Fracture and back stress along the Byrd Glacier flowband on the Ross Ice Shelf
East Antarctic ice discharged by Byrd Glacier continues as a flowband to the calving front of the Ross Ice Shelf. Flow across the grounding line changes from compressive to extensive as it leaves the fjord through the Transantarctic Mountains occupied by Byrd Glacier. Magnitudes of the longitudinal...
Published in: | Antarctic Science |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2004
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0954102004002056 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102004002056 |