The dynamics of glacial sliding over water-saturated tills are poorly constrained and difficult
to capture realistically in large-scale models. Experiments characterize till as a plastic …

The flow of glaciers is largely controlled by changes at the ice–bed interface, where basal
slip and sediment deformation drive basal glacier motion. Determining subglacial conditions …

Subglacial bedforms are relevant geomorphic markers for palaeo-glaciological
reconstructions. Due to the complexity of thermomechanical interactions between ice, till and …

Glaciers are commonly conceptualized as bodies composed of snow and ice. Yet, many
glaciers contain a substantial amount of rock, especially those abutting steep mountains …

Subglacial abrasion drives erosion for many glaciers, inundating forefields and proglacial
marine environments with glaciogenic sediments. Theoretical treatments of this process …

Fast ice affects many coastlines in high-and mid-latitude regions, shaping the coastal
morphology by acting as both a protective barrier from winter storms and as an erosive …

As mobile diamicton sediments move across already deposited sediments whether on land
or into oceans generated by either glaciers/ice sheets or landslides, a series of soft …

Water pressure beneath glaciers influences ice velocity. Subglacial hydrology models are
helpful for gaining insight into basal conditions, but models depend on unconstrained …

Subglacial processes influence the large-scale behaviour of glaciers and determine the
geological processes that occur at the ice-substrate interface. In this paper we focus on …

This review of the dynamics of the flow of glaciers and ice sheets focusses on the
mathematical models which have been developed to explain a number of observations in …