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...
Published in: | Géographie physique et Quaternaire |
---|---|
Main Authors: | , |
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 |