Modification of Clasts in Lodgement Tills by Glacial Erosion
Abstract 7.8% of 1 105 clasts with a B-axis diameter of >32 mm in lodgement tills from Skálafellsjökull, south-east Iceland, had a stoss-and-lee form. Clasts deeply embedded in the tills were more likely to have such a form than those resting lightly on the surface. Deeply embedded basalt and...
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Cambridge University Press (CUP)
1982
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Online Access: | http://dx.doi.org/10.1017/s0022143000005062 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005062 |
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crcambridgeupr:10.1017/s0022143000005062 2024-09-09T19:47:20+00:00 Modification of Clasts in Lodgement Tills by Glacial Erosion Sharp, Martin 1982 http://dx.doi.org/10.1017/s0022143000005062 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005062 en eng Cambridge University Press (CUP) Journal of Glaciology volume 28, issue 100, page 475-481 ISSN 0022-1430 1727-5652 journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0022143000005062 2024-06-19T04:03:59Z Abstract 7.8% of 1 105 clasts with a B-axis diameter of >32 mm in lodgement tills from Skálafellsjökull, south-east Iceland, had a stoss-and-lee form. Clasts deeply embedded in the tills were more likely to have such a form than those resting lightly on the surface. Deeply embedded basalt and andesite clasts were also more rounded than lightly embedded clasts of similar lithology, and more striated and more likely to have a stoss-and-lee form than deeply embedded gabbro and granophyre clasts. Lightly embedded basalt and andesite clasts were more striated than lightly embedded gabbro and granophyre clasts. Within each lithological class, larger clasts were more likely to have a stoss-and-lee form. It is suggested that deeply embedded boulders acquire their rounded stoss-and-lee form by abrasion and fracture by over-riding debris-laden ice. This occurs after they have become firmly lodged by ploughing into the subglacial till bed, and before they become buried by lodgement of debris around them. The degree of modification depends in part upon clast size and lithology. The long-axis orientation of deeply embedded boulders is a good indicator of former ice-flow directions. Article in Journal/Newspaper Iceland Journal of Glaciology Cambridge University Press Journal of Glaciology 28 100 475 481 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract 7.8% of 1 105 clasts with a B-axis diameter of >32 mm in lodgement tills from Skálafellsjökull, south-east Iceland, had a stoss-and-lee form. Clasts deeply embedded in the tills were more likely to have such a form than those resting lightly on the surface. Deeply embedded basalt and andesite clasts were also more rounded than lightly embedded clasts of similar lithology, and more striated and more likely to have a stoss-and-lee form than deeply embedded gabbro and granophyre clasts. Lightly embedded basalt and andesite clasts were more striated than lightly embedded gabbro and granophyre clasts. Within each lithological class, larger clasts were more likely to have a stoss-and-lee form. It is suggested that deeply embedded boulders acquire their rounded stoss-and-lee form by abrasion and fracture by over-riding debris-laden ice. This occurs after they have become firmly lodged by ploughing into the subglacial till bed, and before they become buried by lodgement of debris around them. The degree of modification depends in part upon clast size and lithology. The long-axis orientation of deeply embedded boulders is a good indicator of former ice-flow directions. |
format |
Article in Journal/Newspaper |
author |
Sharp, Martin |
spellingShingle |
Sharp, Martin Modification of Clasts in Lodgement Tills by Glacial Erosion |
author_facet |
Sharp, Martin |
author_sort |
Sharp, Martin |
title |
Modification of Clasts in Lodgement Tills by Glacial Erosion |
title_short |
Modification of Clasts in Lodgement Tills by Glacial Erosion |
title_full |
Modification of Clasts in Lodgement Tills by Glacial Erosion |
title_fullStr |
Modification of Clasts in Lodgement Tills by Glacial Erosion |
title_full_unstemmed |
Modification of Clasts in Lodgement Tills by Glacial Erosion |
title_sort |
modification of clasts in lodgement tills by glacial erosion |
publisher |
Cambridge University Press (CUP) |
publishDate |
1982 |
url |
http://dx.doi.org/10.1017/s0022143000005062 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005062 |
genre |
Iceland Journal of Glaciology |
genre_facet |
Iceland Journal of Glaciology |
op_source |
Journal of Glaciology volume 28, issue 100, page 475-481 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000005062 |
container_title |
Journal of Glaciology |
container_volume |
28 |
container_issue |
100 |
container_start_page |
475 |
op_container_end_page |
481 |
_version_ |
1809916801379729408 |