Glacial and Sea Level History of Lowther and Griffith Islands, Northwest Territories: A Hint of Tectonics
Lowther and Griffith islands, in the centre of Parry Channel, were overrun by the Laurentide Ice Sheet early in the last glaciation. Northeastward Laurentide ice flow persisted across at least Lowther Island until early Holocene déglaciation. Well constrained postglacial emergence curves for the isl...
Published in: | Géographie physique et Quaternaire |
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Format: | Text |
Language: | English |
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Les Presses de l'Université de Montréal
1993
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Online Access: | http://id.erudit.org/iderudit/032944ar https://doi.org/10.7202/032944ar |