Patterns of glacial erosion and deposition around Cumberland Sound, Frobisher Bay and Hudson Strait, and the location of ice streams in the eastern Canadian Arctic in Models in geomorphology.
Multiple deglaciations of the Hudson Bay Lowlands, Canada, since deposition ot the Missinaibi (Last-Interglacial?) Formation
Aminostratigraphie ; Baie d'Hudson ; Canada ; Datation amino-acides ; Déglaciation ; Glaciation ; Géographie de l'Amérique ; Inlandsis Laurentien ; Interstade ; Pléistocène supérieur ; Quaternaire zones froides
intermediate in age between the last interglaciation and the incursion of the Tyrrell Sea 8000 yr ago. Between these two interglacial marine inundations, Hudson Bay is predicted to have been free of ice along its southern shore about 35,000, 75,000, and 105,000
In the Hudson Bay/James Bay Lowlands, along the coasts of Banks Island, and along the eastern coast of Baffin Island continuous and extensive sections in Quaternary sediments are rich in marine fossils, buried peats and soils and contain a wide