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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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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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 |
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Open Polar |
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Wiley Online Library |
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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 |
op_container_end_page |
112 |
_version_ |
1810451105089323008 |