Louise Best
Scottish landform example: isolation basins of Arisaig
Best, Louise; Shennan, Ian
Abstract
An isolation basin is a geomorphological landform that enables the precise reconstruction of the former height and age of relative sea level. A series of isolation basins at different elevations within a small geographical area can provide a high-resolution record of the timing and magnitude of relative sea-level change. Arisaig, on the west coast of Scotland, provides the longest post- Last Glacial Maximum record of relative sea-level change in the UK, produced from the analysis of a series of 16 isolation basins. The records produced from these basins continue to provide important constraints that inform understanding of processes acting from local to global scales, such as glacial and climatic transitions, glacio-isostatic adjustment and global meltwater pulses.
Citation
Best, L., & Shennan, I. (online). Scottish landform example: isolation basins of Arisaig. Scottish Geographical Journal, 1-20. https://doi.org/10.1080/14702541.2024.2401166
Journal Article Type | Article |
---|---|
Acceptance Date | Aug 19, 2024 |
Online Publication Date | Sep 11, 2024 |
Deposit Date | Nov 27, 2024 |
Publicly Available Date | Nov 27, 2024 |
Journal | Scottish Geographical Journal |
Print ISSN | 1470-2541 |
Electronic ISSN | 1751-665X |
Publisher | Taylor and Francis Group |
Peer Reviewed | Peer Reviewed |
Pages | 1-20 |
DOI | https://doi.org/10.1080/14702541.2024.2401166 |
Keywords | sea level; isolation basin; glacio-isostatic adjustment; NW Scotland |
Public URL | https://durham-repository.worktribe.com/output/3107273 |
Additional Information | Peer Review Statement: The publishing and review policy for this title is described in its Aims & Scope.; Aim & Scope: http://www.tandfonline.com/action/journalInformation?show=aimsScope&journalCode=rsgj20; Received: 2024-02-08; Accepted: 2024-08-29; Published: 2024-09-11 |
Other Repo URL | https://eprints.glos.ac.uk/14374/ |
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Copyright Statement
This accepted manuscript is licensed under the Creative Commons Attribution 4.0 licence. https://creativecommons.org/licenses/by/4.0/
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