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Quaternary geology of the Fort Fraser and Manson River map areas, central British Columbia / by Alain Plouffe.M42-554E

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The Fort Fraser and Manson River map areas were last glaciated during the Late Wisconsinan Fraser Glaciation. Quaternary sediments predating this event are rare. The oldest deposits identified are oxidized sand and gravel, which locally contain placer gold. Stratigraphic evidence of a pre-Fraser glaciation was found at one site. Sediments of the Olympia Nonglacial Interval have been identified at three sites. Paleoecological reconstruction indicates climatic conditions cooler than at present for at least part of that nonglacial interval.--Abstract

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Publication information
Department/Agency
  • Geological Survey of Canada.
TitleQuaternary geology of the Fort Fraser and Manson River map areas, central British Columbia / by Alain Plouffe.
Series title
  • Bulletin 0068-7626 554
Publication typeMonograph - View Master Record
Language[English]
FormatPhysical text
Note(s)
  • "The Fort Fraser and Manson River map areas were last glaciated during the Late Wisconsinan Fraser Glaciation. Quaternary sediments predating this event are rare. The oldest deposits identified are oxidized sand and gravel, which locally contain placer gold. Stratigraphic evidence of a pre-Fraser glaciation was found at one site. Sediments of the Olympia Nonglacial Interval have been identified at three sites. Paleoecological reconstruction indicates climatic conditions cooler than at present for at least part of that nonglacial interval."--Abstract.
  • Résumés en français
Publishing information
  • Ottawa - Ontario : Natural Resources Canada. 2000.
BindingSoftcover
Description62p. : figs., illus., maps, references ; 28 cm. + maps.
ISBN0-660-18170-3
ISSN0068-7626
Catalogue number
  • M42-554E
Subject terms
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