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History of Saskatchewan : ウィキペディア英語版
History of Saskatchewan

History of Saskatchewan encompasses the study of past human events and activities of the province of Saskatchewan, the middle of Canada's three prairie provinces. Archaeological studies give some clues as to the history and lifestyles of the Palaeo-Indian, Taltheilei, and Shield Archaic Traditions who were the first occupants of the prehistoric era of this geographical area. They evolved into the history of the first nations people who kept their history alive in oral tradition. The First Nation bands that were a part of this area were the Chipewyan, Cree, Saulteaux, Assiniboine, Atsina and Sioux.〔(Sask Gen Web SGW First Nations Saskatchewan Genealogy Roots ), URL accessed 26 November 2006〕
Henry Kelsey (1667–1724), was the first European (an Englishman) to visit this area, and arrived 1690.〔(Saskatchewan Gen Web Project – SGW – Canadian Migrations Saskatchewan Genealogy Roots ) URL accessed April 12, 2007〕 Other European explorers also soon arrived followed by fur traders such as The Governor and Company of Adventurers of England trading into Hudson's Bay (Hudson's Bay Company) and North West Company. Clifford Sifton, Minister of the Interior in charge of immigration, (1896–1905) induced a variety of agriculturally inclined European emigrants to Canada to settle prairie land around the transcontinental railway. The political boundaries of this area have changed several times evolving through Rupert's Land, Provisional Districts of the North West Territories, and finally a province. Saskatchewan has been a province of Canada since 1905.
==Natural history==
The history of this plains area actually began 2,000–2,100 million years ago wherein there were two continents separated by an ocean. The "Churchill Continent" which would be Manitoba and Saskatchewan, and the "Superior Continent" which would comprise Manitoba and Ontario. 1,830 – 1,800 million years ago these two land masses collided. The Northern shield area and western Rockies formed higher land from the collision.〔(TIME TUNNEL Royal Saskatchewan Museum ), URL accessed 26 November 2006〕
The lower lands of today's parkland were covered by a shallow sea even in the Palaeozoic Era. It was not until the Cretaceous Period
144 – 66 million years ago that the inland sea began to drain. Here we begin to find the paleontological artifacts of various dinosaur species. The ice age of the Quaternary Period totally again re-shaped and re-shifted the landscape of Saskatchewan, occurring 2 million years ago.〔
Following these geological changes to this area, and the formation of the continent of North America as we know it, pre-history to the history of contemporary day can begin.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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