Les formes et dépôts nivéo-éoliens actuels en Antarctique et au Nouveau-Québec
In Antarctica, McMurdo region, Victoria Valley, niveo-eolian deposits, made of alternating layers of wind driven snow and sand, 0-2 m thick, are perennial. Together with sandy glaciers, they perhaps have some kinship with the layered deposits discovered by Mariner 9 in the south polar region of Mars...
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/1972-v16-n39-cgq2613/021079ar.pdf https://www.erudit.org/fr/revues/cgq/1972-v16-n39-cgq2613/021079ar.pdf https://doi.org/10.7202/021079ar https://core.ac.uk/display/59282647 https://www.erudit.org/fr/revues/cgq/1972-v16-n39-cgq2613/021079ar/ https://www.erudit.org/revue/cgq/1972/v16/n39/021079ar.html?vue=resume http://id.erudit.org/iderudit/021079ar https://academic.microsoft.com/#/detail/2132369840 https://id.erudit.org/iderudit/021079ar |