Holocene Environmental Change in the Frobisher Bay Area, Baffin Island, N.W.T.: Deglaciation, Emergence, and the Sequence of Vegetation and Climate

The late-glacial and Holocene paleoenvironmental sequence for the Frobisher Bay area is outlined using glacial, sea level, and palynological evidence. A rapid retreat of ice from the late Foxe glacial maximum in the lower part of the bay after 11,000 BP was followed by a series of stillstands or min...

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Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Authors: Jacobs, J. D., Mode, W. N., Squires, C. A., Miller, G. H.
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1985
Subjects:
Online Access:http://id.erudit.org/iderudit/032599ar
https://doi.org/10.7202/032599ar