Extension of the Antarctic ice sheet between 98oE and 111oE (Obruchev Hills, Bunger Hills & Windmill Islands) at the Last Glacial Maximum.

Related publications

• Petroleum hydrocarbons ten years after spillage at a helipad in Bunger Hills, East Antarctica. Antarctic Science, 1999 (Ref: 8897)
  Authors:

  Gore D.B.Revill A.T.Guille D.
  Category 1: Peer-reviewed literature

  Surface and subsurface sediments from a helipad in Bunger Hills were collected ten years after accidental contamination with a small quantity (probably less than 10 litres) of petroleum products.

• Bunger Hills, East Antarctica: Ice free at the Last Glacial Maximum. Geology, 2001 (Ref: 10403)
  Authors:

  Gore D.B.Rhodes E.J.Augustinus P.C.Leishman M.R.Colhoun E.A.Rees-Jones J.
  Category 1: Peer-reviewed literature
• Chapter 11: Antarctica at the Last Glacial Maximum, Deglaciation and the Holocene Antarctic Climate Evolution. Developments in Earth & Environmental Science, 2008 (Ref: 13917)
  Authors:

  Wright A.P.White D.Gore D.B.Siegert M.J.
  Category 1: Peer-reviewed literature

  : Recent technological advances in the study and dating of both land and marine glacial geologic features combined with improvements in both glaciological and post-glacial isostatic rebound modelling have led to significant improvements in our knowledge and understanding of the Antarctic Ice Sheets…

• Algae River: an extensive drainage system in the Bunger Hills, East Antarctica Polar Record, 2002 (Ref: 10413)
  Authors:

  Gibson J.A.E.Gore D.B.Kaup E.
  Category 1: Peer-reviewed literature
• Reconstruction of ice flow across the Bunger Hills, East Antarctica. Antarctic Science, 1997 (Ref: 8119)
  Authors:

  Augustinus P.C.Gore D.B.Leisman M.R.Zwartz D.Colhoun E.A.
  Category 1: Peer-reviewed literature