La déglaciation et le relèvement isostatique sur la côte est de la baie d’Hudson

• Published in: Cahiers de géographie du Québec
• Main Author: Claude Hillaire-Marcel
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Consortium Erudit 2005
• Subjects: Sciences Humaines et Sociales; Social Sciences and Humanities; Quaternaire; géomorphologie; déglaciation; relèvement isostatique Nouveau-Québec; Baie d'Hudson (côte est); Quaternary; geomorphology; isosatic uplift; Nouveau-Québec; Hudson Bay (eastern coast); geo; envir; Hudson Bay; Hudson; Baleine; la Baleine; Baie d'Hudson; Baie-d'Hudson; Tyrrell; Poste-de-la-Baleine; Manitounuk Sound; Great Whale River
• Online Access: http://www.erudit.org/fr/revues/cgq/1976-v20-n50-cgq2624/021319ar.pdf; https://www.erudit.org/fr/revues/cgq/1976-v20-n50-cgq2624/021319ar.pdf; https://doi.org/10.7202/021319ar; https://www.erudit.org/fr/revues/cgq/1976-v20-n50-cgq2624/021319ar/; https://core.ac.uk/display/59283743; https://www.erudit.org/revue/cgq/1976/v20/n50/021319ar.html?vue=resume; http://id.erudit.org/iderudit/021319ar; https://academic.microsoft.com/#/detail/2118283414; https://id.erudit.org/iderudit/021319ar

On the eastern coast of Hudson Bay, in the area between Great-Whale-River and the Richmond Gulf, the last wisconsinian ices flowed westward. The deglaciation took place between 8.100 l*C yr BP (Great-Whale-River) and 7.600 1 4 C yr BP (Richmond Gulf). The maximum limit of the Tyrrell Sea rises towar...