Geomorphological mapping is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

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 …

Most discharge from large ice sheets takes place through fast-flowing ice streams and their
speed is strongly modulated by interactions between the ice and the underlying sediments …

The geological record of landforms and sediments produced beneath deglaciating ice
sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed …

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 …

Ice sheets flowing across a sedimentary bed usually produce a landscape of blister-like
landforms streamlined in the direction of the ice flow and with each bump of the order of 102 …

This book is a comprehensive overview of the ever-captivating field of glaciation from the
perspective of glacial landsystems. This approach models the many processes, forms and …

Geophysical and geological data indicate that during the last glacial cycle a palaeo-ice
stream drained the Antarctic Peninsula Ice Sheet (APIS) through Marguerite Bay to the edge …

Ice streams influence ice sheet mass balance and stability but key aspects of their behaviour
remain poorly understood. This paper reviews and discusses one very important aspect …