Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5787
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dc.contributorNational Science Foundation (U.S.)-
dc.contributor.authorLangway, Chester C., 1929--
dc.contributor.authorHerron, M. M.-
dc.contributor.authorCragin, James H.-
dc.date.accessioned2016-03-21T21:08:28Z-
dc.date.available2016-03-21T21:08:28Z-
dc.date.issued1974-01-
dc.identifier.urihttp://hdl.handle.net/11681/5787-
dc.descriptionResearch Report-
dc.descriptionAbstract: Measurements of the concentrations of Na+, K+, Mg++ and Ca++ were made on 28 samples from the 255-m-deep ice core from Little America V. All concentrations decrease sharply with depth from the firn-ice transition at 52 m to somewhere between 125 m and 150 m. From 150 m to 250 m the cationic concentrations are relatively constant. This is interpreted to indicate that the ice above 125 m fell as snow on the Ross Ice Shelf and that ice below 150 m originated inland on Marie Byrd Land.-
dc.publisherCold Regions Research and Engineering Laboratory (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1014561-
dc.relation.ispartofseriesResearch report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 316.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectAntarctica-
dc.subjectChemical properties-
dc.subjectGeochemistry-
dc.subjectChemistry-
dc.subjectGeochronology-
dc.subjectIonic concentrations-
dc.subjectIons-
dc.subjectCations-
dc.subjectIon density-
dc.subjectIce cores-
dc.subjectRoss Ice Shelf, Antarctica-
dc.subjectEPOLAR-
dc.titleChemical profile of the Ross ice shelf at Little America V, Antarctica-
dc.typeReporten_US
Appears in Collections:Research Report

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