Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion
Abstract Clasts modified by glacial erosion are described from lodgement tills in front of the glacier Mýrdalsjökull, south Iceland. Many clasts show modification of their lower surfaces in the same way as their upper ones. However, the lower surfaces have a smoothed down-glacier face and a truncate...
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Cambridge University Press (CUP)
1984
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Online Access: | http://dx.doi.org/10.1017/s0022143000006006 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006006 |
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crcambridgeupr:10.1017/s0022143000006006 2024-09-15T18:07:49+00:00 Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion Krüger, Johannes 1984 http://dx.doi.org/10.1017/s0022143000006006 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006006 en eng Cambridge University Press (CUP) Journal of Glaciology volume 30, issue 105, page 241-243 ISSN 0022-1430 1727-5652 journal-article 1984 crcambridgeupr https://doi.org/10.1017/s0022143000006006 2024-08-28T04:03:10Z Abstract Clasts modified by glacial erosion are described from lodgement tills in front of the glacier Mýrdalsjökull, south Iceland. Many clasts show modification of their lower surfaces in the same way as their upper ones. However, the lower surfaces have a smoothed down-glacier face and a truncated up-glacier face, which is the opposite orientation to that of the upper surfaces. This so-called double stoss-lee form is interpreted as a response to basal transport over abrading materials, following deposition of the clast and succeeded by glacial erosion. It is suggested that clasts with a double stoss-lee form are a diagnostic criterion for subglacial deposition by lodgement. Furthermore, the distribution and orientation of clasts with a stoss-lee form was investigated on a ground-moraine surface. 17.3% of 2199 clasts with an a -axis diameter > 30 cm had a stoss-lee form. The proportion of clasts with their smoothed ends facing up-glacier within ± 22.5° of the ice-flow direction was 72.7%. Thus, the preferred stoss-side orientation is closely related to the ice movement and indicates the direction from which the ice came. Only 11.7% of boulders with a divergent stoss-side orientation are located in connection with annual moraines. It is suggested that such boulders have mainly been re-deposited beneath the ice and not at the ice front by minor advances of the glacier. Article in Journal/Newspaper glacier Iceland Journal of Glaciology Mýrdalsjökull Cambridge University Press Journal of Glaciology 30 105 241 243 |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Clasts modified by glacial erosion are described from lodgement tills in front of the glacier Mýrdalsjökull, south Iceland. Many clasts show modification of their lower surfaces in the same way as their upper ones. However, the lower surfaces have a smoothed down-glacier face and a truncated up-glacier face, which is the opposite orientation to that of the upper surfaces. This so-called double stoss-lee form is interpreted as a response to basal transport over abrading materials, following deposition of the clast and succeeded by glacial erosion. It is suggested that clasts with a double stoss-lee form are a diagnostic criterion for subglacial deposition by lodgement. Furthermore, the distribution and orientation of clasts with a stoss-lee form was investigated on a ground-moraine surface. 17.3% of 2199 clasts with an a -axis diameter > 30 cm had a stoss-lee form. The proportion of clasts with their smoothed ends facing up-glacier within ± 22.5° of the ice-flow direction was 72.7%. Thus, the preferred stoss-side orientation is closely related to the ice movement and indicates the direction from which the ice came. Only 11.7% of boulders with a divergent stoss-side orientation are located in connection with annual moraines. It is suggested that such boulders have mainly been re-deposited beneath the ice and not at the ice front by minor advances of the glacier. |
format |
Article in Journal/Newspaper |
author |
Krüger, Johannes |
spellingShingle |
Krüger, Johannes Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion |
author_facet |
Krüger, Johannes |
author_sort |
Krüger, Johannes |
title |
Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion |
title_short |
Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion |
title_full |
Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion |
title_fullStr |
Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion |
title_full_unstemmed |
Clasts with Stoss-Lee Form in Lodgement Tills: A Discussion |
title_sort |
clasts with stoss-lee form in lodgement tills: a discussion |
publisher |
Cambridge University Press (CUP) |
publishDate |
1984 |
url |
http://dx.doi.org/10.1017/s0022143000006006 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006006 |
genre |
glacier Iceland Journal of Glaciology Mýrdalsjökull |
genre_facet |
glacier Iceland Journal of Glaciology Mýrdalsjökull |
op_source |
Journal of Glaciology volume 30, issue 105, page 241-243 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000006006 |
container_title |
Journal of Glaciology |
container_volume |
30 |
container_issue |
105 |
container_start_page |
241 |
op_container_end_page |
243 |
_version_ |
1810445177476612096 |