The Labrador continental shelf (c. 200 km wide) consists of a series of shallow banks and intervening cross-shelf troughs (Fig. 1b). Glacial reconstructions...
In areas where bedrock outcrops are situated between converging glaciers, longitudinal debris accumulations mark the boundary between adjacent ice-flow units....
Elongate glacial landforms are typically orientated in the direction of ice flow (Benn & Evans 2010). They are often preserved in the submarine environment,...
Ice-proximal fans are found where subglacial streams reach the margins of grounded tidewater glaciers. As the streams enter the marine environment, they lose...
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...
Belcher Glacier, a 35 km long tidewater outlet glacier of the 12 000 km2 ice cap on Devon Island (Dowdeswell et al. 2004), is one of the fastest-flowing...
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...
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...
New geophysical techniques (multibeam echo sounding and 3D seismics) have revolutionized high-resolution imaging of the modern seafloor and palaeo-shelf...
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