Surficial geology mapping of the Beaver Mines area, distribution of Canadian Shield erratics, stratigraphy of Quaternary sediments exposed along the Castle...
Silty carbonate till derived from erosion of Paleozoic carbonate and Proterozoic rocks within and adjacent to Hudson Bay covers extensive areas of the Canadian...
Landslide-damming of Silver Lake in the Cascade Mountains took place about 1000BP. Delta growth favoured the faulted west valley side. At the commencement of...
In southwestern Alberta, Canada, a westward-rising last-glacial-maximum continental ice limit has been identified. This limit is defined by the upper elevation...
Fossil records from sites overridden by or adjacent to the Laurentide Ice Sheet indicate that the climate of the last interglaciation (Oxygen-Isotope Substage...
Study of ice-movement indicators in the Darby Lake (NTS 56 N) and Arrowsmith River (NTS 56-O/9-16) map areas revealed a complex ice-flow history involving four...
Preliminary investigation of ice-flow directions in the Arrowsmith River map area in the Committee Bay area of Nunavut, indicates that ice moved in four...