This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new map** inventory that includes previously hypothesised ice …

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

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

The new Second Edition of Glacial Geology provides a modern, comprehensive summary of
glacial geology and geomorphology. It is has been thoroughly revised and updated from the …

Morphological interpretation of regional and detailed bathymetric data sets on the 2500-km-
long Norwegian shelf from the North Sea (57° N) to Svalbard (80° N) has revealed a …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …

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 …

Marine-based ice streams whose beds deepen inland are thought to be inherently
unstable,,. This instability is of particular concern because significant portions of the marine …

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 …

Studying the history of ice-sheet behaviour in the Ross Sea, Antarctica's largest drainage
basin can improve our understanding of patterns and controls on marine-based ice-sheet …