Articles | Volume 14, issue 6
https://doi.org/10.5194/tc-14-1989-2020
© Author(s) 2020. 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-14-1989-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
18 Jun 2020
Research article |
| 18 Jun 2020
| 18 Jun 2020
A quasi-annual record of time-transgressive esker formation: implications for ice-sheet reconstruction and subglacial hydrology
Stephen J. Livingstone
CORRESPONDING AUTHOR
Department of Geography, University of Sheffield, Sheffield, UK
Emma L. M. Lewington
Department of Geography, University of Sheffield, Sheffield, UK
Chris D. Clark
Department of Geography, University of Sheffield, Sheffield, UK
Robert D. Storrar
Department of the Natural and Built Environment, Sheffield Hallam
University, Sheffield, UK
Andrew J. Sole
Department of Geography, University of Sheffield, Sheffield, UK
Isabelle McMartin
Geological Survey of Canada, Natural Resources Canada, Ottawa, ON, Canada
Nico Dewald
Department of Geography, University of Sheffield, Sheffield, UK
Department of Geography, University of Sheffield, Sheffield, UK
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Cited
20 citations as recorded by crossref.
- Distribution, characteristics and formation of esker enlargements N. Dewald et al. 10.1016/j.geomorph.2021.107919
- Regional stagnation of the western Keewatin ice sheet and the significance of meltwater corridors and eskers, northern Canada D. Sharpe et al. 10.1139/cjes-2020-0136
- Distinct modes of meltwater drainage and landform development beneath the last Barents Sea ice sheet C. Shackleton et al. 10.3389/feart.2023.1111396
- Subglacial meltwater routes of the Fennoscandian Ice Sheet N. Dewald et al. 10.1080/17445647.2022.2071648
- Multiple sites of recent wet-based glaciation identified from eskers in western Tempe Terra, Mars S. Woodley et al. 10.1016/j.icarus.2022.115147
- A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain S. Furze et al. 10.3390/rs13214210
- Advances in understanding subglacial meltwater drainage from past ice sheets L. Simkins et al. 10.1017/aog.2023.16
- Conceptual model for the formation of bedforms along subglacial meltwater corridors (SMCs) by variable ice‐water‐bed interactions J. Vérité et al. 10.1002/esp.5725
- The infill of tunnel valleys in the central North Sea: Implications for sedimentary processes, geohazards, and ice-sheet dynamics J. Kirkham et al. 10.1016/j.margeo.2023.107185
- Geological and glaciological controls of 21,700 active methane seeps in the northern Norwegian Barents sea P. Serov et al. 10.3389/feart.2024.1404027
- Footprint of the Baltic Ice Stream: geomorphic evidence for shifting ice stream pathways S. Greenwood et al. 10.1111/bor.12634
- Topographic Controls on Channelized Meltwater in the Subglacial Environment L. Simkins et al. 10.1029/2021GL094678
- A model for interaction between conduits and surrounding hydraulically connected distributed drainage based on geomorphological evidence from Keewatin, Canada E. Lewington et al. 10.5194/tc-14-2949-2020
- Tunnel valley infill and genesis revealed by high-resolution 3-D seismic data J. Kirkham et al. 10.1130/G49048.1
- Complex genesis of N-channel eskers illustrated with the example of an esker near Tosie (east-central Poland) M. Frydrych 10.18778/1427-9711.20.02
- The sedimentology and multi-stage evolution of a Pleistocene esker on soft substratum, a case from North Central Poland T. Salamon 10.1016/j.sedgeo.2024.106771
- Morphology of eskers in Poland, southward of the Last Glacial Maximum M. Frydrych 10.1016/j.geomorph.2022.108418
- A new map of glacigenic features and glacial landsystems in central mainland Nunavut, Canada I. McMartin et al. 10.1111/bor.12479
- Variations in esker morphology and internal architecture record time-transgressive deposition during ice margin retreat in Northern Ireland B. Stoker et al. 10.1016/j.pgeola.2021.03.002
- 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
20 citations as recorded by crossref.
- Distribution, characteristics and formation of esker enlargements N. Dewald et al. 10.1016/j.geomorph.2021.107919
- Regional stagnation of the western Keewatin ice sheet and the significance of meltwater corridors and eskers, northern Canada D. Sharpe et al. 10.1139/cjes-2020-0136
- Distinct modes of meltwater drainage and landform development beneath the last Barents Sea ice sheet C. Shackleton et al. 10.3389/feart.2023.1111396
- Subglacial meltwater routes of the Fennoscandian Ice Sheet N. Dewald et al. 10.1080/17445647.2022.2071648
- Multiple sites of recent wet-based glaciation identified from eskers in western Tempe Terra, Mars S. Woodley et al. 10.1016/j.icarus.2022.115147
- A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain S. Furze et al. 10.3390/rs13214210
- Advances in understanding subglacial meltwater drainage from past ice sheets L. Simkins et al. 10.1017/aog.2023.16
- Conceptual model for the formation of bedforms along subglacial meltwater corridors (SMCs) by variable ice‐water‐bed interactions J. Vérité et al. 10.1002/esp.5725
- The infill of tunnel valleys in the central North Sea: Implications for sedimentary processes, geohazards, and ice-sheet dynamics J. Kirkham et al. 10.1016/j.margeo.2023.107185
- Geological and glaciological controls of 21,700 active methane seeps in the northern Norwegian Barents sea P. Serov et al. 10.3389/feart.2024.1404027
- Footprint of the Baltic Ice Stream: geomorphic evidence for shifting ice stream pathways S. Greenwood et al. 10.1111/bor.12634
- Topographic Controls on Channelized Meltwater in the Subglacial Environment L. Simkins et al. 10.1029/2021GL094678
- A model for interaction between conduits and surrounding hydraulically connected distributed drainage based on geomorphological evidence from Keewatin, Canada E. Lewington et al. 10.5194/tc-14-2949-2020
- Tunnel valley infill and genesis revealed by high-resolution 3-D seismic data J. Kirkham et al. 10.1130/G49048.1
- Complex genesis of N-channel eskers illustrated with the example of an esker near Tosie (east-central Poland) M. Frydrych 10.18778/1427-9711.20.02
- The sedimentology and multi-stage evolution of a Pleistocene esker on soft substratum, a case from North Central Poland T. Salamon 10.1016/j.sedgeo.2024.106771
- Morphology of eskers in Poland, southward of the Last Glacial Maximum M. Frydrych 10.1016/j.geomorph.2022.108418
- A new map of glacigenic features and glacial landsystems in central mainland Nunavut, Canada I. McMartin et al. 10.1111/bor.12479
- Variations in esker morphology and internal architecture record time-transgressive deposition during ice margin retreat in Northern Ireland B. Stoker et al. 10.1016/j.pgeola.2021.03.002
- 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
Latest update: 13 Dec 2024
Short summary
We map series of aligned mounds (esker beads) across central Nunavut, Canada. Mounds are interpreted to have formed roughly annually as sediment carried by subglacial rivers is deposited at the ice margin. Chains of mounds are formed as the ice retreats. This high-resolution (annual) record allows us to constrain the pace of ice retreat, sediment fluxes, and the style of drainage through time. In particular, we suggest that eskers in general record a composite signature of ice-marginal drainage.
We map series of aligned mounds (esker beads) across central Nunavut, Canada. Mounds are...
