Search results
Results from the WOW.Com Content Network
The District of Mackenzie was a regional administrative district of Canada's Northwest Territories. The district consisted of the portion of the Northwest Territories directly north of British Columbia , Alberta , and Saskatchewan on Canada's mainland.
Mackenzie was a federal electoral district in Saskatchewan, Canada, that was represented in the House of Commons of Canada from 1904 to 1997. This riding was created in 1903, when Saskatchewan was still a part of the Northwest Territories. In 1905, when Saskatchewan was created, the district was retained in the province.
The MacKenzie Art Gallery (MAG; French: Musee d’art MacKenzie) [2] is an art museum located in Regina, Saskatchewan, Canada.The museum occupies the multipurpose T. C. Douglas Building, situated at the edge of the Wascana Centre.
The Districts of Alberta, Assiniboia, Athabasca, and Saskatchewan were reorganized to form the provinces of Alberta and Saskatchewan (1905). The autonomous District of Keewatin, portions of which had been converted into the expansion of Manitoba and Ontario, gave up its autonomy and became a district within the North-West Territories (1905).
The Mackenzie River has a similar range of fish fauna to the Mississippi River system. It is believed that the two river systems were connected during the Ice Ages by meltwater lakes and channels, allowing fish in the two rivers to interbreed. [48] Fish in the Mackenzie River proper include the northern pike, several minnow species, and lake ...
Saskatchewan: William Mackenzie King: 29 October 1925 28 June 1926 Portage la Prairie: Manitoba: Arthur Meighan: 29 June 1926 25 September 1926 Prince Albert: Saskatchewan: William Mackenzie King: 25 September 1926 6 August 1930 Calgary West: Alberta: R.B. Bennett: 7 August 1930 22 October 1935 Prince Albert: Saskatchewan: William Mackenzie ...
The mafic dikes cut Archean and Proterozoic rocks, including those in the Athabasca Basin in Saskatchewan, Thelon Basin in Nunavut and the Baker Lake Basin in the Northwest Territories. The source for the Mackenzie dike swarm is considered to have been a mantle plume center called the Mackenzie hotspot.
Tectonic and magmatic features associated with the Mackenzie Large Igneous Province. Red star shows the initial Mackenzie plume zone relative to the lithosphere; partial black circle is the estimate of the zone of plume influence on stress-field orientation; dark lines are dikes of the Mackenzie swarm; CRB indicates the Coppermine River basalts; M indicates the Muskox intrusion.