Late Wisconsinan deglaciation and glacial lake development in the Appalachians of southeastern Québec

Late Wisconsinan deglaciation in southeastern Québec was preceded by a northward ice-flow reversal that was recorded in the northeastern part of the region. The reversal event was generated by flow convergence toward the St. Lawrence Ice Stream, a northeastward-flowing ice stream which formed in the...

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Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Authors: Parent, Michel, Occhietti, Serge
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1999
Subjects:
Online Access:http://id.erudit.org/iderudit/004859ar
https://doi.org/10.7202/004859ar