An emerging body of evidence from studies of the last glacial/interglacial cycle suggests that
the East and West Antarctic ice sheets have not advanced and retreated in concert. The …

Simple insights from the physics of ice, water and sediment place constraints on the possible
sediment-transport behavior of glaciers and ice sheets. Because glaciers concentrate runoff …

Transport of participate material across continental shelves is well demonstrated by the
distributions on the seabed and in the water column of geological, chemical, or biological …

Onshore and offshore studies show that an expanded, grounded ice sheet occupied the
Ross Sea Embayment during the Last Glacial Maximum (LGM). Results from studies of till …

Ice-shelf development is favored by rapid flow of cold ice from outlet glaciers or ice streams
into protected embayments with localized high spots. Basal melting of ice shelves is rapid …

Most of the velocity of ice stream B near the Upstream B camp (UpB), West Antarctica,
appears to arise from deformation of a seismically detected, subglacial till layer that …

In part 1 a simple sedimentation model is presented in which subglacial icecontact,
proglacial ice-contact, inner and outer proximal, and distal glacimarine zones are …

This paper argues that glaciomarine environments can be regarded as special, glacially-
influenced types of continental margin environments (eg continental shelf, slope, rise and …

In many geological epochs, glacial sediments are widespread. This type of sedimentation
results from the interaction between atmosphere, cryosphere, hydrosphere and biosphere …

Studying the history of ice-sheet behaviour in the Ross Sea, Antarctica's largest drainage
basin can improve our understanding of patterns and controls on marine-based ice-sheet …