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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] |
Robert Kindersley, 1st Baron Kindersley
Robert Molesworth Kindersley, 1st Baron Kindersley (21 November 1871 – 20 July 1954) was an England, English Businessperson, businessman, stockbroker, merchant banker, and public servant who organised the National Savings Movement. Background Kindersley was born in Wanstead, Essex, the son of Edward Nassau Molesworth Kindersley, of Sherborne, Dorset, and Ada Good, daughter of John Murray. His father was an Old Etonian and Oxford graduate from a wealthy family who had been a Captain (British Army and Royal Marines), captain in the Green Howards and the British Indian Army, Indian Army, but had fallen on hard times since resigning his commission and becoming a Pharmacist, chemist, working for Scott & Co. Chemical Works at Bow, London; he was also a director of the Anglo American Leather Cloth Company. Kindersley was educated at Repton School but was forced to leave in 1887 when his father could no longer afford the fees. Kindersley was the great-grandson of the civil servant and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Relief
Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Bathymetry is the study of underwater relief, while hypsometry studies terrain relative to sea level. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, drainage characteristics, drainage systems, groundwater systems, water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rocky Mountain Trench
The Rocky Mountain Trench, also known as the Valley of a Thousand Peaks or simply the Trench, is a large valley on the western side of the northern part of North America's Rocky Mountains. The Trench is both visually and cartographically a striking physiographic feature extending approximately from Flathead Lake, Montana, to the Liard River, just south of the British Columbia–Yukon border near Watson Lake, Yukon. The trench bottom is wide and is above sea level. The general orientation of the Trench is an almost straight 150/330° geographic north vector and has become convenient as a visual guide for aviators heading north or south. Although some of its topography has been carved into U-shaped glacial valleys, it is primarily a byproduct of geologic faulting. The Trench separates the Rocky Mountains on its east from the Columbia Mountains and the Cassiar Mountains on its west. It also skirts part of the McGregor Plateau area of the Nechako Plateau sub-area of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edgewater, British Columbia
Edgewater is an unincorporated hamlet located in the East Kootenay region of southeastern British Columbia with a population of 720 in 2021 and a population density of 70.4 people per square kilometre. It is along Highway 95 south of Golden and on the perimeter of Kootenay National Park. It was originally founded as a farming community in 1912. Many of its residents were from England, and returned there after the war, causing the community to suffer a decline in population. Edgewater has since recovered, and the area's economy includes forestry, agriculture, and tourism. Edgewater has couple of major attractions that draw travellers. The area around the community is farmland used for Christmas trees. During the summer, the Saturday Farmer's Market is where tourists can purchase arts and crafts, fresh produce and dairy products. Edgewater is also home to the Steamboat Mountain Music Festival in July. The community gets its name from being at the edge of the waters of the Colu ... [...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] |
Mount Harkin
Mount Harkin is a mountain summit located in the Kootenay River Valley along the eastern border of Kootenay National Park. Park visitors can see the peak from Highway 93, also known as the Banff–Windermere Highway. It is part of the Mitchell Range, which is a sub-range of the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Assiniboine, to the northeast. __NOTOC__ History The mountain was named in 1923 by Morrison P. Bridgland in honor of James Bernard Harkin (1875–1955), who was Canada's first National Parks commissioner from 1911 until 1936. Harkin established 11 new national parks and has been called the "Father of the National Parks of Canada." The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Bridgland (1878–1948) was a Dominion Land Surveyor who named many peaks in the Canadian Rockies. Geology Mount Harkin is composed principally of Ottertail limestone, a sedimentary rock laid down during t ... [...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] |
Robert Molesworth Kindersley 1924
The name Robert is an ancient Germanic given name, from Proto-Germanic "fame" and "bright" (''Hrōþiberhtaz''). Compare Old Dutch ''Robrecht'' and Old High German ''Hrodebert'' (a compound of '' Hruod'' () "fame, glory, honour, praise, renown, godlike" and ''berht'' "bright, light, shining"). It is the second most frequently used given name of ancient Germanic origin.Reaney & Wilson, 1997. ''Dictionary of English Surnames''. Oxford University Press. It is also in use as a surname. Another commonly used form of the name is Rupert. After becoming widely used in Continental Europe, the name entered England in its Old French form ''Robert'', where an Old English cognate form (''Hrēodbēorht'', ''Hrodberht'', ''Hrēodbēorð'', ''Hrœdbœrð'', ''Hrœdberð'', ''Hrōðberχtŕ'') had existed before the Norman Conquest. The feminine version is Roberta. The Italian, Portuguese, and Spanish form is Roberto. Robert is also a common name in many Germanic languages, including Eng ... [...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] |
