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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Published in | Nature geoscience Vol. 2; no. 8; pp. 585 - 588 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
London
Nature Publishing Group UK
01.08.2009
Nature Publishing Group |
Subjects | |
Online Access | Get full text |
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