Articles | Volume 15, issue 6
https://doi.org/10.5194/tc-15-2889-2021
© 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/tc-15-2889-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
28 Jun 2021
Research article |
| 28 Jun 2021
| 28 Jun 2021
Formation of ribbed bedforms below shear margins and lobes of palaeo-ice streams
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans CEDEX 9,
France
Édouard Ravier
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans CEDEX 9,
France
Olivier Bourgeois
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Université de Nantes, 2 rue de la Houssinière, BP 92208, 44322
Nantes CEDEX 3, France
Stéphane Pochat
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Université de Nantes, 2 rue de la Houssinière, BP 92208, 44322
Nantes CEDEX 3, France
Thomas Lelandais
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans CEDEX 9,
France
Régis Mourgues
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans CEDEX 9,
France
Christopher D. Clark
Department of Geography, University of Sheffield, Sheffield, UK
Paul Bessin
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans CEDEX 9,
France
David Peigné
Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS,
Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans CEDEX 9,
France
Nigel Atkinson
Alberta Geological Survey, 4th Floor Twin Atria Building, 4999-98
Ave., Edmonton, AB, T6B 2X3, Canada
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Cited
13 citations as recorded by crossref.
- The Kola Peninsula and Russian Lapland: A review of Late Weichselian glaciation B. Boyes et al. 10.1016/j.quascirev.2021.107087
- Physical characteristics of hydrofracture systems and their fills in glacial sediments E. Ravier 10.1016/j.sedgeo.2024.106593
- A conceptual geological model for offshore wind sites in former ice stream settings: the Utsira Nord site, North Sea H. Petrie et al. 10.1144/jgs2021-163
- Footprint of the Baltic Ice Stream: geomorphic evidence for shifting ice stream pathways S. Greenwood et al. 10.1111/bor.12634
- Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers É. Ravier et al. 10.1017/jog.2022.107
- Reconstructing terrestrial ice sheet retreat dynamics from hummocky topography using multiscale evidence: An example from central Ireland C. Delaney et al. 10.1016/j.quascirev.2023.108041
- GIS dataset: geomorphological record of terrestrial-terminating ice streams, southern sector of the Baltic Ice Stream Complex, last Scandinavian Ice Sheet, Poland I. Szuman et al. 10.5194/essd-13-4635-2021
- The last Fennoscandian Ice Sheet glaciation on the Kola Peninsula and Russian Lapland (Part 1): Ice flow configuration B. Boyes et al. 10.1016/j.quascirev.2022.107871
- The kinematic significance of subglacial bedforms and their use in palaeo-glaciological reconstructions J. Vérité et al. 10.1016/j.epsl.2023.118510
- Formation of Murtoos by Repeated Flooding of Ribbed Bedforms Along Subglacial Meltwater Corridors J. Vérité et al. 10.2139/ssrn.3978870
- Formation of murtoos by repeated flooding of ribbed bedforms along subglacial meltwater corridors J. Vérité et al. 10.1016/j.geomorph.2022.108248
- Late erosion pulse triggered by rapid melt in the cold‐based interior of the last Fennoscandian Ice Sheet, an example from Rogen M. van Boeckel et al. 10.1002/esp.5464
- New metrics reveal the evolutionary continuum behind the morphological diversity of subglacial bedforms J. Vérité et al. 10.1016/j.geomorph.2023.108627
13 citations as recorded by crossref.
- The Kola Peninsula and Russian Lapland: A review of Late Weichselian glaciation B. Boyes et al. 10.1016/j.quascirev.2021.107087
- Physical characteristics of hydrofracture systems and their fills in glacial sediments E. Ravier 10.1016/j.sedgeo.2024.106593
- A conceptual geological model for offshore wind sites in former ice stream settings: the Utsira Nord site, North Sea H. Petrie et al. 10.1144/jgs2021-163
- Footprint of the Baltic Ice Stream: geomorphic evidence for shifting ice stream pathways S. Greenwood et al. 10.1111/bor.12634
- Variations in hydraulic efficiency of the subglacial drainage landsystem control surging and streaming regimes of outlet glaciers É. Ravier et al. 10.1017/jog.2022.107
- Reconstructing terrestrial ice sheet retreat dynamics from hummocky topography using multiscale evidence: An example from central Ireland C. Delaney et al. 10.1016/j.quascirev.2023.108041
- GIS dataset: geomorphological record of terrestrial-terminating ice streams, southern sector of the Baltic Ice Stream Complex, last Scandinavian Ice Sheet, Poland I. Szuman et al. 10.5194/essd-13-4635-2021
- The last Fennoscandian Ice Sheet glaciation on the Kola Peninsula and Russian Lapland (Part 1): Ice flow configuration B. Boyes et al. 10.1016/j.quascirev.2022.107871
- The kinematic significance of subglacial bedforms and their use in palaeo-glaciological reconstructions J. Vérité et al. 10.1016/j.epsl.2023.118510
- Formation of Murtoos by Repeated Flooding of Ribbed Bedforms Along Subglacial Meltwater Corridors J. Vérité et al. 10.2139/ssrn.3978870
- Formation of murtoos by repeated flooding of ribbed bedforms along subglacial meltwater corridors J. Vérité et al. 10.1016/j.geomorph.2022.108248
- Late erosion pulse triggered by rapid melt in the cold‐based interior of the last Fennoscandian Ice Sheet, an example from Rogen M. van Boeckel et al. 10.1002/esp.5464
- New metrics reveal the evolutionary continuum behind the morphological diversity of subglacial bedforms J. Vérité et al. 10.1016/j.geomorph.2023.108627
Discussed (preprint)
Latest update: 29 Jun 2024
Short summary
Subglacial bedforms are commonly used to reconstruct past glacial dynamics and investigate processes occuring at the ice–bed interface. Using analogue modelling and geomorphological mapping, we demonstrate that ridges with undulating crests, known as subglacial ribbed bedforms, are ubiquitous features along ice stream corridors. These bedforms provide a tantalizing glimpse into (1) the former positions of ice stream margins, (2) the ice lobe dynamics and (3) the meltwater drainage efficiency.
Subglacial bedforms are commonly used to reconstruct past glacial dynamics and investigate...
