In areas where bedrock outcrops are situated between converging glaciers, longitudinal debris accumulations mark the boundary between adjacent ice-flow units....
The Labrador continental shelf (c. 200 km wide) consists of a series of shallow banks and intervening cross-shelf troughs (Fig. 1b). Glacial reconstructions...
Ice-proximal fans are found where subglacial streams reach the margins of grounded tidewater glaciers. As the streams enter the marine environment, they lose...
Elongate glacial landforms are typically orientated in the direction of ice flow (Benn & Evans 2010). They are often preserved in the submarine environment,...
In the past two decades there have been several advances that make the production of an atlas of submarine glacial landforms timely. First is the development...
Glaciers erode bedrock at all scales, from striations of millimetres in width through to the landscape-scale of U-shaped valleys and fjords. Glacier erosion...
Glacimarine processes affect about 20% of the global ocean today, and this area expanded considerably under cyclical full-glacial conditions during the...
M'Clure Strait in the Canadian Beaufort Sea (Fig. 1) is one of the largest cross-shelf troughs in the High Arctic, with a length of over 1000 km and a maximum...
The Labrador Shelf is characterized by several cross-shelf troughs separated by intervening shallower banks. The troughs were probably occupied by fast-flowing...
Périodique (revue)
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