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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...

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Bibliographic Details
Published in:Cahiers de géographie du Québec
Main Author: Jean Demangeot
Format: Article in Journal/Newspaper
Language:French
Published: Département de géographie de l'Université Laval 2005
Subjects:
Sciences Humaines et Sociales
Social Sciences and Humanities
Glissements de terrain
gélifluxion
thermokarst
foirage
nivation
permafrost
Poste-de-la-Baleine
Nouveau-Québec
Landslides
Solifluxion
Flowage
Great Whale
New Québec
geo
envir
Hudson Bay
Hudson
La Grande Rivière
Baleine
la Baleine
Gauche
Grande rivière de la Baleine
Grande Rivière de la Baleine
Great Whale River
Thermokarst
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

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