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...

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Bibliographic Details
Main Authors: Rignot, E, Hallet, B, Fountain, A
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2002
Subjects:
Online Access:https://escholarship.org/uc/item/5nq6z04d