Last edited by Vigul
Friday, May 1, 2020 | History

3 edition of Precambrian geology of the Half Way Hills area, District of Keewatin found in the catalog.

Precambrian geology of the Half Way Hills area, District of Keewatin

Frederick C. Taylor

Precambrian geology of the Half Way Hills area, District of Keewatin

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  • 28 Currently reading

Published by Geological Survey of Canada, Canadian Govt. Pub. Centre, Supply and Services Canada [distributor] in Ottawa, Canada .
Written in English

    Places:
  • Nunavut,
  • Half Way Hills Region.
    • Subjects:
    • Geology, Stratigraphic -- Precambrian.,
    • Geology -- Nunavut -- Half Way Hills Region.

    • Edition Notes

      StatementF.C. Taylor.
      SeriesMemoir / Geological Survey of Canada ;, 415, Memoir (Geological Survey of Canada) ;, 415.
      Classifications
      LC ClassificationsQE185 .A2 no. 415, QE653.5 .A2 no. 415
      The Physical Object
      Pagination19 p. :
      Number of Pages19
      ID Numbers
      Open LibraryOL2281491M
      ISBN 100660119293
      LC Control Number86146361


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Precambrian geology of the Half Way Hills area, District of Keewatin by Frederick C. Taylor Download PDF EPUB FB2

Get this from a library. Precambrian geology of the Half Way Hills area, District of Keewatin. [Frederick C Taylor; Geological Survey of Canada.]. An Aquatic Resource Survey of Victoria and King William Islands and the Northeastern District of Keewatin, Northwest Territories.

[Ottawa]: Supply and Services Canada, ISBN ; Taylor, Frederick C. Precambrian Geology of the Half Way Hills Area, District of Keewatin. Ottawa, Canada: Geological Survey of Canada, ISBN Not to be confused with Keewatin Region, Northwest Territories, although much of their territory overlapped.

Extent of the District of Keewatin before its reorganization in The District of Keewatin was a territory of Canada and later an. An introduction to the geology of Dayton and vicinity, with special reference to the gravel ridge area south of the city, including Hills and dales and Moraine park, (Dayton, O.

[Indianapolis, The Hollenbeck Press, printers], ), by Aug. Foerste (page images at HathiTrust; US access only). The horizontal section is one which is in constant use by the practical geologist: the results of the first traverse of a district may be jotted down in his note-book in the form of a horizontal section (with accompanying notes), and the written memoir on the geology of any district composed largely of stratified rocks will almost certainly.

Gordon, T M.,Precambrian geology of the Daly Bay area, District of Keewatin: Ottawa, Geol. Survey of Canada Memoir21 p. Mapping the Upper Mantle: Three-Dimensional Modeling of Earth. Regional structural and metamorphic geology of the Committee Bay Belt, Laughland Lake area, central mainland, Nunavut; Geological Survey of Canada, Current Research C13, 19 p.

Sudbury (official name Greater Sudbury) is a city of approximatelypeople, located in Northern Ontario, Canada. It is Northern Ontario’s largest city in both area and population, and a major retail and service centre for the region. Understand Sudbury’s weather is typical of locations on the Canadian Shield, with hot summers and cold winters.

This chapter describes tectonic evolution in the Precambrian. An analysis of the Precambrian sequences Precambrian geology of the Half Way Hills area the continents of the Southern Hemisphere is presented along with a compilation of proposed correlations according to the scheme used for the Northern Hemisphere.

District of Keewatin book GEOLOGY OF THE Precambrian geology of the Half Way Hills area PASS AREA, FREMONT COUNTY, WYOMING 0 10 MILES m EXPLANATION Tertiary rocks Mesozoic rocks ~ L'.2J Paleozoic rocks ~ I Precambrian granite 0 Precambrian metasedimentary rocks Quadrangle locations I t7de:r on plate 1 FIGURE I.-Generalized geologic map showing the geographicCited by: Thompson (populat) is the largest city in the Northern Region of Manitoba and is situated along the Burntwood River, kilometers ( miles) north of ally founded in as a mining town, Thompson now primarily serves as the "Hub of the North", providing goods and services (e.g., healthcare, retail trade) to the surrounding : Northern Region.

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The stratified rocks straddling the Larder Lake-Cadillac Break historically have been subdivided into two volcanic and two sedimentary groups (Wilson, ).The older volcanic unit, composed mainly of ultramafic to mafic rocks with rare felsic units, is termed the Precambrian geology of the Half Way Hills area Group in the eastern part of the area, while its equivalent in the western part is referred to as the Larder Lake Group.

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Re-release; Geological Survey of Canada. Geological Survey of Canada, Geophysical Series Map G,Abstract: The Precambrian geology of eastern Zambia and Malawi is highly complex due to multiple episodes of rifting and collision, particularly during the formation of Greater Gondwana as a product of the Neoproterozoic Pan-African Orogeny.

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