Origine, âge et taux d’accrétion verticale de la tourbière à palses de Blanc-Sablon, basse Côte-Nord, Golfe du Saint-Laurent, Québec
The palsa peat bog in the Blanc-Sablon area was formed in a lacustrine basin isolated by a moraine ridge at the head of the Blanc-Sablon River valley when the isostatic land recovery reached the 60-70 m level. At the beginning, the depth of the lake was about 10 m however, the lake was soon drained...
| Published in: | Géographie physique et Quaternaire |
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| Main Authors: | , |
| Format: | Text |
| Language: | French |
| Published: |
Les Presses de l'Université de Montréal
2006
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| Subjects: | |
| Online Access: | https://doi.org/10.7202/016829ar http://id.erudit.org/iderudit/016829ar |