An Unusual Ice Formation on the Ottawa River

Abstract An unusual humped formation of floating ice, about 10 m. high, 100 m. wide and 1,200 m. long. was observed on the Ottawa River, Canada. Some characteristics of this formation are described. The cause of the humps was found to be frazil ice deposited in a trench about 90 m. wide, 90 m. deep...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Gold, L. W., Williams, G. P.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1963
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000028100
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028100
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spelling crcambridgeupr:10.1017/s0022143000028100 2024-03-03T08:46:06+00:00 An Unusual Ice Formation on the Ottawa River Gold, L. W. Williams, G. P. 1963 http://dx.doi.org/10.1017/s0022143000028100 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028100 en eng Cambridge University Press (CUP) Journal of Glaciology volume 4, issue 35, page 569-573 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1963 crcambridgeupr https://doi.org/10.1017/s0022143000028100 2024-02-08T08:47:47Z Abstract An unusual humped formation of floating ice, about 10 m. high, 100 m. wide and 1,200 m. long. was observed on the Ottawa River, Canada. Some characteristics of this formation are described. The cause of the humps was found to be frazil ice deposited in a trench about 90 m. wide, 90 m. deep and 1,200 m. long. The frazil ice was formed in rapids up-stream from the humps. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Canada Humps ENVELOPE(-57.450,-57.450,-63.983,-63.983) Journal of Glaciology 4 35 569 573
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Gold, L. W.
Williams, G. P.
An Unusual Ice Formation on the Ottawa River
topic_facet Earth-Surface Processes
description Abstract An unusual humped formation of floating ice, about 10 m. high, 100 m. wide and 1,200 m. long. was observed on the Ottawa River, Canada. Some characteristics of this formation are described. The cause of the humps was found to be frazil ice deposited in a trench about 90 m. wide, 90 m. deep and 1,200 m. long. The frazil ice was formed in rapids up-stream from the humps.
format Article in Journal/Newspaper
author Gold, L. W.
Williams, G. P.
author_facet Gold, L. W.
Williams, G. P.
author_sort Gold, L. W.
title An Unusual Ice Formation on the Ottawa River
title_short An Unusual Ice Formation on the Ottawa River
title_full An Unusual Ice Formation on the Ottawa River
title_fullStr An Unusual Ice Formation on the Ottawa River
title_full_unstemmed An Unusual Ice Formation on the Ottawa River
title_sort unusual ice formation on the ottawa river
publisher Cambridge University Press (CUP)
publishDate 1963
url http://dx.doi.org/10.1017/s0022143000028100
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028100
long_lat ENVELOPE(-57.450,-57.450,-63.983,-63.983)
geographic Canada
Humps
geographic_facet Canada
Humps
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 4, issue 35, page 569-573
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000028100
container_title Journal of Glaciology
container_volume 4
container_issue 35
container_start_page 569
op_container_end_page 573
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