Matthews, John A., Wilson, Peter, Winkler, Stefan, Mourne, Richard W., Hill, Jennifer L. ORCID: 0000-0002-0682-783X, Owen, Geraint, Hiemstra, John F., Hallang, Helen and Geary, Andrew P. (2019) Age and development of active cryoplanation terraces in the alpine permafrost zone at Svartkampan, Jotunheimen, southern Norway. Quaternary Research, 92 (3). pp. 641-664. doi:10.1017/qua.2019.41
|
Text
7810-Hill-(2019)-Age-and-development-of-active-cryoplanation-terraces.pdf - Accepted Version Available under License All Rights Reserved. Download (3MB) | Preview |
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.
Item Type: | Article |
---|---|
Article Type: | Article |
Uncontrolled Keywords: | Cryoplanation terraces; Schmidt-hammer exposure-age dating; Mountain permafrost; Periglacial processes; Alpine landform development; Frost weathering; Nivation |
Subjects: | G Geography. Anthropology. Recreation > GB Physical geography |
Divisions: | Professional Services > Academic Quality, Enhancement and Innovation |
Research Priority Areas: | Society and Learning |
Depositing User: | Susan Turner |
Date Deposited: | 20 Dec 2019 15:47 |
Last Modified: | 04 Feb 2022 15:30 |
URI: | https://eprints.glos.ac.uk/id/eprint/7810 |
University Staff: Request a correction | Repository Editors: Update this record