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

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 sat...

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Bibliographic Details
Published inNature geoscience Vol. 2; no. 8; pp. 585 - 588
Main Authors King, E. C, Hindmarsh, R. C. A, Stokes, C. R
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 01.08.2009
Nature Publishing Group
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