Abstract Bedforms of Thwaites Glacier, West Antarctica both record and affect ice flow, as
shown by geophysical data and simple models. Thwaites Glacier flows across the tectonic …

Exhaustive sedimentological analysis of freshly exposed subglacial surfaces and moraines
in southern Iceland provides diagnostic sedimentological signatures of: a) debris transport …

Initially a matter of intellectual curiosity, but now important for understanding ice‐sheet
dynamics, the formation of subglacial bedforms has been a subject of scientific enquiry for …

Scientific progress does not take place in a linear fashion, but often occurs through sudden
advances following years of stagnation, in the course of which quite heated battles between …

A contemporary trend in glacial geomorphology is the quest for a unifying theory of drumlin
and ribbed moraine formation. Three Swedish example areas of each are here newly …

The drumlin field at the surge‐type glacier, Múlajökull, provides an unusual opportunity to
build a model of drumlin formation based on field observations in a modern drumlin‐forming …

Flutes are flow-parallel till ridges that form subglacially and are conspicuous geomorphic
indicators of slip at glacier beds. Flutes commonly have a boulder at their head, lodged in …

Ice‐sheets flowing over soft sediments produce undulations in the bed, typically of metres in
relief, of which drumlins are the most abundant and widely investigated. Consensus …

Drumlins are landforms essential to understanding of ice sheet movement over soft beds,
sediment transport along the ice/bed interface, and the formation of a wide range of glacial …

The study of glacial landforms is important for understanding past subglacial processes and
dynamics. The Nordenskiöldbreen forefield hosts numerous streamlined landforms resulting …