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Analysis of the Byrd Station Strain Net, Antarctica

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/51511

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dc.creator Dewart, Gilbert
dc.creator Whillans, Ian M.
dc.creator Brecher, Henry H.
dc.date.accessioned 2012-02-23T16:12:42Z
dc.date.available 2012-02-23T16:12:42Z
dc.date.issued 1974-06
dc.identifier.citation Dewart, Gilbert, Ian M. Whillans and Henry H. Brecher. 1974. Analysis of the Byrd Station Strain Net, Antarctica. Institute of Polar Studies Report No. 48, Research Foundation and the Institute of Polar Studies, The Ohio State University, iv, 49 pages. en_US
dc.identifier.issn 0078-415X
dc.identifier.uri http://hdl.handle.net/1811/51511
dc.description On cover: RF 2500. en_US
dc.description.abstract This report presents some results of field investigations relating to the study of glacier flow in Marie Byrd Land, Antarctica. The physical quantities necessary for a solution to the problem of the mode of flow of the continental ice sheet in the Ross glacial drainage basin are being sought by several principal lines of investigation: determination of surface strain rate and surface slope by analysis of precise surveys of the Byrd Station Strain Net that have been carried out by the Topographic Branch of the U.S. Geological Survey; determination of strain rate and temperature distribution at depth in the deep hole at Byrd Station drilled by the U.S. Army Cold Regions Research and Engineering Laboratory; determination of ice thickness and of glacier bed configuration and conditions by geophysical exploration, including seismic, gravimetric, magnetic and radio-echo sounding methods; analysis of the structure and dynamic physical properties of ice; and observation of snow deposition and metamorphosis and surface morphology in order to explain parts of the core from Byrd Station deep drill hole, and estimate the mass balance. Much of the material presented in the report is based upon observations made by field parties which were based at Byrd Station and operated in the region of the Byrd Station Strain Net, which lies between Byrd Station and the Ross-Amundsen ice divide, during the austral summers of 1967-68, 1969-70, 1971-72, and 1973-74. en_US
dc.description.sponsorship National Science Foundation Grants GA-1141, GA-14425 and GV-26137X. en_US
dc.language.iso en_US en_US
dc.publisher Research Foundation anf the Institute of Polar Studies, The Ohio State University. en_US
dc.relation.ispartofseries Institute of Polar Studies Report No. 48. en_US
dc.subject Glacier flow en_US
dc.subject Byrd Station Strain Net en_US
dc.subject Antarctic glaciation en_US
dc.title Analysis of the Byrd Station Strain Net, Antarctica en_US
dc.type Technical Report en_US