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 …

Investigation of drumlins is significant to both glaciology and palaeoglaciology but the sheer
diversity of their composition and internal structure is often cited as a major obstacle towards …

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 …

Subglacially-produced drift lineations provide spatially extensive evidence of ice flow that
can be used to aid reconstructions of the evolution of former ice sheets. Such …

Clast-supported boulder gravel in outwash-fans along the glacial-maximum margin of the
Laurentide Ice Sheet in Wisconsin indicates the occurrence of outburst floods. These …

Recent marginal retreat of Múlajökull, a surge-type outlet glacier of Hofsjökull, Iceland, has
revealed a drumlin field consisting of more than 50 drumlins. The drumlins are 90–320 m …

Surging glaciers are potential analogues for land-terminating palaeo-ice streams and
surging ice sheet lobes, and research on surge-type glaciers is important for understanding …

Despite their importance in understanding glaciological processes and constraining large-
scale flow patterns in palaeo-glaciology, there is little consensus as to how drumlins are …

Glacially induced flow naturally tends to thin and extended till cover through shock
formation, even in the absence of longitudinal gradients in the applied stress. Thicker till …

Subglacial bedforms are a range of landforms (10-105m long) shaped mostly in glacial
sediments and are abundant on ice-sheet beds. Numerous explanations for their …