Satellite images provide unique means of identifying large-scale flow-generated lineations
produced by former ice sheets. They can be interpreted to reconstruct the major elements …

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 …

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 …

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 …

The third edition of this successful textbook will supply advanced undergraduate and
graduate students with the tools they need to understand modern glaciological research …

The areal extents of the Laurentide and Fennoscandian ice sheets during the Last Glacial
Maximum (about 20,000 years ago) are well known, but thickness estimates range widely …

This paper examines ice-sheet wide variations in subglacial thermal regime and ice
dynamics using the landform record exposed on the beds of former mid-latitude ice sheets …

The last glacial maximum (LGM) outline and subsequent retreat pattern (21–7kyr) of North
American ice sheets are reasonably well established. However, the evolution of the ice …

It has long been recognised that the formerly glaciated area of Fennoscandia shows large
spatial differences in thicknesses of Quaternary deposits (mainly tills), and exhibits distinct …

Understanding the evolution of the ice-bed interface is fundamentally important for gaining
insight into the dynamics of ice masses and how subglacial landforms are created. However …