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Age and development of active cryoplanation terraces in the alpine permafrost zone at Svartkampan, Jotunheimen, southern Norway

Matthews, John A.; Wilson, Peter; Winkler, Stefan; Mourne, Richard W.; Hill, Jennifer L.; Owen, Geraint; Hiemstra, John F.; Hallang, Helen; Geary, Andrew P.

Authors

John A. Matthews

Peter Wilson

Stefan Winkler

Jenny Hill Jennifer.Hill@uwe.ac.uk
Associate Professor in Teaching and Learning

Geraint Owen

John F. Hiemstra

Helen Hallang

Andrew P. Geary andrew.geary@uwe.ac.uk



Abstract

Schmidt-hammer exposure-age dating (SHD) of boulders on cryoplanation terrace treads and associated bedrock cliff faces revealed Holocene ages ranging from 0 ± 825 to 8890 ± 1185 yr. The cliffs were significantly younger than the inner treads, which tended to be younger than the outer treads. Radiocarbon dates from the regolith of 3854 to 4821 cal yr BP (2σ range) indicated maximum rates of cliff recession of ~0.1 mm/year, which suggests the onset of terrace formation prior to the last glacial maximum. Age, angularity and size of clasts, together with planation across bedrock structures and the seepage of groundwater from the cliff foot, all support a process-based conceptual model of cryoplanation terrace development in which frost weathering leads to parallel cliff recession and hence terrace extension. The availability of groundwater during autumn freeze-back is viewed as critical for frost wedging and/or the growth of segregation ice during prolonged winter frost penetration. Permafrost promotes cryoplanation by providing an impermeable frost table beneath the active layer, focusing groundwater flow, and supplying water for sediment transport by solifluction across the tread. Snowbeds are considered an effect rather than a cause of cryoplanation terraces and cryoplanation is seen as distinct from nivation.

Citation

Matthews, J. A., Wilson, P., Winkler, S., Mourne, R. W., Hill, J. L., Owen, G., …Geary, A. P. (2019). Age and development of active cryoplanation terraces in the alpine permafrost zone at Svartkampan, Jotunheimen, southern Norway. Quaternary Research, 92(3), 641-664. https://doi.org/10.1017/qua.2019.41

Journal Article Type Article
Acceptance Date Jun 13, 2019
Online Publication Date Sep 9, 2019
Publication Date Nov 1, 2019
Publicly Available Date Mar 10, 2020
Journal Quaternary Research
Print ISSN 0033-5894
Electronic ISSN 1096-0287
Publisher Cambridge University Press (CUP)
Peer Reviewed Peer Reviewed
Volume 92
Issue 3
Pages 641-664
DOI https://doi.org/10.1017/qua.2019.41
Keywords cryoplanation terraces, Schmidt-hammer exposure-age dating, mountain permafrost, periglacial processes, alpine landform development, frost weathering, nivation
Public URL https://uwe-repository.worktribe.com/output/1492860

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Cryoplanation - final accepted manuscript (3).pdf (806 Kb)
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Copyright Statement
This is the author's accepted manuscript. Not for re-distribution or re-use. © copyright holder. The final published version is available online at: https://doi.org/10.1017/qua.2019.41





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