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Ice core / Glaciology / Glacier / Antarctica / Shabtaie Ice Ridge / Physical geography / Whillans Ice Stream / Mercer Ice Stream


Ice stream C, which is next to ice stream B, is in contrast, virtually stagnant. Its velocity is less than 10 meters per year (McDonald and Whillans, in press), and it must be thickening. The net mass accumulation for th
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Document Date: 2011-05-06 15:41:32


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City

Washington / D.C. / Vancouver / /

Company

Engineering Laboratory / S. ANANDAKRISHNAN D.D. / RB. D.D. / Blankenship D.D. C. / R.V. D.D. / ST. D.D. / CR. D.D. / S.T. D.D. / Blankenship D. D. / R.B. D.D. / S. Shabtaie D.D. / S. D.D. / /

Continent

Antarctica / /

Country

Greenland / United States / /

Facility

University of Washington / Ohio State University / Polar Research Center University of Wisconsin Madison / Upstream B camp / University of Wisconsin / Ohio State North Camp / Byrd Station / /

IndustryTerm

satellite tracking / satellite tracking data / Fault-plane solutions / transit satellite tracking / seismic travel times / strain energy causes / strain energy dissipation / energy / /

NaturalFeature

Ross Sea / Byrd Glacier / Siple Coast / /

Organization

University of Washington / American Geophysical Union / Polar Ice Coring Office / National Science Foundation / United States Army / Ohio State University / Geophysical and Polar Research Center / Polar Research Center University of Wisconsin Madison / University of Wisconsin / /

Person

Marie Byrd Land / /

Product

Bentley 1987a / /

ProvinceOrState

Alberta / Wisconsin / British Columbia / /

PublishedMedium

Journal of Geophysical Research / /

Region

Antarctic / West Antarctic / West Antarctica / /

Technology

geophysics / Remote sensing / /

SocialTag