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...
Main Authors: | , , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science
2004
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Subjects: | |
Online Access: | https://www.zora.uzh.ch/id/eprint/136420/ https://www.zora.uzh.ch/id/eprint/136420/1/2004_Vieli_1948.full.pdf https://doi.org/10.5167/uzh-136420 https://doi.org/10.1126/science.1101072 |