Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland
Abstract The paper uses a case study in Scotland to examine the amount and processes of landscape modification by Quaternary ice sheets. There is an inverse correlation between the distribution of landforms of glacial erosion and pre‐glacial landscape remnants in northeast Scotland. The implication...
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crwiley:10.1002/esp.3290120510 2024-09-15T18:12:23+00:00 Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland Hall, Adrian M. Sugden, David E. 1987 http://dx.doi.org/10.1002/esp.3290120510 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290120510 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290120510 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Earth Surface Processes and Landforms volume 12, issue 5, page 531-542 ISSN 0197-9337 1096-9837 journal-article 1987 crwiley https://doi.org/10.1002/esp.3290120510 2024-07-25T04:20:36Z Abstract The paper uses a case study in Scotland to examine the amount and processes of landscape modification by Quaternary ice sheets. There is an inverse correlation between the distribution of landforms of glacial erosion and pre‐glacial landscape remnants in northeast Scotland. The implication is that in places ice sheets can preserve a pre‐glacial landscape unscathed, while elsewhere they remove the pre‐glacial weathered rock. The location of glacial protection or erosion is strongly influenced by the topography and its influence on former ice sheet flow and basal thermal regime. The classic glacially eroded landscape of areal scouring can be produced by the removal of only 10–50 m of weathered rock. Furthermore rock basins, often regarded as the hallmark of glacial erosion, may be directly inherited from the pre‐glacial pattern of deep weathering. Article in Journal/Newspaper Ice Sheet Wiley Online Library Earth Surface Processes and Landforms 12 5 531 542 |
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Wiley Online Library |
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crwiley |
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English |
description |
Abstract The paper uses a case study in Scotland to examine the amount and processes of landscape modification by Quaternary ice sheets. There is an inverse correlation between the distribution of landforms of glacial erosion and pre‐glacial landscape remnants in northeast Scotland. The implication is that in places ice sheets can preserve a pre‐glacial landscape unscathed, while elsewhere they remove the pre‐glacial weathered rock. The location of glacial protection or erosion is strongly influenced by the topography and its influence on former ice sheet flow and basal thermal regime. The classic glacially eroded landscape of areal scouring can be produced by the removal of only 10–50 m of weathered rock. Furthermore rock basins, often regarded as the hallmark of glacial erosion, may be directly inherited from the pre‐glacial pattern of deep weathering. |
format |
Article in Journal/Newspaper |
author |
Hall, Adrian M. Sugden, David E. |
spellingShingle |
Hall, Adrian M. Sugden, David E. Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland |
author_facet |
Hall, Adrian M. Sugden, David E. |
author_sort |
Hall, Adrian M. |
title |
Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland |
title_short |
Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland |
title_full |
Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland |
title_fullStr |
Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland |
title_full_unstemmed |
Limited modification of mid‐latitude landscapes by ice sheets: The case of northeast Scotland |
title_sort |
limited modification of mid‐latitude landscapes by ice sheets: the case of northeast scotland |
publisher |
Wiley |
publishDate |
1987 |
url |
http://dx.doi.org/10.1002/esp.3290120510 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290120510 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290120510 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Earth Surface Processes and Landforms volume 12, issue 5, page 531-542 ISSN 0197-9337 1096-9837 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/esp.3290120510 |
container_title |
Earth Surface Processes and Landforms |
container_volume |
12 |
container_issue |
5 |
container_start_page |
531 |
op_container_end_page |
542 |
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1810449971266191360 |