La déglaciation de la région de Rimouski, Bas-Saint-Laurent (Québec) : indices d’une récurrence glaciaire dans la Mer de Goldthwait entre 12 400 et 12 000 BP
The spatial distribution of land- forms associated with the deglaciation of the Rimouski area (outwash deltas, eskers, kames, and ice disintegration features) was analysed in relation to the morphostructural framework. The main physiographic elements are NE-SW ridges and depressions parallel to the...
| Published in: | Géographie physique et Quaternaire |
|---|---|
| Main Author: | |
| Format: | Text |
| Language: | French |
| Published: |
Les Presses de l'Université de Montréal
1998
|
| Subjects: | |
| Online Access: | http://id.erudit.org/iderudit/004832ar https://doi.org/10.7202/004832ar |