Submarine sediment failures and related mass-transport deposits (MTDs) are widespread
on the eastern Canadian continental slope settings and in general, have been related to ice …

In the Younger Dryas (YD) the circum-North Atlantic region returned to near glacial
conditions, widely attributed to the release of fresh water from the Laurentide Ice Sheet (LIS) …

Flemish Pass is a small, perched slope basin seaward of the Grand Banks on the eastern
Canadian continental margin. Glacial ice crossed the Grand Banks to reach the upper …

Bonanza Canyon is a complex canyon system on the slope from the intermittently glaciated
Grand Bank on the south side of Orphan Basin. A 3D seismic reflection volume, 2D high …

The eastern Canadian continental margin is a typical glaciated passive margin where
historic earthquakes have triggered submarine landslides. This study compares …

Quaternary deposits in southern Orphan Basin include complex mass transport deposits
(MTD) comprising both glaciogenic debris flows (GDF) and blocky MTD. 3D seismic …

The shallow sedimentary sequence in Flemish Pass, a small perched basin along the north-
eastern Grand Banks margin, was studied for improving the knowledge of timing of …

Several deep-water sectors offshore Newfoundland and Labrador are available for parcel
nomination in the next few years. This paper summarizes the current availability of …

Oil and gas exploration in Eastern Canada has included deep water regions of the Orphan
Basin, St. Pierre slope and Scotian slope. The Geological Survey of Canada, in …

This 2004 ethnographic inquiry, set in the evolving Winfield-Wessex context of French
colonization in Ontario, interrogated the informal and formal pedagogical practices of mother …