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...

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Bibliographic Details
Main Authors: Siegert, Martin J, Welch, Brian, Morse, David, Vieli, Andreas, Blankenship, Donald D, Joughin, Ian, King, Edward C, Leysinger Vieli, Gwendolyn, Payne, Antony J, Jacobel, Robert
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science 2004
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