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Formation of mega-scale glacial lineations observed beneath a West Antarctic ice stream

King, E.C.; Hindmarsh, R.C.A.; Stokes, C.R.


E.C. King

R.C.A. Hindmarsh


Most discharge from large ice sheets takes place through fast-flowing ice streams and their speed is strongly modulated by interactions between the ice and the underlying sediments. Seismic surveys and investigations through boreholes have revealed a spatial association between fast ice flow and saturated deformable sediments. Nevertheless, our knowledge of the morphology of the interface between ice and sediments is still limited, resulting in only rudimentary understanding of the basal boundary conditions beneath ice streams and the generation of subglacial bedforms. Here we present radar data from the bed of a West Antarctic ice stream that reveal the presence of mega-scale glacial lineations. We combine these data with previously published seismic data and show that these lineations develop in areas of dilatant deforming till and are part of a dynamic sedimentary system that undergoes significant change by erosion and deposition on decadal timescales. We find that the mega-scale glacial lineations are indistinguishable from those found on beds of palaeo-ice streams, providing conclusive evidence for the hypothesis that highly elongate bedforms are a characteristic of fast-flow regions in ice sheets.


King, E., Hindmarsh, R., & Stokes, C. (2009). Formation of mega-scale glacial lineations observed beneath a West Antarctic ice stream. Nature Geoscience, 2(8), 585-596.

Journal Article Type Article
Publication Date Aug 1, 2009
Deposit Date Sep 23, 2009
Journal Nature Geoscience
Print ISSN 1752-0894
Electronic ISSN 1752-0908
Publisher Nature Research
Peer Reviewed Peer Reviewed
Volume 2
Issue 8
Pages 585-596