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Mount Rundle
Mount Rundle is a mountain in Canada's Banff National Park overlooking the towns of Banff and Canmore, Alberta. The Cree name was ''Waskahigan Watchi'' or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s. He introduced syllabics there James Evans the supervisor of the Wesleyan missionaries in Rupert's Land who is credited with devising the Cree syllabics—a written language developed for the Cree, as part of his missionary work. He only visited the Stoney-Nakoda of the area around what is now called Mount Rundle in 1844 and 1847. Mt. Rundle could actually be considered a small mountain range as the mountain extends for over , on the south side of the Trans-Canada Highway eastward from Banff to Canmore with seven distinct peaks along the way. The third peak southeast of Banff is the highest at . West of the Spray Lakes road is the Eas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vermilion Lakes
The Vermilion Lakes are a series of lakes located immediately west of Banff, Alberta, in the Canadian Rocky Mountains. The three lakes are formed in the Bow River valley, in the Banff National Park, at the foot of Mount Norquay. They are located between the Trans-Canada Highway and the Canadian Pacific Railway tracks. A hot spring is found at the third lake. History Archeological evidence proves human activity around the lakes dating back 10,800 years. The site was excavated by Parks Canada's Daryl Fedje, - Ice Age Tools Found in Banff and found remains of campsites and obsidian tools. Activities Activities on and around the lakes include[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Evans (linguist)
James Evans (January 18, 1801 – November 23, 1846) was an English-Canadian Wesleyan Methodist missionary and amateur linguist. He is known for creating the "syllabic" writing system for Ojibwe and Cree, which was later adapted to other languages such as Inuktitut. Life Evans was born in Kingston-upon-Hull in England, but emigrated with his parents to Lower Canada in 1822, where he worked as a teacher. He later moved to Rice Lake and continued his teaching work. In 1833 he was ordained as a Wesleyan Methodist minister, and in 1840 he was given authority over the local district in Norway House in Manitoba. During this time Evans worked on the development of the Ojibwe and Cree scripts. Evans had picked up Ojibwe during his work among the people in Upper Canada. He created the Ojibwe script after first trying to apply a Roman script to their language. Later, he modified syllabics slightly and applied it to Cree, a related language. The syllabic writing system was inspired ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable bedding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (mineral)
Dolomite () is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite. An alternative name sometimes used for the dolomitic rock type is dolostone. History As stated by Nicolas-Théodore de Saussure the mineral dolomite was probably first described by Carl Linnaeus in 1768. In 1791, it was described as a rock by the French naturalist and geologist Déodat Gratet de Dolomieu (1750–1801), first in buildings of the old city of Rome, and later as samples collected in the mountains now known as the Dolomite Alps of northern Italy. Nicolas-Théodore de Saussure first named the mineral (after Dolomieu) in March 1792. Properties The mineral dolomite crystallizes in the trigonal-rhombohedral system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions. Unle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow Valley & River, Banff, Mount Rundle And Sulphur Mountain
Bow often refers to: * Bow and arrow, a weapon * Bowing, bending the upper body as a social gesture * An ornamental knot made of ribbon Bow may also refer to: * Bow (watercraft), the foremost part of a ship or boat * Bow (position), the rower seated in the bow of a racing shell Knots * Bow knot, a shoelace knot or a rosette * Bow tie, a type of necktie * Pussy bow, a style of neckwear Music * Bow (music), used to play a stringed instrument * Musical bow, a musical instrument resembling an archer's bow * EBow, electronic device for playing the electric guitar * Bows (band), a band from the UK Porcelain * Bow porcelain factory Places England * Bow, Devon, a village in mid Devon * Bow, a hamlet in the parish of Ashprington in South Devon * Bow, London, a district * Bow, Oxfordshire, a hamlet United States * Bow, Kentucky * Bow, New Hampshire * Bow, Washington Canada * The Bow (skyscraper), Calgary, Alberta * Bow River, Alberta Other * Bow (name), including a list of peo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goat Range (Kananaskis)
The Goat Range is a mountain range of the Canadian Rockies in southwestern Alberta, Canada. It is a part of the Front Ranges of the Southern Continental Ranges and lies on the western edge of Kananaskis Country, on the boundary between Spray Valley Provincial Park and Banff National Park. To the east, the Spray Lakes Reservoir separates the Goat Range from the Kananaskis Range, to the north-east, Goat Creek separates it from Mount Rundle, and to the south-west, the Spray River separates it from Sundance Range The Sundance Range is a mountain range in the Canadian Rockies, south of the town of Banff. It is located on the Continental Divide, which forms the boundary between British Columbia and Alberta Alberta ( ) is one of the thirteen provinces .... It covers an area of about 115 km², extending about 25 km in a NNW-SSE direction with a width ranging between 4 and 6 km. The highest peak is Old Goat Mountain (3109 m), located near the southern end of the range. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sulphur Mountain (Alberta)
Sulphur Mountain is a mountain in Banff National Park in the Canadian Rocky Mountains overlooking the town of Banff, Alberta, Canada. The mountain was named in 1916 for the hot springs on its lower slopes. George Dawson had referred to this landform as Terrace Mountain on his 1886 map of the area. Sanson's Peak was named in 1948 for Norman Bethune Sanson who diligently attended the observatory recording equipment atop Sulphur Mountain for nearly 30 years. Recreation Two hot springs have been commercially developed. The lowest is the Cave and Basin National Historic Site and the highest is the Banff Upper Hot Springs. A gondola on the eastern slope goes to the summit ridge which has an upper terminal containing three restaurants, a gift shop, and multiple observation decks. The summit ridge provides views both westward up and east down the Bow Valley. A boardwalk can be followed on the north side to the top of Sanson's Peak (). The original, and more scenic, summit acces ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sundance Range
The Sundance Range is a mountain range in the Canadian Rockies, south of the town of Banff. It is located on the Continental Divide, which forms the boundary between British Columbia and Alberta Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest T ... in this region. Mountains This range includes the following mountains and peaks: References Further reading * Jane G. Ferrigno, 'U.S. Geological Survey Professional Paper'', P 216 *Dave Birrell, '50 Roadside Panoramas in the Canadian Rockies'', P 81 Ranges of the Canadian Rockies Mountain ranges of Alberta Mountain ranges of British Columbia {{Alberta-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Winnie-the-Pooh
Winnie-the-Pooh, also called Pooh Bear and Pooh, is a fictional anthropomorphic teddy bear created by English author A. A. Milne and English illustrator E. H. Shepard. The first collection of stories about the character was the book ''Winnie-the-Pooh'' (1926), and this was followed by '' The House at Pooh Corner'' (1928). Milne also included a poem about the bear in the children's verse book ''When We Were Very Young'' (1924) and many more in '' Now We Are Six'' (1927). All four volumes were illustrated by E. H. Shepard. The Pooh stories have been translated into many languages, including Alexander Lenard's Latin translation, , which was first published in 1958, and, in 1960, became the only Latin book ever to have been featured on ''The New York Times'' Best Seller list. In 1961, Walt Disney Productions licensed certain film and other rights of Milne's Winnie-the-Pooh stories from the estate of A. A. Milne and the licensing agent Stephen Slesinger, Inc., and adapted th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East End Of Rundle
East End of Rundle (EEOR) is a mountain located immediately west of the town of Canmore, Alberta and immediately west of the Spray Lakes road in the Canadian Rockies. Mount Rundle occupies the space between Canmore and Banff on the southwest side of the Trans-Canada Highway. There is a scrambling route up from the Spray Lakes road. Geology The mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, the mountain is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Rundle drains into the Bow River which is a tributary of the Saskatchewan River. See also * List of mountains of Canada *Geography of Alberta Alberta is one o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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