Last edited by Zolorr
Sunday, April 26, 2020 | History

4 edition of Synopsis of the geology of Canada found in the catalog.

Synopsis of the geology of Canada

being a summary of the principal terms employed in Canadian geological nomenclature

by Henry Marc Ami

  • 29 Want to read
  • 28 Currently reading

Published by s.n. in [Ottawa? .
Written in English

    Subjects:
  • Geology -- Canada.,
  • Géologie -- Canada.

  • Edition Notes

    Statementby Henry M. Ami
    SeriesCIHM/ICMH Microfiche series = CIHM/ICMH collection de microfiches -- no. 26308, CIHM/ICMH microfiche series -- no. 26308
    ContributionsRoyal Society of Canada
    The Physical Object
    FormatMicroform
    Pagination1 microfiche (24 fr.).
    Number of Pages24
    ID Numbers
    Open LibraryOL24141098M
    ISBN 100665263082


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Summary; Geological History of Canada: The continent Laurentia, which includes what is now the Canadian Shield, was formed through the assembly of a number of smaller continents over the period from around 4 Ga to 1 Ga. Over the past Ma, Laurentia moved north from deep within the southern hemisphere.

The three major sections of this volume include six chapters describing the regional Quaternary geology of Canada, two describing the Quaternary geology and climatic history of Greenland, and six that review applied Quaternary geology in Canada, including chapters on paleobotanical analysis, geodynamics, geomorphic processes, terrain geochemistry, Quaternary resources.

84 Summary of the Geology of Canada Canada embraces four major geological regions*: (1) the continental shelves and coastal plains marginal to Synopsis of the geology of Canada book Atlantic, Pacific and Arctic Oc-eans; {2) the Phanerozoic orogens-- Appalachian, Cordilleran and lnnuitian, bordering the continent; {3) the adjacent plat- forms-St.

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[Robert Gordon Blackadar; J A Fraser]. Locality: South side of St. Helen's Island. ORDOVICIAN. The Ordovician (Cambro-Silurian and Lower Silurian) formations in the Montreal district are seven in number, and from the Lorraine or upper- most Ordovician in Canada, down to the Potsdam sandstone there is not a single break in the suc- cession.

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