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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Format: | Text |
Language: | unknown |
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PDXScholar
2002
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Online Access: | https://pdxscholar.library.pdx.edu/geology_fac/3 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1002&context=geology_fac |