Patterns of glacio‐isostatic adjustment in mainland Scotland: new data from western central Scotland, proximal to the zone of maximum rebound
Journal article
Smith, David, Firth, Callum R. and Rose, James 2024. Patterns of glacio‐isostatic adjustment in mainland Scotland: new data from western central Scotland, proximal to the zone of maximum rebound. Boreas. https://doi.org/10.1111/bor.12650
| Authors | Smith, David, Firth, Callum R. and Rose, James |
|---|---|
| Abstract | The results of geomorphological mapping and survey of Lateglacial and Holocene displaced shorelines in the Clyde estuary and around Loch Lomond, western central Scotland are described. On the basis of morphology, sedimentology, altitude and radiocarbon dating, four discrete shorelines are identified and are correlated with previously identified Scottish displaced shorelines. The shoreline formerly referred to as the Main Postglacial Shoreline is renamed the Menteith Shoreline. This body of data, combined with data on displaced shorelines for Scotland as a whole has been analysed using Gaussian quadratic trend surface analysis in order to determine the centre of glacio‐isostatic displacement for each shoreline. These Gaussian models of palaeo‐relative sea‐level suggest that the zone of greatest displacement lay NNW of Loch Lomond in the Lateglacial then moved SSE to the region of Loch Lomond during the Holocene and the Clyde in the Late Holocene. The factors responsible for the movement of the zone of greatest uplift are discussed, including temporal variations in the ice‐sheet thickness, variations in water load in the adjacent sea‐lochs and neotectonic processes. Comparison is made with glacial isostatic adjustment (GIA) models. A sensitivity analysis has been carried out on the use of Gaussian trend surface analysis glacio‐isostatic modelling and this is included in the research evaluation, and reported in full in the Supporting Information files, along with the raw data used throughout this study. |
| Keywords | Geology; Archeology |
| Year | 2024 |
| Journal | Boreas |
| Publisher | Wiley |
| ISSN | 0300-9483 |
| 1502-3885 | |
| Digital Object Identifier (DOI) | https://doi.org/10.1111/bor.12650 |
| Official URL | https://onlinelibrary.wiley.com/doi/full/10.1111/bor.12650 |
| Publication dates | |
| 24 Feb 2024 | |
| Online | 23 Feb 2024 |
| Publication process dates | |
| Deposited | 26 Feb 2024 |
| Accepted | 16 Jan 2024 |
| Publisher's version | License File Access Level Open |
| Supplemental file | File Access Level Open |
| Output status | Published |
| License | http://creativecommons.org/licenses/by/4.0/ |
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https://repository.canterbury.ac.uk/item/972yv/patterns-of-glacio-isostatic-adjustment-in-mainland-scotland-new-data-from-western-central-scotland-proximal-to-the-zone-of-maximum-rebound
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Publisher's version
| Boreas - 2024 - Smith - Patterns of glacio‐isostatic adjustment in mainland Scotland new data from western central.pdf | ||
| License: CC BY 4.0 | ||
| File access level: Open | ||
Supplemental file
| Table S1.xls | ||
| Table S2.xlsx | ||
| Data S1.doc | ||
| File access level: Open | ||
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