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Mount Sinclair
Mount Sinclair is a mountain in British Columbia, Canada. Description Mount Sinclair is located north of Radium Hot Springs, British Columbia, Radium Hot Springs in Kootenay National Park. The peak is the third-highest point of the Stanford Range which is a subrange of the Canadian Rockies. Precipitation runoff from this mountain's east slope drains to the Kootenay River, whereas the west slope drains to the Columbia River via Sinclair Creek. Topographic relief is significant with the summit rising over 1,400 metres (4,593 ft) above Sinclair Creek in . The nearest higher peak is Mount Kindersley to the north-northwest. Mount Sinclair is named after James Sinclair (fur trader), James Sinclair (1811–1856), a trader and explorer with the Hudson's Bay Company. In 1841, Sinclair travelled through nearby Sinclair Pass while leading an expedition consisting of 121 people from 23 Métis in Canada, Métis families from Red River Colony.George Simpson, ''An Overland Journey R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Sinclair (fur Trader)
James Sinclair (1811 – March 26, 1856) was a trader and explorer with the Hudson's Bay Company (HBC). He twice led large parties of settlers from the Red River Colony to the Columbia River valley. These were both authorized by the HBC as a part of grandiose plans to strengthen British claims in the Oregon boundary dispute. Early life James Sinclair was born in 1811 in Rupert's Land. His mother was a Cree woman named Nahovway, his father was William Sinclair, a HBC factor (agent), factor from Eastaquoy in Harray, and his brother was William Sinclair (fur trader), William Sinclair Jr. He was educated in Scotland at the University of Edinburgh. Red River colonists James Sinclair was appointed by Duncan Finlayson to guide the settler families to Fort Vancouver on the Columbia River. Most of the families were of mixed race; sons and daughters of Scotish or French fur trappers and their native wives.Métis people (Canada), Métis. The expedition was headed by men who were capable ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Columbia River
The Columbia River (Upper Chinook language, Upper Chinook: ' or '; Sahaptin language, Sahaptin: ''Nch’i-Wàna'' or ''Nchi wana''; Sinixt dialect'' '') is the largest river in the Pacific Northwest region of North America. The river headwater, forms in the Rocky Mountains of British Columbia, Canada. It flows northwest and then south into the U.S. state of Washington, then turns west to form most of the border between Washington and the state of Oregon before emptying into the Pacific Ocean. The river is long, and its largest tributary is the Snake River. Columbia River drainage basin, Its drainage basin is roughly the size of France and extends into seven states of the United States and one Canadian province. The fourth-largest river in the United States by River flow, flow, the Columbia has the greatest flow of any river into the eastern Pacific. The Columbia and its tributaries have been central to the region's culture and economy for thousands of years. They have been use ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banff–Windermere Highway
The Banff–Windermere Highway, also known as the Banff-Windermere Parkway, is a highway which runs through the Canadian Rockies in British Columbia and Alberta in Canada. It runs from Radium Hot Springs, British Columbia to Castle Junction, Alberta (midway between Banff and Lake Louise), passing through Kootenay National Park and Banff National Park. It is designated as part of British Columbia Highway 93 and Alberta Highway 93. Route description The Banff–Windermere Highway begins at British Columbia Highway 95 in village of Radium Hot Springs at the north end of the Highway 93/95 concurrency, approximately north of Windermere Lake where the highway gains its name. The highway passes through the village, passing numerous tourist services, overlooking Sinclair Creek. Approximately northeast of Highway 95, it enters Kootenay National Park, passing through the park gates. It continues through Sinclair Canyon and the Radium Hot Springs pools before passing through a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of British Columbia
The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of the different types and ages of rock hint at the complex geology, which is still undergoing revision despite a century of exploration and mapping. The province's most prominent geological features are its mountain ranges, including the North American Cordillera which stretches from Southern Mexico to Alaska. Terrane theory Terrane theory was first proposed by Jim Monger of the Geological Survey of Canada and Charlie Rouse in 1971 as an explanation for a set of fusulinid fossils that were found in central British Columbia. Rather than suggest that facies changes or seaways were behind this (which were common explanations at the time), the two geologists proposed that the fossils in question had been part of an assemblage of rocks that had migrated across the Pacific Ocean to their present location. This theor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of British Columbia
British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a continental climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates. Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada. History It was created in December 1897, by Order in Council, as the Geographic Board of Canada. It consisted of one Board member from each of four Government of Canada departments, as well as the Surveyor General of Dominion Lands, while a secretariat was provided by the then-extant Department of the Interior. In December 1899, the Order in Council was amended to give the Canadian provinces and territories the right to nominate one official, each, to be a Board member. The board was succeeded by the Canadian Board on Geographic Names in 1948, then reorganized as the Canadian Permanent Committee on Geographic Names (CPCGN) in 1961. Structure , the Board consists of 27 members, one from each of the provinces and territories, and ot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Red River Colony
The Red River Colony (or Selkirk Settlement), also known as Assiniboia, was a colonization project set up in 1811 by Thomas Douglas, 5th Earl of Selkirk, on of land in British North America. This land was granted to Douglas by the Hudson's Bay Company in the Selkirk Concession. It included portions of Rupert's Land, or the watershed of Hudson Bay, bounded on the north by the line of 52° N latitude roughly from the Assiniboine River east to Lake Winnipegosis. It then formed a line of 52° 30′ N latitude from Lake Winnipegosis to Lake Winnipeg, and by the Winnipeg River, Lake of the Woods and Rainy River (Minnesota–Ontario), Rainy River. West of the Selkirk Concession, it is roughly formed by the current boundary between Saskatchewan and Manitoba. These covered portions consisted of present-day southern Manitoba, northern Minnesota, and eastern North Dakota, in addition to small parts of eastern Saskatchewan, northwestern Ontario, and northeastern South Dakota. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Métis In Canada
The Métis ( , , , ) are a mixed-race Indigenous people whose historical homelands include Canada's three Prairie Provinces extending into parts of Ontario, British Columbia, the Northwest Territories and the northwest United States. They have a shared history and culture, deriving from specific mixed European (primarily French, Scottish, and English) and Indigenous ancestry (primarily Cree with strong kinship to Cree people and communities), which became distinct through ethnogenesis by the mid-18th century, during the early years of the North American fur trade. In Canada, the Métis, with a population of 624,220 as of 2021, are one of three legally recognized Indigenous peoples in the ''Constitution Act, 1982'', along with the First Nations and Inuit. The term ''Métis'' (uppercase 'M') typically refers to the specific community of people defined as the Métis Nation, which originated largely in the Red River Valley and organized politically in the 19th century, radiating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinclair Pass
Sinclair Pass (el. ) is a high mountain pass in Kootenay National Park between the Columbia and Kootenay Rivers to the northeast of present-day Radium Hot Springs in the province of British Columbia, Canada. History It was named after James Sinclair, a fur trading merchant from Red River colony. In 1841, under the guidance of Cree chief Maskepetoon, Sinclair travelled through the pass while leading an expedition consisting of 121 people from 23 Métis families from Red River Colony. They were hired by the Pugets Sound Agricultural Company to settle outside Cowlitz Farm and Fort Nisqually in modern Washington state. This was an attempt to get the northern bank of the Columbia River awarded to the United Kingdom of Great Britain and Ireland in any potential settlement in the Oregon boundary dispute. See also *List of mountain passes This is a list of mountain passes. Africa Egypt * Halfaya Pass (near Libya) Lesotho * Moteng Pass * Mahlasela pass * Sani Pass Morocco * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Kindersley
Mount Kindersley is a mountain in British Columbia, Canada. Description Mount Kindersley is located north of Radium Hot Springs in Kootenay National Park. The peak is the second-highest point of the Brisco Range which is a subrange of the Canadian Rockies. Precipitation runoff from this mountain's east slope drains to the Kootenay River via Nixon and Meadow creeks, whereas the west slope drains to the Columbia River via Kindersley Creek. Topographic relief is significant with the summit rising 1,100 metres (3,609 ft) above Kindersley Creek in . The mountain is named after Sir Robert Kindersley (1871–1954), who toured Canada in 1920. Kindersley was Governor (Company Chairman) of the Hudson's Bay Company from 1915 to 1925. The mountain's toponym was officially adopted September 9, 1924, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Mount Kindersley is located in a subarctic climate zone with cold, snowy winters, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
