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The movement of water beneath ice sheets exerts an important, yet poorly understood, control on how ice masses respond to climatic warming. However, the subglacial realm of ice sheets is one of the most inaccessible environments on Earth. Consequently, little is known about the processes that operate beneath today's ice masses - and how these will evolve in the future. Subglacial landforms present in formerly-glaciated regions provide comparatively accessible records of glacial erosion, deposition, and sediment transport beneath ice sheets that have undergone deglaciation. This thesis investigates the potential of these landforms to reconstruct the flow of water beneath past ice sheets as analogues for how contemporary ice masses will evolve in a warming climate. A combination of geophysical approaches, including multibeam-bathymetric surveys, high-resolution 3D seismic-reflection data, conventional 3D seismic-reflection data, and geotechnical information from boreholes, is used to investigate the flow of water beneath ice sheets which covered western Europe and more expansive regions of the Antarctic continental shelf in the past. These data are first used to constrain the routing and fluxes of subglacial water beneath the retreating West Antarctic Ice Sheet. The impact of subglacial water flow on ice-sheet dynamics during deglaciation is then examined by imaging the internal structures of ancient channels incised by meltwater - tunnel valleys - in the North Sea. The unprecedented detail provided by the high-resolution 3D seismic-reflection data provides links between ice-sheet dynamics and subglacial meltwater flow during deglaciation. A numerical modelling approach constrains these linkages further by estimating the time that the meltwater channels take to form beneath deglaciating ice sheets. Finally, the sedimentation patterns resulting from subglacial water flow and other glacially-influenced processes during deglaciation are examined. Greater coverage of geophysical data on formerly glaciated continental margins, combined with chronological constraints from shallow drilling, will improve understanding of the hydrological systems and dynamics of former and contemporary ice sheets.

The use of iceberg-keel ploughmarks as proxy indicators of past and present iceberg morphology, keel depth and drift direction has seldom been approached in the southern hemisphere. Using high-resolution multi-beam swath bathymetry of the mid-shelf Pine Island Trough and outermost Weddell Sea shelf regions of Antarctica, detailed analysis of >13,000 iceberg-keel ploughmarks was undertaken. By considering the draft of icebergs calved from Antarctica today, calculated from detailed satellite altimetric datasets by this work, almost all observed ploughmarks were interpreted to be relict features. In Pine Island Trough, ploughmark planform parameters and cross-sections imply calving of a large number of non-tabular icebergs with v-shaped keels from the palaeo-Pine Island-Thwaites ice stream. Geological evidence of ploughmark form and modern water depth distribution indicates calving-margin thicknesses (949 m) and subaerial ice cliff elevations (102 m) equivalent to the theoretical threshold predicted to trigger ice-cliff structural collapse and calving by marine ice-cliff instability (MICI) processes. Thus, ploughmarks provide the first observational evidence of rapid retreat of the palaeo-Pine Island-Thwaites ice stream, driven by MICI processes commencing ~12.3 cal ka BP. On the Weddell Sea shelf, ploughmark morphologies imply considerable variation in palaeo-iceberg shape and size, most likely reflecting calving from multiple source margins. In turn, an absence of grounded ice on the Weddell Sea shelf and a palaeo-oceanographic regime comparable to today are implied at the time of formation. Analysis of a 3D seismic cube of the Sea Lion Field area of the North Falkland Basin reveals iceberg-keel ploughmarks incised into the modern- and palaeo-seafloor, formed by icebergs of varying shape and size that most-likely calved from the Antarctic Ice Sheet during three past glacial periods (estimated ages ~18 - 26.5 ka BP, ~246 ka BP, ~9.8 Ma BP). Despite illustrating the possibility of iceberg drift into the North Falkland Basin today, the relict ploughmark age implies little risk to any seafloor structures in the area, which might be required for hydrocarbon production. By these analyses, the significance of iceberg-keel ploughmarks as indicators of palaeo-glaciology and palaeo-oceanography at the time of formation is emphasised.