What sort of ice dynamics are crevasse fillings connected with? – research overview
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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www.wydawnictwo.umcs.lublin.pl
2016
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Online Access: | https://journals.umcs.pl/b/article/view/1324 https://doi.org/10.17951/b.2015.70.2.27 |
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ftmcsunivojs:oai:ojs.umcsd.home.net.pl:article/1324 2023-05-15T16:40:26+02:00 What sort of ice dynamics are crevasse fillings connected with? – research overview Z jaką dynamiką lodu należy wiązać formy szczelinowe? Godlewska, Anna Praca została sfinansowana ze środków przyznanych w ramach Badań Statutowych „Młoda Kadra i Doktoranci” Wydziału Nauk o Ziemi i Gospodarki Przestrzennej Uniwersytetu Marii Curie-Skłodowskiej w Lublinie. 2016-07-07 application/pdf https://journals.umcs.pl/b/article/view/1324 https://doi.org/10.17951/b.2015.70.2.27 pol pol www.wydawnictwo.umcs.lublin.pl https://journals.umcs.pl/b/article/view/1324/2791 https://journals.umcs.pl/b/article/view/1324 doi:10.17951/b.2015.70.2.27 Prawa autorskie (c) 2016 Anna Godlewska http://creativecommons.org/licenses/by/4.0 CC-BY Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; Vol 70, No 2 (2015); 27 0137-1983 crevasse fillings ice crevasse stagnant ice surging ice glacier/ice-sheet formy szczelinowe szczelina lodowa lód stagnujący lód szarżujący lodowiec/lądolód info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftmcsunivojs https://doi.org/10.17951/b.2015.70.2.27 2020-03-17T13:06:54Z 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 University of Maria Curie-Skłodowska (UMCS): Scientific e-Journals Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 70 2 27 |
institution |
Open Polar |
collection |
University of Maria Curie-Skłodowska (UMCS): Scientific e-Journals |
op_collection_id |
ftmcsunivojs |
language |
Polish |
topic |
crevasse fillings ice crevasse stagnant ice surging ice glacier/ice-sheet formy szczelinowe szczelina lodowa lód stagnujący lód szarżujący lodowiec/lądolód |
spellingShingle |
crevasse fillings ice crevasse stagnant ice surging ice glacier/ice-sheet formy szczelinowe szczelina lodowa lód stagnujący lód szarżujący lodowiec/lądolód Godlewska, Anna What sort of ice dynamics are crevasse fillings connected with? – research overview |
topic_facet |
crevasse fillings ice crevasse stagnant ice surging ice glacier/ice-sheet formy szczelinowe szczelina lodowa lód stagnujący lód szarżujący lodowiec/lądolód |
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. |
author2 |
Praca została sfinansowana ze środków przyznanych w ramach Badań Statutowych „Młoda Kadra i Doktoranci” Wydziału Nauk o Ziemi i Gospodarki Przestrzennej Uniwersytetu Marii Curie-Skłodowskiej w Lublinie. |
format |
Article in Journal/Newspaper |
author |
Godlewska, Anna |
author_facet |
Godlewska, Anna |
author_sort |
Godlewska, Anna |
title |
What sort of ice dynamics are crevasse fillings connected with? – research overview |
title_short |
What sort of ice dynamics are crevasse fillings connected with? – research overview |
title_full |
What sort of ice dynamics are crevasse fillings connected with? – research overview |
title_fullStr |
What sort of ice dynamics are crevasse fillings connected with? – research overview |
title_full_unstemmed |
What sort of ice dynamics are crevasse fillings connected with? – research overview |
title_sort |
what sort of ice dynamics are crevasse fillings connected with? – research overview |
publisher |
www.wydawnictwo.umcs.lublin.pl |
publishDate |
2016 |
url |
https://journals.umcs.pl/b/article/view/1324 https://doi.org/10.17951/b.2015.70.2.27 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; Vol 70, No 2 (2015); 27 0137-1983 |
op_relation |
https://journals.umcs.pl/b/article/view/1324/2791 https://journals.umcs.pl/b/article/view/1324 doi:10.17951/b.2015.70.2.27 |
op_rights |
Prawa autorskie (c) 2016 Anna Godlewska http://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
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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1766030840988434432 |