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Reconstructing the Holocene glacial history of northern Troms and western Finnmark, Arctic Norway

Leigh, Josh R.; Jones, Richard S.; Stokes, Chris R.; Evans, David J. A.; Carr, J. Rachel; Andreassen, Liss M.

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Authors

Profile image of Joshua Leigh

Joshua Leigh joshua.r.leigh@durham.ac.uk
PGR Student Doctor of Philosophy

Richard S. Jones

J. Rachel Carr

Liss M. Andreassen



Abstract

Here we present the first Lateglacial and Holocene glacial history from Rotsunddalen, northern Troms and western Finnmark county, northern Norway, based on both relative and numerical moraine dating using Schmidt hammer, soil chronosequencing and terrestrial cosmogenic nuclide dating. We combine these chronological data with a regional map of the glacial geomorphology to hypothesize key events in the glacial history from around 14 ka to present. Our reconstruction shows that, following deglaciation of the main ice sheet across central Troms and Finnmark, mountain glaciers were terminating on land, close to the coast, between around 12.1 and 10.6 ka. Continued recession of the main Fennoscandian Ice Sheet margin towards the SE led to the isolation of several large plateau icefields and outlet glaciers that generated moraines at around 10.2–9.2 ka, which we ascribe to the Erdalen Event, and 8.4–8.2 ka, which is broadly contemporaneous with the 8.2 ka cold event. Although the latter corresponds with the Scandinavian Finse Event, very few moraines have been dated to this time and we therefore view it as a tentative hypothesis for future work to test. During the Holocene Thermal Maximum (~6.6 to 6.3 ka) most (if not all) glaciers in the region disappeared, but then regrew during the Neoglaciation and produced large moraines dated to around 4.7 ka that lie a few hundred metres distal to the prominent Little Ice Age moraines (previously dated to AD 1810s–1870s). Given the limitations of our dating approach, the preservation of moraines dated to this period in northern Norway also warrants further investigation. We also highlight that terrestrial cosmogenic nuclide dating of the moraines is not consistent with other dating approaches and the widely established deglaciation history of the region, probably owing to cosmogenic inheritance and insufficient glacial erosion.

Citation

Leigh, J. R., Jones, R. S., Stokes, C. R., Evans, D. J. A., Carr, J. R., & Andreassen, L. M. (2024). Reconstructing the Holocene glacial history of northern Troms and western Finnmark, Arctic Norway. Boreas: An International Journal of Quaternary Research, 53(4, Special issue: Late Middle Pleistocene (MIS 11‐6) in Europe), 619-654. https://doi.org/10.1111/bor.12668

Journal Article Type Article
Acceptance Date May 14, 2024
Online Publication Date Jun 12, 2024
Publication Date 2024-10
Deposit Date May 15, 2024
Publicly Available Date Jun 13, 2024
Journal Boreas
Print ISSN 0300-9483
Electronic ISSN 1502-3885
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 53
Issue 4, Special issue: Late Middle Pleistocene (MIS 11‐6) in Europe
Pages 619-654
DOI https://doi.org/10.1111/bor.12668
Public URL https://durham-repository.worktribe.com/output/2440243

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