Rock glacier surface motion in Beacon Valley, Antarctica, from synthetic-aperture radar interferometry
We present radar interferograms of rock glaciers in the Beacon Valley sector of the McMurdo Dry Valleys, in East Antarctica, as part of a comprehensive study of surface processes in the area. Due to the relative absence of net precipitation (snow) in this region and the stability of the surface, the...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
eScholarship, University of California
2002
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Subjects: | |
Online Access: | https://escholarship.org/uc/item/5nq6z04d |