Hostname: page-component-745bb68f8f-l4dxg Total loading time: 0 Render date: 2025-01-15T02:40:03.020Z Has data issue: false hasContentIssue false
  • English
  • Français

Evidence for Early Holocene deglaciation of the Vestfold Hills, east Antarctica

Published online by Cambridge University Press:  27 October 2009

Sean J. Fitzsimons  and
Eugene W. Domack
Sean J. Fitzsimons
Affiliation:
Department of Geography, University of Otago, PO Box 56, Dunedin, New Zealand
Eugene W. Domack
Affiliation:
Department of Geology, Hamilton College, Clinton, New York 13323, USA
Get access Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Notes
Information
Polar Record , Volume 29 , Issue 170 , July 1993 , pp. 237 - 240
Copyright
Copyright © Cambridge University Press 1993

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adamson, D.A., and Pickard, J.. 1983. Late Quaternary ice movements across the Vestfold Hills, east Antarctica. In: Oliver, R.L., James, P.R., and Jago, J.B. (editors). Antarctic earth science. Canberra: Australian Academy of Sciences: 465–469.Google Scholar
Adamson, D.A., and Pickard, J.. 1986. Cainozoic history of the Vestfold Hills. In: Pickard, J. (editor). Antarctic oasis. Sydney: Academic Press: 63–97.Google Scholar
Clapperton, C.M., and Sugden, D.E.. 1982. Late Quaternary glacial history of George VI Sound area, west Antarctica. Quaternary Research 18 (3): 243–267.CrossRefGoogle Scholar
Colhoun, E.A. 1991. Geological evidence for changes in the east Antarctic ice sheet (60°–120°E) during the last glaciation. Polar Record 27 (163): 345–355.Google Scholar
Colhoun, E.A., Mabin, M.C.G., Adamson, D.A., and Kirk, R.M.. 1992. Antarctic ice volume and contribution to sealevel fall at 20,000 yr BP from raised beaches. Nature 358: 316–319.CrossRefGoogle Scholar
Denton, G.H., Bockheim, J.G., Wilson, S.C., and Stuiver, M.. 1989. Late Wisconsin and Early Holocene glacial history, inner Ross Embayment, Antarctica. Quaternary Research 31 (2): 151–182.Google Scholar
Domack, E.W., Jull, A.J.T., Anderson, J.B., Linick, T.W., and Williams, C.R.. 1989. Application of tandem accelerator mass-spectrometer dating to Late Pleistocene-Holocene sediments of the east Antarctic continental shelf. Quaternary Research 31 (2): 277–287.Google Scholar
Domack, E.W., Jull, A.J.T., and Nakao, S.. 1991. Advance of east Antarctic outlet glaciers during the hypsithermal: implications for the volume state of the Antarctic ice sheet under global warming. Geology 19: 1059–1062.Google Scholar
Fitzsimons, S.J. 1991. Geomorphic development of the Vestfold Hills: questions regarding Holocene deglaciation. In: Gillieson, D.S., and Fitzsimons, S.J. (editors). Quaternary research in Australian Antarctica: future directions. Canberra: Department of Geography and Oceanography, University College, Australian Defence Force Academy (Special Publication 3): 25–35.Google Scholar
Payne, A.J., Sugden, D.E., and Clapperton, C.M.. 1989. Modeling the growth and decay of the Antarctic Peninsula ice sheet. Quaternary Research 31 (2): 119–134.Google Scholar