountain ranges J. Robl et al. 10.1016/j.earscirev.2017.03.007
- Geomorphometry today I. Florinsky 10.35595/2414-9179-2021-2-27-394-448
- Coarse sediment supply sets the slope of bedrock channels in rapidly uplifting terrain: Field and topographic evidence from eastern Taiwan L. Lai et al. 10.1002/esp.5200
- The Influence of Sediment Transport on Stationary and Mobile Knickpoints in River Profiles S. Hergarten 10.1029/2021JF006218
- Gölmarmara Fayı’nın Morfotektonik Evriminin CBS Tabanlı Yöntemlerle Araştırılması, Gediz Grabeni, Batı Anadolu S. ESKİ et al. 10.25288/tjb.679584
- The destiny of orogen-parallel streams in the Eastern Alps: the Salzach–Enns drainage system G. Trost et al. 10.5194/esurf-8-69-2020
- Comparing methods for calculating channel steepness index A. Smith et al. 10.1016/j.earscirev.2022.103970
- A systematic approach and software for the analysis of point patterns on river networks W. Schwanghart et al. 10.1002/esp.5127
- Impact of Changing Concavity Indices on Channel Steepness and Divide Migration Metrics B. Gailleton et al. 10.1029/2020JF006060
- The linear feedback precipitation model (LFPM 1.0) – a simple and efficient model for orographic precipitation in the context of landform evolution modeling S. Hergarten & J. Robl 10.5194/gmd-15-2063-2022
- How erosional efficiency modulates landscape response to drainage reorganization: New empirical evidence from the Andes H. García-Delgado et al. 10.1016/j.geomorph.2023.108893
- Quantifying the transient landscape response to active faulting using fluvial geomorphic analysis in the Qianhe Graben on the southwest margin of Ordos, China Z. Liu et al. 10.1016/j.geomorph.2019.106974
- Landscape ‘stress’ and reorganization from χ‐maps: Insights from experimental drainage networks in oblique collision setting L. Guerit et al. 10.1002/esp.4477
- Evidence for and against landscape transience in the Northern Qinling Mountains, China Y. Wang & S. Mudd 10.1016/j.geomorph.2021.107890
- How concave are river channels? S. Mudd et al. 10.5194/esurf-6-505-2018
- Impact of climate on landscape form, sediment transfer and the sedimentary record R. Harries et al. 10.1002/esp.5075
- Frontiers in Geomorphometry and Earth Surface Dynamics: possibilities, limitations and perspectives G. Sofia et al. 10.5194/esurf-4-721-2016
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Latest update: 21 Nov 2024
Short summary
Longitudinal river profiles are increasingly used for unraveling the tectonic history on a regional scale. In the last years, the introduction of the so-called chi transform brought significant technical progress, but this method is still limited to the domain governed by fluvial erosion covering only a small part of the surface. Here we present and compare extensions of the method towards smaller catchment sizes where hillslope processes or debris flows significantly contribute to erosion.
Longitudinal river profiles are increasingly used for unraveling the tectonic history on a...
Special issue