Ice Flow Direction Change in Interior West Antarctica
Upstream of Byrd Station (West Antarctica), ice-penetrating radar data reveal a distinctive fold structure within the ice, in which isochronous layers are unusually deep. The fold has an axis more than 50 kilometers long, which is aligned up to 45° to the ice flow direction. Although explanations fo...
Published in: | Science |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
2004
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Subjects: | |
Online Access: | http://dx.doi.org/10.1126/science.1101072 https://www.science.org/doi/pdf/10.1126/science.1101072 |