Articles
Where the Great Whale River empties into the Hudson Bay, it is intrenched in the Tyrrel Sea sands (altitude : about 30 m) and in slightly older glacio-marine clays. On the left side of the river, this materials is eaten away by a dozen hemicycles. This morphology has been produced, during the last t...
Published in: | Cahiers de géographie du Québec |
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Format: | Article in Journal/Newspaper |
Language: | French |
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Département de géographie de l'Université Laval
2005
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Online Access: | http://www.erudit.org/fr/revues/cgq/1974-v18-n45-cgq2619/021223ar.pdf https://www.erudit.org/fr/revues/cgq/1974-v18-n45-cgq2619/021223ar.pdf https://id.erudit.org/iderudit/021223ar https://doi.org/10.7202/021223ar https://core.ac.uk/display/59283371 https://www.erudit.org/fr/revues/cgq/1974-v18-n45-cgq2619/021223ar/ https://academic.microsoft.com/#/detail/2131857279 |