Z jaką dynamiką lodu należy wiązać formy szczelinowe?
The paper presents discussion on crevasse fillings – one of a group of glacial forms whose formation is assigned by various authors to two peripheral dynamics of ice-sheet masses: stagnant ice and surging glaciers. Examples from literature of crevasse filling formation in these two states of dynamic...
Published in: | Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia |
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Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
2015
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Online Access: | https://doi.org/10.17951/b.2015.70.2.27 https://bibliotekanauki.pl/articles/763164.pdf https://bibliotekanauki.pl/articles/763164 |
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fttriple:oai:gotriple.eu:oai:bibliotekanauki.pl:763164 2023-05-15T16:40:40+02:00 Z jaką dynamiką lodu należy wiązać formy szczelinowe? Which ice dynamics should be attached to slit forms? Godlewska, Anna 2015-01-01 https://doi.org/10.17951/b.2015.70.2.27 https://bibliotekanauki.pl/articles/763164.pdf https://bibliotekanauki.pl/articles/763164 pl pol Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej doi:10.17951/b.2015.70.2.27 https://bibliotekanauki.pl/articles/763164.pdf https://bibliotekanauki.pl/articles/763164 lic_creative-commons Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; 2015, 70, 2 0137-1983 geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.17951/b.2015.70.2.27 2023-01-22T18:24:27Z The paper presents discussion on crevasse fillings – one of a group of glacial forms whose formation is assigned by various authors to two peripheral dynamics of ice-sheet masses: stagnant ice and surging glaciers. Examples from literature of crevasse filling formation in these two states of dynamics are presented. The author makes an overview of documented in the literature examples of crevasse fillings forming in stagnant surging ice and discuss the differences between the group formed in stagnant and the group formed in surging ice. In the conclusion, the author proposes – at the background of references – assigning crevasse fillings to the surge dynamics of ice masses whereas glacial forms, which develop in stagnant ice crevasses, should not be termed crevasse fillings, but interpreted e.g. as kames, eskers, hummocky moraines. The paper presents discussion on crevasse fillings – one of a group of glacial forms which formation is assigned by various authors to two peripheral dynamics of ice-sheet masses: stagnant ice and surging glaciers. Examples from literature of crevasse filling formation in these two states of dynamics are presented. The author makes an overview of documented in the literature examples of crevasse fillings forming in stagnant surging ice and discuss the differences between the group formed in stagnant and the group formed in surging ice. In the conclusion, the author proposes – at the background of references – assigning crevasse fillings to the surge dynamics of ice masses whereas glacial forms, which develop in stagnant ice crevasses, should not be termed crevasse fillings, but interpreted e.g. as kames, eskers, hummocky moraines. Article in Journal/Newspaper Ice Sheet Unknown Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 70 2 27 |
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Polish |
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geo envir |
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geo envir Godlewska, Anna Z jaką dynamiką lodu należy wiązać formy szczelinowe? |
topic_facet |
geo envir |
description |
The paper presents discussion on crevasse fillings – one of a group of glacial forms whose formation is assigned by various authors to two peripheral dynamics of ice-sheet masses: stagnant ice and surging glaciers. Examples from literature of crevasse filling formation in these two states of dynamics are presented. The author makes an overview of documented in the literature examples of crevasse fillings forming in stagnant surging ice and discuss the differences between the group formed in stagnant and the group formed in surging ice. In the conclusion, the author proposes – at the background of references – assigning crevasse fillings to the surge dynamics of ice masses whereas glacial forms, which develop in stagnant ice crevasses, should not be termed crevasse fillings, but interpreted e.g. as kames, eskers, hummocky moraines. The paper presents discussion on crevasse fillings – one of a group of glacial forms which formation is assigned by various authors to two peripheral dynamics of ice-sheet masses: stagnant ice and surging glaciers. Examples from literature of crevasse filling formation in these two states of dynamics are presented. The author makes an overview of documented in the literature examples of crevasse fillings forming in stagnant surging ice and discuss the differences between the group formed in stagnant and the group formed in surging ice. In the conclusion, the author proposes – at the background of references – assigning crevasse fillings to the surge dynamics of ice masses whereas glacial forms, which develop in stagnant ice crevasses, should not be termed crevasse fillings, but interpreted e.g. as kames, eskers, hummocky moraines. |
format |
Article in Journal/Newspaper |
author |
Godlewska, Anna |
author_facet |
Godlewska, Anna |
author_sort |
Godlewska, Anna |
title |
Z jaką dynamiką lodu należy wiązać formy szczelinowe? |
title_short |
Z jaką dynamiką lodu należy wiązać formy szczelinowe? |
title_full |
Z jaką dynamiką lodu należy wiązać formy szczelinowe? |
title_fullStr |
Z jaką dynamiką lodu należy wiązać formy szczelinowe? |
title_full_unstemmed |
Z jaką dynamiką lodu należy wiązać formy szczelinowe? |
title_sort |
z jaką dynamiką lodu należy wiązać formy szczelinowe? |
publisher |
Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej |
publishDate |
2015 |
url |
https://doi.org/10.17951/b.2015.70.2.27 https://bibliotekanauki.pl/articles/763164.pdf https://bibliotekanauki.pl/articles/763164 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; 2015, 70, 2 0137-1983 |
op_relation |
doi:10.17951/b.2015.70.2.27 https://bibliotekanauki.pl/articles/763164.pdf https://bibliotekanauki.pl/articles/763164 |
op_rights |
lic_creative-commons |
op_doi |
https://doi.org/10.17951/b.2015.70.2.27 |
container_title |
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia |
container_volume |
70 |
container_issue |
2 |
container_start_page |
27 |
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1766031074870165504 |