Chronological list of expeditions and histrical events in northern Canda. IX. 1881–96

Polar Record ◽  
1973 ◽  
Vol 16 (103) ◽  
pp. 559-577
Author(s):  
Alan Cooke ◽  
Clive Holland

During this short period began what may be termed the re-exploration of northern Canada, a scientific examination of lands that had been roughly charted by expeditions of the previous hundred years, but that were otherwise little known except to fur traders, a few missionaries, and the occasional traveller. Only now did the newly confederated Dominion of Canada begin to take a practical interest in its vast northern expansions. The government sent three scientific expeditions to Hudson Strait and Hudson Bay, and the Geological Survey of Canada began to direct its attention towards the north. One of its officers, A. P. Low, explored the length and breadth of the Quebec-Labrador peninsula virtually single-handed and, as if anticipating the Klondike gold rush, towards which the work of many prospectors in Yukon Territory was steadily leading, Dawson, McConnell and Ogilvie published detailed accounts of routes and conditions in the Northwest Territories and Yukon Territory, information that proved invaluable to both government and individuals when the rush was on.

Polar Record ◽  
1973 ◽  
Vol 16 (104) ◽  
pp. 707-722 ◽  
Author(s):  
Alan Cooke ◽  
Clive Holland

With this instalment of our list, the Klondike gold rush reached its height and, nearly as quickly, began to decline as the miners’ interest turned to newer strikes in Alaska. The great influx of prospectors to the Klondike region led to the passage of the Yukon Act and to the extension into the area of the enforcement of Canadian laws by the North West Mounted Police. In most other respects, the important trends noticed in the previous instalment continue: the officers of the Geological Survey of Canada and other scientists continued their careful and productive surveys; missionaries extended their efforts to remoter tribes; and sportsmen ranged still farther afield in search of big game. The number of expeditions each year steadily increased, and we are having to be increasingly selective in the ones we list. It has been impossible to include individual journeys to the Klondike, even of those persons who published narratives.


1894 ◽  
Vol 1 (9) ◽  
pp. 394-399 ◽  
Author(s):  
J. Burr Tyrrell

In the extreme northernmost part of Canada, lying between North Latitudes 56° and 68° and West Longitudes 88° and 112°, is an area of about 400,000 square miles, which had up to the past two years remained geologically unexplored.In 1892 the Director of the Geological Survey of Canada sent the writer to explore the country north of Churchill River, and south-west of Lake Athabasca;in1893 the exploration was continued northward, along the north shore of Athabasca Lake


Polar Record ◽  
1971 ◽  
Vol 15 (99) ◽  
pp. 893-920
Author(s):  
Alan Cooke ◽  
Clive Holland

During the period covered by this instalment of our list, the accomplishments of the North West Company, both in geographical exploration and in the realization of profits were great. It consolidated its position in the fur-rich Athabasca district and, with a few posts along Mackenzie River, began to draw in the furs of that immense territory. Its traders invaded not only the western part of Rupert's Land but even Hudson Bay itself. The Hudson's Bay Company rose only slowly to the challenge of its formidable rival, but, gradually, it began to adopt new policies and new techniques and to meet the North West Company on its own grounds and on its own terms. Finally, after a bitter struggle that was almost the destruction of both companies, the Hudson's Bay Company, in 1821, effectively absorbed the North West Company in a coalition that gave the older company greater strength than ever and a wider monopoly than Prince Rupert had thought of.


2020 ◽  
Author(s):  
Ashley Rudy ◽  
Steve Kokelj ◽  
Alice Wilson ◽  
Tim Ensom ◽  
Peter Morse ◽  
...  

<p>The Beaufort Delta region in Northwest Territories, Canada is one of the most rapidly warming areas on Earth. Permafrost thaw and climate change are major stressors on northern infrastructure, particularly in this region which hosts the highest density of Arctic communities and the longest road network constructed on ice-rich permafrost in Canada. The Dempster and Inuvik to Tuktoyaktuk Highways (ITH) comprise a 400-km corridor connecting the region with southern Canada. The corridor delivers a unique opportunity to develop a societally-relevant, northern-driven permafrost research network to encourage collaboration, and support pure and applied studies that engage stakeholders, encourage community participation, and acknowledge northern interests. Successful implementation requires leadership and institutional support from the Government of the Northwest Territories (GNWT) and Inuvialuit and Gwich’in Boards and landowners, and coordination between research organizations including NWT Geological Survey, Aurora Research Institute, Geological Survey of Canada, and universities to define key research priorities, human and financial resources to undertake studies, and protocols to manage data collection and reporting.</p><p>In 2017, a state of the art ground temperature monitoring network was established along the Dempster-ITH corridor by the GNWT in collaboration with Federal and Academic partners. This network in combination with the maintenance of the Dempster Highway and recent design and construction of the ITH, has created a national legacy of permafrost geotechnical, terrain and geohazard information in this region. The objectives of this program are to integrate old and new data to synthesize physiographic, hydrological, thermal, and geotechnical conditions along the corridor, and to develop applied permafrost research projects that support planning and maintenance of this critical northern infrastructure. In this presentation, we highlight: 1) a collaborative research framework that builds northern capacity and involves northerners in the generation of knowledge and its application to increase community based permafrost monitoring; 2) summaries of existing infrastructure datasets and their foundation for research; and 3) new projects that address emerging climate-driven infrastructure stressors. As the effects of climate change on permafrost environments, infrastructure and communities continue to increase, the need for northern scientific capacity and applied research to support informed decision-making, climate change adaptation and risk management will become increasingly critical. The development of resilient researcher-stakeholder-community relationships is also necessary for the scientific and research initiatives to reach their potential.</p><p> </p>


ARCTIC ◽  
1965 ◽  
Vol 18 (2) ◽  
pp. 146
Author(s):  
A.R. Byers

James Buckland Mawdsley, M.B.E., Ph.D., F.R.S.C., a Charter Associate of the Arctic Institute of North America, died very suddenly on 3 December 1964 at the age of 70. As Director of the Institute for Northern Studies, University of Saskatchewan, he played a major role in its organization and development and exerted a very great influence on research in northern Canada. He was born on 22 July 1894 near Siena, Italy, the son of British-American parents. In 1904 the Mawdsley family left Italy and settled in the village of Gainsborough, southeastern Saskatchewan. After receiving his public and high school training in Saskatchewan he entered McGill University in 1913. His career, like that of many of his contemporaries, was interrupted by the First World War. Twice wounded in France, first with the Princess Patricia Canadian Light Infantry and then as a pilot with the Royal Flying Corps, he was awarded the M.B.E. at the end of the war. In 1919 he returned to McGill and two years later graduated in Mining Engineering. He then went to Princeton University where he obtained his Doctor of Philosophy degree in Geology in 1924. That same year he joined the Geological Survey of Canada and for the next five years applied his scientific knowledge to the problems of the regional geology of northwestern Quebec. A new chapter in his life began in 1929 when he accepted the appointment of professor and head of the Department of Geology at the University of Saskatchewan, a position he held until he became Dean of Engineering in 1961 and also the Director of the Institute for Northern Studies. In 1963 he retired as Dean and was then able to devote all his time to the affairs of the Institute. In addition to his academic duties his professional activities included field work in northern Saskatchewan for the Geological Survey of Canada and the Saskatchewan Department of Mineral Resources, and private consulting assignments took him to other parts of northern Canada, to the United States and Great Britain. He was the author of 51 scientific papers and his honours were many. He was elected a Fellow of the Royal Society of Canada in 1933 and was chairman of Section IV for the year 1954-55. He was president of the Geological Association of Canada during 1955-56 and of the Canadian Institute of Mining and Metallurgy for 1961-62. In 1953 he was awarded the Institute's Barlow Memorial Medal in recognition of his paper entitled "Uraninite-bearing deposits, Charlebois Lake area, northeastern Saskatchewan". He was a Fellow and Director of the Royal Canadian Geographical Society, a Fellow of the Geological Society of America, a member of the Society of Economic Geologists, the Engineering Institute of Canada, and the Association of Professional Engineers of Saskatchewan. He had an eventful life, travelled widely, met and was a friend to many people. Such qualities as tact, kindliness, sincerity and respect for the thoughts of others enabled him to present his views without arousing undue antagonism, and to cooperate with others in reaching decisions. Recognized as an able administrator, scientist, and teacher, perhaps his greatest service will prove to be the influence he had on those who worked or studied under him. In them he not only instilled a feeling of scientific curiosity but also a keen interest and love of the North.


Polar Record ◽  
1965 ◽  
Vol 12 (81) ◽  
pp. 683-702
Author(s):  
Amil Dubnie ◽  
W. Keith Buck

For the purpose of this paper, northern Canada comprises all the territory north of lat 60° N. Included in this area of approximately 1500000 square miles are all of Yukon and Northwest Territories and small parts of Quebec and Labrador. Although the area is clearly defined by latitude, the subject matter of this paper also takes into account those developments farther south which have a direct effect upon the north.


Polar Record ◽  
1971 ◽  
Vol 15 (98) ◽  
pp. 699-721
Author(s):  
Alan Cooke ◽  
Clive Holland

If the Treaty of Paris in 1763 secured the Hudson's Bay Company in its monopoly of Rupert's Land, it also, by the Cession of Canada, opened to British enterprise the river-and-lake routes, discovered by the French, from Montreal to the fur-rich country west of Hudson Bay. This instalment of our list covers the years of the Montreal traders' expansion into the North-west, their crossing of the Arctic watershed into the fur trader's Eldorado, the Athabasca district, their organization into the Hudson's Bay Company's formidable rival, the North West Company, and concludes with the climax of their north-westward surge, Alexander Mackenzie's arrival at the Arctic Ocean in 1789. This activity obliged the Hudson's Bay Company to change its policy of waiting for the Indians to bring their furs to posts on Hudson Bay and made them push inland to compete for furs with the pedlars from Montreal. In the meantime, the Moravians had established missions on the coast of Labrador, searches for a North-west Passage were directed away from Hudson Bay to the Pacific coast of North America, the first scientific expedition was sent to Hudson Bay, and the Indians were decimated by smallpox. Toward the end of this instalment, we begin to draw our southern boundary of “northern Canada” both westward and northward and to omit many expeditions and events of peripheral or minor importance, such as activities south of Saskatchewan River, or of regular occurrence, such as annual voyages northward from Churchill.


Polar Record ◽  
1982 ◽  
Vol 21 (131) ◽  
pp. 117-125 ◽  
Author(s):  
Bernard W. Funston

‘No scheme of Canadian historiography yet advanced is wholly satisfactory because none as yet takes account of the occurrence of the North’ (Morton, 1970, p 31). Where Canadian historiography has been silent, studies of Canadian federalism have chosen to ignore. The Northwest Territories (NWT) and die Yukon Territory have certainly never been major actors in national political forums, nor have they yet to play a significant role in the political processes surrounding the two major preoccupations of Canadian federalism, namely the economy and national unity.


Polar Record ◽  
1970 ◽  
Vol 15 (95) ◽  
pp. 151-166 ◽  

Northern Canada consists of two political subdivisions. Yukon Territory and the Northwest Territories. Some 3.8 million km2 of land and the large continental shelf lie north of lat 60°N, which is the southern boundary of the two territories. The land area comprises 40 per cent of the whole of Canada. Distances are great, topography varies from flat plains and muskeg to high mountains, and variations in temperature are extreme. Nevertheless, despite these difficulties, the north is a land of great change and rapid development, particularly in the field of mineral exploitation. It was once considered that these territories were destined to remain a producer of precious metals only—commodities of high unit value. The turning point in mining developments came in November 1964, when the first shipment of ore from the Pine Point lead-zinc deposits marked the start of the tremendous and continuing surge forward in mining development. The oil and gas industry has also shown a keen interest in the potential of northern Canada in recent years and the sedimentary basins are all but covered with oil and gas exploration permits. A significant gas strike has been made in the Arctic archipelago and, far away in the south-west corner of the Northwest Territories, a major gas pool is being developed in the Pointed Mountain area.


1980 ◽  
Vol 58 (18) ◽  
pp. 1947-1985 ◽  
Author(s):  
Charles D. Bird ◽  
John W. Thomson ◽  
Alfred H. Marsh ◽  
George W. Scotter ◽  
Pak Yau Wong

The distribution and general ecology of 249 macrolichen taxa is described for 230 000 km2 of coniferous forest, open fens, and alpine terrain along the Mackenzie River in the District of Mackenzie, Northwest Territories, and the Peel River, a major tributary which rises in the Yukon Territory. Permafrost plays a major role in determining the plant communities that are present. Fire and man-made disturbances initiate succession. There are 45 new reports for the District of Mackenzie and 30 for the Yukon. Of the taxa, 86% are found in Europe, Asia, and North America, 9% are known from Asia and North America, whereas only 4% are restricted to North America. Pilophorus robustus is new to Canada. High mountains in the western part of the area, generally nonglaciated during the Wisconsinian, support a flora that contains many Arctic and Arctic–Alpine taxa. Amphi-Beringian species occur primarily in the north.


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