Age and significance of mountain-top detritus
In north-west Scotland, mountain-top detritus forms blockfields or diamicts, depending on lithology. Clast angularity, absence of grussification and transition to underlying rock imply formation by frost-wedging of bedrock. Age is constrained by trimlines and exposure dating of weathering zones. Mou...
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1998
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Online Access: | https://research-portal.st-andrews.ac.uk/en/researchoutput/age-and-significance-of-mountaintop-detritus(8ee1b78d-8e28-4dec-bc7f-9ca9cc2ec945).html https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 http://www.scopus.com/inward/record.url?scp=0032421874&partnerID=8YFLogxK |
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ftunstandrewcris:oai:research-portal.st-andrews.ac.uk:publications/8ee1b78d-8e28-4dec-bc7f-9ca9cc2ec945 2024-06-23T07:53:46+00:00 Age and significance of mountain-top detritus Ballantyne, Colin Kerr 1998-10 https://research-portal.st-andrews.ac.uk/en/researchoutput/age-and-significance-of-mountaintop-detritus(8ee1b78d-8e28-4dec-bc7f-9ca9cc2ec945).html https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 http://www.scopus.com/inward/record.url?scp=0032421874&partnerID=8YFLogxK eng eng https://research-portal.st-andrews.ac.uk/en/researchoutput/age-and-significance-of-mountaintop-detritus(8ee1b78d-8e28-4dec-bc7f-9ca9cc2ec945).html info:eu-repo/semantics/restrictedAccess Ballantyne , C K 1998 , ' Age and significance of mountain-top detritus ' , Permafrost and Periglacial Processes , vol. 9 , no. 4 , pp. 327-345 . https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 mountain-top detritus blockfields weathering periglacial trimlines weathering zones clay minerals cosmogenic isotope dating LAST ICE-SHEET NORTHWEST SCOTLAND SOUTHERN NORWAY HIGH PLATEAUS GLACIATION HIGHLANDS ALTITUDE NUNATAKS GASPESIE ICEFIELD article 1998 ftunstandrewcris https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 2024-06-13T00:03:34Z In north-west Scotland, mountain-top detritus forms blockfields or diamicts, depending on lithology. Clast angularity, absence of grussification and transition to underlying rock imply formation by frost-wedging of bedrock. Age is constrained by trimlines and exposure dating of weathering zones. Mountain-top detritus is ubiquitous on nunataks that remained above the level of the last ice sheet, but occurs only on well-jointed rocks in areas exposed to periglacial conditions since ice-sheet downwastage and is absent from areas exposed to weathering only during the Holocene. Most secondary clay minerals are equally represented both above and below a trimline cut by the last ice sheet, indicating formation since deglaciation, though haematite and gibbsite are preferentially represented on former nunataks. The age and significance of mountain-top detritus are determined by lithology and glacial history. On well-jointed rocks, such detritus has developed within a few millennia of exposure to periglacial conditions. On massive lithologies, however, it has formed over much longer timescales on nunataks above the last and possibly earlier ice sheets. In north-east Scotland ancient (possibly pre-Pleistocene) regolith also appears to have survived under a cover of cold-based ice. Use of the distribution of mountain-top detritus in palaeoglaciological reconstructions therefore requires caution. (C) 1998 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice Sheet Permafrost and Periglacial Processes University of St Andrews: Research Portal Norway |
institution |
Open Polar |
collection |
University of St Andrews: Research Portal |
op_collection_id |
ftunstandrewcris |
language |
English |
topic |
mountain-top detritus blockfields weathering periglacial trimlines weathering zones clay minerals cosmogenic isotope dating LAST ICE-SHEET NORTHWEST SCOTLAND SOUTHERN NORWAY HIGH PLATEAUS GLACIATION HIGHLANDS ALTITUDE NUNATAKS GASPESIE ICEFIELD |
spellingShingle |
mountain-top detritus blockfields weathering periglacial trimlines weathering zones clay minerals cosmogenic isotope dating LAST ICE-SHEET NORTHWEST SCOTLAND SOUTHERN NORWAY HIGH PLATEAUS GLACIATION HIGHLANDS ALTITUDE NUNATAKS GASPESIE ICEFIELD Ballantyne, Colin Kerr Age and significance of mountain-top detritus |
topic_facet |
mountain-top detritus blockfields weathering periglacial trimlines weathering zones clay minerals cosmogenic isotope dating LAST ICE-SHEET NORTHWEST SCOTLAND SOUTHERN NORWAY HIGH PLATEAUS GLACIATION HIGHLANDS ALTITUDE NUNATAKS GASPESIE ICEFIELD |
description |
In north-west Scotland, mountain-top detritus forms blockfields or diamicts, depending on lithology. Clast angularity, absence of grussification and transition to underlying rock imply formation by frost-wedging of bedrock. Age is constrained by trimlines and exposure dating of weathering zones. Mountain-top detritus is ubiquitous on nunataks that remained above the level of the last ice sheet, but occurs only on well-jointed rocks in areas exposed to periglacial conditions since ice-sheet downwastage and is absent from areas exposed to weathering only during the Holocene. Most secondary clay minerals are equally represented both above and below a trimline cut by the last ice sheet, indicating formation since deglaciation, though haematite and gibbsite are preferentially represented on former nunataks. The age and significance of mountain-top detritus are determined by lithology and glacial history. On well-jointed rocks, such detritus has developed within a few millennia of exposure to periglacial conditions. On massive lithologies, however, it has formed over much longer timescales on nunataks above the last and possibly earlier ice sheets. In north-east Scotland ancient (possibly pre-Pleistocene) regolith also appears to have survived under a cover of cold-based ice. Use of the distribution of mountain-top detritus in palaeoglaciological reconstructions therefore requires caution. (C) 1998 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Ballantyne, Colin Kerr |
author_facet |
Ballantyne, Colin Kerr |
author_sort |
Ballantyne, Colin Kerr |
title |
Age and significance of mountain-top detritus |
title_short |
Age and significance of mountain-top detritus |
title_full |
Age and significance of mountain-top detritus |
title_fullStr |
Age and significance of mountain-top detritus |
title_full_unstemmed |
Age and significance of mountain-top detritus |
title_sort |
age and significance of mountain-top detritus |
publishDate |
1998 |
url |
https://research-portal.st-andrews.ac.uk/en/researchoutput/age-and-significance-of-mountaintop-detritus(8ee1b78d-8e28-4dec-bc7f-9ca9cc2ec945).html https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 http://www.scopus.com/inward/record.url?scp=0032421874&partnerID=8YFLogxK |
geographic |
Norway |
geographic_facet |
Norway |
genre |
Ice Sheet Permafrost and Periglacial Processes |
genre_facet |
Ice Sheet Permafrost and Periglacial Processes |
op_source |
Ballantyne , C K 1998 , ' Age and significance of mountain-top detritus ' , Permafrost and Periglacial Processes , vol. 9 , no. 4 , pp. 327-345 . https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 |
op_relation |
https://research-portal.st-andrews.ac.uk/en/researchoutput/age-and-significance-of-mountaintop-detritus(8ee1b78d-8e28-4dec-bc7f-9ca9cc2ec945).html |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1002/(SICI)1099-1530(199810/12)9:4%3C327::AID-PPP298%3E3.3.CO;2-0 |
_version_ |
1802645575163707392 |