Glaciers and ice sheets erode mountains and produce vast quantities of sediments that are
delivered to rivers and oceans, impacting global sediment and biogeochemical balances …

Glacier-erosion rates range across orders of magnitude, and much of this variation cannot
be attributed to basal sliding rates. Subglacial till acts as lubricating 'fault gouge'or 'sawdust' …

Since the late nineteenth century, it has been debated whether rivers or glaciers are more
effective agents of erosion. The dramatic landscapes associated with glaciated terrain have …

Glacial retreat in recent decades has exposed unstable slopes and allowed deep water to
extend beneath some of those slopes. Slope failure at the terminus of Tyndall Glacier on 17 …

The Antarctic Dry Valleys (ADV) are generally classified as a hyper-arid, cold-polar desert.
The region has long been considered an important terrestrial analog for Mars because of its …

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

Quantitative estimates of sediment flux and the global cycling of sediments from hillslopes to
rivers, estuaries, deltas, continental shelves, and deep-sea basins have a long research …

The temporal variability in sediment export yield from glaciers over a timescale of multiple
glacial cycles (eg 1× 102− 1× 106 years) is of interest for a wide range of applications in …

Accelerated glacier and ice sheet retreat and thinning in recent decades has profound
consequences for catchment sediment supply with attendant repercussions for nutrient …

The presence of a complex bedform arrangement on the sea floor of the continental shelf in
the western Amundsen Sea Embayment, West Antarctica, indicates a multi-temporal record …