Les glissements rétrogressifs de fonte de la rivière Willow, Territoires du Nord-Ouest, Canada: Caractéristiques sédimentologiques, distribution spatiale et temporelle
The Willow River (Richardson Mountains, N.W.T.) drainage basin is located at the western limit reached by the Laurentide ice-sheet during the Last Glacial Maximum (LGM). The icesheet covered the eastern fringe of the Mountains and deposited a lodgment till. The textural maturity and the lithology of...
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Format: | Thesis |
Language: | French |
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Université d'Ottawa / University of Ottawa
2003
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Online Access: | https://dx.doi.org/10.20381/ruor-18187 http://www.ruor.uottawa.ca/handle/10393/26444 |