The climate variability of the last deglaciation is often linked to meltwater discharges from the melting of large ice sheets. One of the best examples comes...
Glacial Lake Ojibway occupied large areas in northeastern Ontario and northwestern Quebec during the last deglaciation. Paleogeographic reconstructions depict...
Physical evidence for the drainage of glacial lakes remains relatively rare in depositional records, giving rise to much debate on the location of outlets and...
Lake Ojibway developed at the southern Laurentide Ice Sheet margin during the last deglaciation and covered vast expanses of northeastern Ontario and...
Outcrops bearing stained, striated facets indicative of north-northeastward moving ice, truncated by unstained, striated facets indicative of various younger...
Field mapping and sampling of glacial and glaciolacustrine sediments undertaken in 2007 in National Topographic System (NTS) 42H and in part of 32E was...
The Glacial Map of Canada shows an enigmatic ice-flow anomaly (Area A) covering about 10 000 km2 in the Hearst/Kapuskasing area of northern Ontario which...
Deglaciation of the James Bay region was highly dynamic, with the occurrence of ice (Cochrane) readvances into glacial Lake Ojibway around final deglaciation...