Glacially moulded landslide runout debris in the Scottish Highlands
A tongue of hummocky terrain ∼1 km long and ∼400 m wide extends downslope from the source area of a rock-slope failure that formed the summit arête of Sgùrr nan Ceathreamhnan in the NW Highlands. The tongue descends from ∼810 m to ∼650 m, crosses a corrie obliquely and laps onto an opposing slope. I...
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Online Access: | https://hdl.handle.net/10023/18130 https://doi.org/10.1080/14702541.2018.1501085 |
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ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/18130 2024-05-19T07:42:11+00:00 Glacially moulded landslide runout debris in the Scottish Highlands Ballantyne, Colin K. University of St Andrews. School of Geography & Sustainable Development 2019-07-19 13 1830574 application/pdf https://hdl.handle.net/10023/18130 https://doi.org/10.1080/14702541.2018.1501085 eng eng Scottish Geographical Journal 255005398 c7f3747e-6089-481e-8e88-a25e2f0ad1ad 85050282981 000451529400009 Ballantyne , C K 2018 , ' Glacially moulded landslide runout debris in the Scottish Highlands ' , Scottish Geographical Journal , vol. 134 , no. 3-4 , pp. 224–236 . https://doi.org/10.1080/14702541.2018.1501085 1470-2541 RIS: urn:6026917B8D956A7BAAFBEB6FE377C44C https://hdl.handle.net/10023/18130 doi:10.1080/14702541.2018.1501085 Glacial bedforms Hummocks Lateglacial Loch Lomond Stade Rock avalanche Rock-slope failure G Geography (General) NDAS G1 Journal article 2019 ftstandrewserep https://doi.org/10.1080/14702541.2018.1501085 2024-04-30T23:32:55Z A tongue of hummocky terrain ∼1 km long and ∼400 m wide extends downslope from the source area of a rock-slope failure that formed the summit arête of Sgùrr nan Ceathreamhnan in the NW Highlands. The tongue descends from ∼810 m to ∼650 m, crosses a corrie obliquely and laps onto an opposing slope. Individual hummocks are circular to elongate, up to 6 m high and streamlined. A possible origin as recessional or ice-stagnation moraines is inconsistent with hummock morphology and the alignment of the hummock belt, and the streamlining of the hummocks is incompatible with the form of unmodified rock-avalanche runout hummocks. It is proposed that the tongue of hummocky terrain represents rock-slope failure during or after ice-sheet deglaciation, and subsequent modification of runout debris by subglacial erosion during the Loch Lomond Stade (∼12.9–11.7 ka). This interpretation implies (i) that the debris was deposited by an excess-runout rock avalanche; (ii) that the glacier that subsequently occupied the corrie was warm-based; (iii) that Lateglacial landslide runout debris was not invariably evacuated by Loch Lomond Stadial glaciers, as previously suggested; and (iv) that some features interpreted as hummocky moraines elsewhere may have a similar origin. Peer reviewed Article in Journal/Newspaper Ice Sheet University of St Andrews: Digital Research Repository Scottish Geographical Journal 134 3-4 224 236 |
institution |
Open Polar |
collection |
University of St Andrews: Digital Research Repository |
op_collection_id |
ftstandrewserep |
language |
English |
topic |
Glacial bedforms Hummocks Lateglacial Loch Lomond Stade Rock avalanche Rock-slope failure G Geography (General) NDAS G1 |
spellingShingle |
Glacial bedforms Hummocks Lateglacial Loch Lomond Stade Rock avalanche Rock-slope failure G Geography (General) NDAS G1 Ballantyne, Colin K. Glacially moulded landslide runout debris in the Scottish Highlands |
topic_facet |
Glacial bedforms Hummocks Lateglacial Loch Lomond Stade Rock avalanche Rock-slope failure G Geography (General) NDAS G1 |
description |
A tongue of hummocky terrain ∼1 km long and ∼400 m wide extends downslope from the source area of a rock-slope failure that formed the summit arête of Sgùrr nan Ceathreamhnan in the NW Highlands. The tongue descends from ∼810 m to ∼650 m, crosses a corrie obliquely and laps onto an opposing slope. Individual hummocks are circular to elongate, up to 6 m high and streamlined. A possible origin as recessional or ice-stagnation moraines is inconsistent with hummock morphology and the alignment of the hummock belt, and the streamlining of the hummocks is incompatible with the form of unmodified rock-avalanche runout hummocks. It is proposed that the tongue of hummocky terrain represents rock-slope failure during or after ice-sheet deglaciation, and subsequent modification of runout debris by subglacial erosion during the Loch Lomond Stade (∼12.9–11.7 ka). This interpretation implies (i) that the debris was deposited by an excess-runout rock avalanche; (ii) that the glacier that subsequently occupied the corrie was warm-based; (iii) that Lateglacial landslide runout debris was not invariably evacuated by Loch Lomond Stadial glaciers, as previously suggested; and (iv) that some features interpreted as hummocky moraines elsewhere may have a similar origin. Peer reviewed |
author2 |
University of St Andrews. School of Geography & Sustainable Development |
format |
Article in Journal/Newspaper |
author |
Ballantyne, Colin K. |
author_facet |
Ballantyne, Colin K. |
author_sort |
Ballantyne, Colin K. |
title |
Glacially moulded landslide runout debris in the Scottish Highlands |
title_short |
Glacially moulded landslide runout debris in the Scottish Highlands |
title_full |
Glacially moulded landslide runout debris in the Scottish Highlands |
title_fullStr |
Glacially moulded landslide runout debris in the Scottish Highlands |
title_full_unstemmed |
Glacially moulded landslide runout debris in the Scottish Highlands |
title_sort |
glacially moulded landslide runout debris in the scottish highlands |
publishDate |
2019 |
url |
https://hdl.handle.net/10023/18130 https://doi.org/10.1080/14702541.2018.1501085 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
Scottish Geographical Journal 255005398 c7f3747e-6089-481e-8e88-a25e2f0ad1ad 85050282981 000451529400009 Ballantyne , C K 2018 , ' Glacially moulded landslide runout debris in the Scottish Highlands ' , Scottish Geographical Journal , vol. 134 , no. 3-4 , pp. 224–236 . https://doi.org/10.1080/14702541.2018.1501085 1470-2541 RIS: urn:6026917B8D956A7BAAFBEB6FE377C44C https://hdl.handle.net/10023/18130 doi:10.1080/14702541.2018.1501085 |
op_doi |
https://doi.org/10.1080/14702541.2018.1501085 |
container_title |
Scottish Geographical Journal |
container_volume |
134 |
container_issue |
3-4 |
container_start_page |
224 |
op_container_end_page |
236 |
_version_ |
1799481839350448128 |