Grounding-zone wedges (GZWs) are asymmetric sedimentary depocentres which form
through the rapid accumulation of glacigenic debris along a line-source at the grounding …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

In this paper, regional and high-resolution bathymetric data are used to reconstruct the
pattern and dynamics of ice-sheet flow in the fjord and shelf areas of northern Norway …

The rate of deglacial ice-sheet retreat across polar continental shelves, and possible ice-
stream collapse and sea-level rise, has been much debated. High-resolution imagery of …

Mega‐scale glacial lineations (MSGLs) are a characteristic landform on ice stream beds.
Solving the puzzle of their formation is key to understanding how ice interacts with its bed …

Grounding-zone wedges form where halts of decades to centuries during ice-sheet retreat
across polar shelves allow sediment buildup at the grounding zone through delivery of …

The Amundsen Sea continental shelf is one of the most remote areas of coastal Antarctica
and was relatively unexplored until the late 1980s. Over the last two decades, increased …

Glacimarine processes affect about 20% of the global ocean today, and this area expanded
considerably under cyclical full-glacial conditions during the Quaternary (Fig. 1)(Dowdeswell …

High‐resolution bathymetric map** of the fjords and continental shelf around the Svalbard
archipelago shows an extensive pattern of large‐and medium‐scale submarine landforms …

U-series age patterns obtained on reef framework–forming cold-water corals collected over
a nearly 6000-km-long continental margin sector, extending from off Mauritania (17° N; …