Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden
Despite a long history of glaciological research, the palaeo‐environmental significance of moraine systems in the Kebnekaise Mountains, Sweden, has remained uncertain. These landforms offer the potential to elucidate glacier response prior to the period of direct monitoring and provide an insight in...
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crwiley:10.1111/bor.12220 2024-09-15T18:26:08+00:00 Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden Tonkin, Toby N. Midgley, Nicholas G. Graham, David J. Labadz, Jillian C. Seventh Framework Programme 2016 http://dx.doi.org/10.1111/bor.12220 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12220 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12220 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 46, issue 2, page 199-211 ISSN 0300-9483 1502-3885 journal-article 2016 crwiley https://doi.org/10.1111/bor.12220 2024-06-25T04:16:17Z Despite a long history of glaciological research, the palaeo‐environmental significance of moraine systems in the Kebnekaise Mountains, Sweden, has remained uncertain. These landforms offer the potential to elucidate glacier response prior to the period of direct monitoring and provide an insight into the ice‐marginal processes operating at polythermal valley glaciers. This study set out to test existing interpretations of Scandinavian ice‐marginal moraines, which invoke ice stagnation, pushing, stacking/dumping and push‐deformation as important moraine forming processes. Moraines at Isfallsglaciären were investigated using ground‐penetrating radar to document the internal structural characteristics of the landform assemblage. Radar surveys revealed a range of substrate composition and reflectors, indicating a debris‐ice interface and bounding surfaces within the moraine. The moraine is demonstrated to contain both ice‐rich and debris‐rich zones, reflecting a complex depositional history and a polygenetic origin. As a consequence of glacier overriding, the morphology of these landforms provides a misleading indicator of glacial history. Traditional geochronological methods are unlikely to be effective on this type of landform as the fresh surface may post‐date the formation of the landform following reoccupation of the moraine rampart by the glacier. This research highlights that the interpretation of geochronological data sets from similar moraine systems should be undertaken with caution. Article in Journal/Newspaper Northern Sweden Wiley Online Library Boreas 46 2 199 211 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Despite a long history of glaciological research, the palaeo‐environmental significance of moraine systems in the Kebnekaise Mountains, Sweden, has remained uncertain. These landforms offer the potential to elucidate glacier response prior to the period of direct monitoring and provide an insight into the ice‐marginal processes operating at polythermal valley glaciers. This study set out to test existing interpretations of Scandinavian ice‐marginal moraines, which invoke ice stagnation, pushing, stacking/dumping and push‐deformation as important moraine forming processes. Moraines at Isfallsglaciären were investigated using ground‐penetrating radar to document the internal structural characteristics of the landform assemblage. Radar surveys revealed a range of substrate composition and reflectors, indicating a debris‐ice interface and bounding surfaces within the moraine. The moraine is demonstrated to contain both ice‐rich and debris‐rich zones, reflecting a complex depositional history and a polygenetic origin. As a consequence of glacier overriding, the morphology of these landforms provides a misleading indicator of glacial history. Traditional geochronological methods are unlikely to be effective on this type of landform as the fresh surface may post‐date the formation of the landform following reoccupation of the moraine rampart by the glacier. This research highlights that the interpretation of geochronological data sets from similar moraine systems should be undertaken with caution. |
author2 |
Seventh Framework Programme |
format |
Article in Journal/Newspaper |
author |
Tonkin, Toby N. Midgley, Nicholas G. Graham, David J. Labadz, Jillian C. |
spellingShingle |
Tonkin, Toby N. Midgley, Nicholas G. Graham, David J. Labadz, Jillian C. Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden |
author_facet |
Tonkin, Toby N. Midgley, Nicholas G. Graham, David J. Labadz, Jillian C. |
author_sort |
Tonkin, Toby N. |
title |
Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden |
title_short |
Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden |
title_full |
Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden |
title_fullStr |
Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden |
title_full_unstemmed |
Internal structure and significance of ice‐marginal moraine in the Kebnekaise Mountains, northern Sweden |
title_sort |
internal structure and significance of ice‐marginal moraine in the kebnekaise mountains, northern sweden |
publisher |
Wiley |
publishDate |
2016 |
url |
http://dx.doi.org/10.1111/bor.12220 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12220 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12220 |
genre |
Northern Sweden |
genre_facet |
Northern Sweden |
op_source |
Boreas volume 46, issue 2, page 199-211 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/bor.12220 |
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Boreas |
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46 |
container_issue |
2 |
container_start_page |
199 |
op_container_end_page |
211 |
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1810466585426526208 |