Fast-flow signature in the stagnated Kamb Ice Stream, West Antarctica
Among the major ice streams that drain West Antarctica, Kamb Ice Stream (formerly called Ice Stream C) is unique in that it stagnated ∼150 yr ago, but its former fast-flow conditions are virtually unknown. Here we present surface-based radar profiles of the ice stream's undulating internal stra...
| Published in: | Geology |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Geological Society of America
2004
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| Subjects: | |
| Online Access: | https://eprints.whiterose.ac.uk/92154/ https://eprints.whiterose.ac.uk/92154/1/G20317_Ng_merged.pdf https://doi.org/10.1130/G20317.1 |