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 …

This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …

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 …

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

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 …

Antarctic geothermal heat flow (GHF) affects the temperature of the ice sheet, determining its
ability to slide and internally deform, as well as the behaviour of the continental crust …

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 …

We present a machine learning approach to statistically derive geothermal heat flow (GHF)
for Antarctica. The adopted approach estimates GHF from multiple geophysical and …

We review the geomorphological, sedimentological and chronological evidence for palaeo-
ice streams on the continental shelf of Antarctica and use this information to investigate …

The geothermal heat flux is a critical thermal boundary condition that influences the melting,
flow, and mass balance of ice sheets, but measurements of this parameter are difficult to …