Tidal flexure at ice shelf margins
Hinge zones accommodate the differential tidal movement between floating ice shelves, which move with the sea tide, and grounded ice sheets, which do not. Observations on Rutford Ice Stream and Ronne Ice Shelf, Antarctica, using the kinematic method of Global Positioning System, have yielded the fir...
Published in: | Journal of Geophysical Research: Solid Earth |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | unknown |
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American Geophysical Union
1995
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Online Access: | http://nora.nerc.ac.uk/id/eprint/515880/ https://doi.org/10.1029/94JB02467 |