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Sunday, November 22, 2020 | History

2 edition of Quaternary geology of Wollaston Peninsula, Victoria Island, Northwest Territories found in the catalog.

Quaternary geology of Wollaston Peninsula, Victoria Island, Northwest Territories

Quaternary geology of Wollaston Peninsula, Victoria Island, Northwest Territories

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  • 28 Currently reading

Published by Energy, Mines and Resources in Ottawa .
Written in English

    Subjects:
  • Geology - Northwest Territories - Victoria Island

  • Edition Notes

    11

    The Physical Object
    Pagination84 p.
    Number of Pages84
    ID Numbers
    Open LibraryOL22018422M
    ISBN 100660144263


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Quaternary geology of Wollaston Peninsula, Victoria Island, Northwest Territories Download PDF EPUB FB2

Late Glacial landforms of Wollaston Peninsula, Victoria Island, Northwest Territories: product of ice-marginal retreat, surge, and mass stagnation February Canadian Journal of Earth Sciences. Late Quaternary sea level history in the Paulatuk to Bathurst Inlet area, Northwest Territories.

raised beaches of western Wollaston Peninsula, Victoria Island, Canadian Arctic, near the. Geology of the Tertiary and Quaternary Periods in the North-west Part of Peru Thomas Owen Bosworth, Henry Woods Macmillan and Company, limited, - Geology - pages.

Northwest Territories: InfoCanada: Provinces and Territories on *FREE* shipping on qualifying offers. Surficial geology, Storkerson Peninsula, Victoria Island and Stefansson Island, District of Franklin, Northwest Territories. Geological Survey of Canada, Ottawa, Cited by: Book Chapter (8) Article Type.

Facet list. Research Article Victoria British Columbia (1) Northwest Territories (1) Saskatchewan Wollaston Lake Belt (1) Yukon Territory (2) Caribbean region West Indies.

The Quaternary history of the Western Plains of Victoria, Australia: geology, landscape and people. Quaternary volcanic zones in the North Island of New Zealand and their relationship to structure J. Cole 1 Bulletin Volcanologique vol pages – () Cite this articleCited by:.