B.J. Davies
Dynamic ice stream retreat in the central sector of the last British-Irish Ice Sheet
Davies, B.J.; Livingstone, S.J.; Roberts, D.H.; Evans, D.J.A.; Gheorghiu, D.M.; Ó Cofaigh, C.
Authors
S.J. Livingstone
Professor Dave Roberts d.h.roberts@durham.ac.uk
Professor
Professor David Evans d.j.a.evans@durham.ac.uk
Professor
D.M. Gheorghiu
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Head Of Department
Abstract
During the Last Glacial Maximum (LGM), ice streams of the last British-Irish Ice Sheet (BIIS) controlled ice discharge from various dispersal centres. Deglaciation was characterised by shifts in ice-divide location and changes in internal ice-sheet dynamics, resulting in substantial flow switches and significant ice-stream reconfiguration, and hence modification of their landform signatures. We present new geomorphological mapping and 11 10Be cosmogenic nuclide ages from Northern England (Stainmore Gap, Eden Valley and Vale of York), that constrain regional dynamic ice-stream retreat following the LGM. We identify complex decoupling of competing ice lobes, characterised by early retreat of the North Sea Lobe and a minor re-advance of Stainmore ice prior to ∼20 ka. This was followed by rapid recession of the central Stainmore Gap, which was ice-free by 19.8 ± 0.7 to 18.0 ± 0.5 ka, contemporaneous with the recession of the Tyne Gap Ice Stream. In the southern Vale of Eden, Crossby Ravensworth Fell became exposed between 19.2 and 20.3 ka. The northwards ice-flow reversal in the Vale of Eden was associated with the development of ice domes across the northern Pennines, Howgill Fells and the Lake District. This shift in dispersal centres and ice divide migration likely triggered the rapid collapse of eastward ice stream corridors. The central sector of the BIIS rapidly collapsed back up into upland dispersal centres between 20 and 17.5 ka. This work highlights the role internal factors, such as topography, in driving ice-divide migration and flow switches during externally and climatically forced ice-sheet thinning.
Citation
Davies, B., Livingstone, S., Roberts, D., Evans, D., Gheorghiu, D., & Ó Cofaigh, C. (2019). Dynamic ice stream retreat in the central sector of the last British-Irish Ice Sheet. Quaternary Science Reviews, 225, Article 105989. https://doi.org/10.1016/j.quascirev.2019.105989
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 3, 2019 |
Online Publication Date | Oct 12, 2019 |
Publication Date | Dec 31, 2019 |
Deposit Date | Oct 15, 2019 |
Publicly Available Date | Oct 15, 2019 |
Journal | Quaternary Science Reviews |
Print ISSN | 0277-3791 |
Electronic ISSN | 1873-457X |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 225 |
Article Number | 105989 |
DOI | https://doi.org/10.1016/j.quascirev.2019.105989 |
Public URL | https://durham-repository.worktribe.com/output/1282788 |
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Copyright Statement
© 2019 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/)
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