La déglaciation et le relèvement isostatique sur la côte est de la baie d’Hudson
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...
Published in: | Cahiers de géographie du Québec |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Consortium Erudit
2005
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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 |