Forms at the Base of Till Strata as Indicators of Ice Movement
Abstract The direction of inland ice movement can, in some cases, be reconstructed by a study of the forms at the base of till strata. These forms are “ribs”, which are formed either as slickensides or as a type of negative “flute”; “edges” and “wedges”, which are caused by shearing movements at the...
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Language: | English |
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Cambridge University Press (CUP)
1979
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Online Access: | http://dx.doi.org/10.1017/s0022143000014325 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014325 |
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crcambridgeupr:10.1017/s0022143000014325 2024-09-15T18:15:38+00:00 Forms at the Base of Till Strata as Indicators of Ice Movement Ehlers, J. Stephan, H.-J. 1979 http://dx.doi.org/10.1017/s0022143000014325 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014325 en eng Cambridge University Press (CUP) Journal of Glaciology volume 22, issue 87, page 345-355 ISSN 0022-1430 1727-5652 journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000014325 2024-08-28T04:03:21Z Abstract The direction of inland ice movement can, in some cases, be reconstructed by a study of the forms at the base of till strata. These forms are “ribs”, which are formed either as slickensides or as a type of negative “flute”; “edges” and “wedges”, which are caused by shearing movements at the base of the ice; or “undulations”, probably created by restricting movements at the base of the ice. These forms appear to be elongated in the direction of ice movement. As these features can easily be measured, they can be used to check, supplement, or replace the results of till-fabric measurements. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 22 87 345 355 |
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Open Polar |
collection |
Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract The direction of inland ice movement can, in some cases, be reconstructed by a study of the forms at the base of till strata. These forms are “ribs”, which are formed either as slickensides or as a type of negative “flute”; “edges” and “wedges”, which are caused by shearing movements at the base of the ice; or “undulations”, probably created by restricting movements at the base of the ice. These forms appear to be elongated in the direction of ice movement. As these features can easily be measured, they can be used to check, supplement, or replace the results of till-fabric measurements. |
format |
Article in Journal/Newspaper |
author |
Ehlers, J. Stephan, H.-J. |
spellingShingle |
Ehlers, J. Stephan, H.-J. Forms at the Base of Till Strata as Indicators of Ice Movement |
author_facet |
Ehlers, J. Stephan, H.-J. |
author_sort |
Ehlers, J. |
title |
Forms at the Base of Till Strata as Indicators of Ice Movement |
title_short |
Forms at the Base of Till Strata as Indicators of Ice Movement |
title_full |
Forms at the Base of Till Strata as Indicators of Ice Movement |
title_fullStr |
Forms at the Base of Till Strata as Indicators of Ice Movement |
title_full_unstemmed |
Forms at the Base of Till Strata as Indicators of Ice Movement |
title_sort |
forms at the base of till strata as indicators of ice movement |
publisher |
Cambridge University Press (CUP) |
publishDate |
1979 |
url |
http://dx.doi.org/10.1017/s0022143000014325 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014325 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 22, issue 87, page 345-355 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000014325 |
container_title |
Journal of Glaciology |
container_volume |
22 |
container_issue |
87 |
container_start_page |
345 |
op_container_end_page |
355 |
_version_ |
1810453508098359296 |