Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland

Several subglacially formed short flutes show crescentic scours around the boulders at their proximal end and furrows along their sides. The crescentic scours and furrows are partly filled by sorted sand and gravel. and it is suggested here that they were formed by fast flowing, turbulent meltwater...

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Published in:Boreas
Main Author: DREIMANIS, ALEKSIS
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1993
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1993.tb00170.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1993.tb00170.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1993.tb00170.x
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spelling crwiley:10.1111/j.1502-3885.1993.tb00170.x 2024-09-15T18:13:21+00:00 Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland DREIMANIS, ALEKSIS 1993 http://dx.doi.org/10.1111/j.1502-3885.1993.tb00170.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1993.tb00170.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1993.tb00170.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 22, issue 2, page 110-112 ISSN 0300-9483 1502-3885 journal-article 1993 crwiley https://doi.org/10.1111/j.1502-3885.1993.tb00170.x 2024-07-25T04:19:27Z Several subglacially formed short flutes show crescentic scours around the boulders at their proximal end and furrows along their sides. The crescentic scours and furrows are partly filled by sorted sand and gravel. and it is suggested here that they were formed by fast flowing, turbulent meltwater in the subglacial cavity where the flute was formed. Article in Journal/Newspaper Iceland Wiley Online Library Boreas 22 2 110 112
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Several subglacially formed short flutes show crescentic scours around the boulders at their proximal end and furrows along their sides. The crescentic scours and furrows are partly filled by sorted sand and gravel. and it is suggested here that they were formed by fast flowing, turbulent meltwater in the subglacial cavity where the flute was formed.
format Article in Journal/Newspaper
author DREIMANIS, ALEKSIS
spellingShingle DREIMANIS, ALEKSIS
Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland
author_facet DREIMANIS, ALEKSIS
author_sort DREIMANIS, ALEKSIS
title Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland
title_short Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland
title_full Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland
title_fullStr Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland
title_full_unstemmed Water‐eroded crescentic scours and furrows associated with subglacial flutes at Breidamerkurjökull, Iceland
title_sort water‐eroded crescentic scours and furrows associated with subglacial flutes at breidamerkurjökull, iceland
publisher Wiley
publishDate 1993
url http://dx.doi.org/10.1111/j.1502-3885.1993.tb00170.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1993.tb00170.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1993.tb00170.x
genre Iceland
genre_facet Iceland
op_source Boreas
volume 22, issue 2, page 110-112
ISSN 0300-9483 1502-3885
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1502-3885.1993.tb00170.x
container_title Boreas
container_volume 22
container_issue 2
container_start_page 110
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