Évolution postglaciaire de la sédimentation éolienne au sommet de deux parois rocheuses du nord de la Gaspésie, Québec (Canada)
The analysis of two aeolian cliff-top deposits in northern Gaspésie (Québec, Canada) allowed us to trace its postglacial evolution in relation to concomitant environmental changes. The aeolian sediments come from the rock walls below. They are blown up on the summit plateau by the very powerful asce...
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| Format: | Article |
| Language: | English |
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Physio-Géo
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| Series: | Physio-Géo |
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| Online Access: | https://journals.openedition.org/physio-geo/11507 |