Cainozoic history of the Vestfold Hills.

D. A. Adamson, J. Pickard

Research output: Contribution to journalArticlepeer-review

123 Citations (Scopus)

Abstract

The fossil record, sediments and landforms of the Vestfold Hills all provide evidence of those Cainozoic events which initiated the largest ice sheet on earth, viz Antarctica. A Pliocene marine deposit is unique to E Antarctica; its geological character and fossil biota are discussed. The evolution of freshwater lakes is outlined; these major features of the Vestfold Hills, with 8% of the area (plus a further 2% comprising saline and hypersaline lakes) includes supraglacial and proglacial waterbodies, and closed and open rock basins. -P.J.Jarvis School Biological Sciences, Macquarie Univ., North Ryde, NSW 2113, Australia.

Original languageEnglish
Pages (from-to)63-97
Number of pages35
JournalAmerican Society of Mechanical Engineers (Paper)
Publication statusPublished - 1986

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