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Mount Hungabee
Mount Hungabee, officially Hungabee Mountain, is a mountain located on the boundaries of Banff National Park and Yoho National Park on the Continental Divide at the head of Paradise Valley, in Canada. The peak was named in 1894 by Samuel Allen after the Stoney Indian (also known as Nakoda) word for "chieftain" as the mountain is higher than its neighbouring peaks. The mountain can be seen from the Icefields Parkway (#93) in the upper Bow Valley. Climbing ;History Mt. Hungabee was first climbed in 1903 by H.C. Parker who was guided by Hans Kaufmann and Christian Kaufmann. ;Routes The normal climbing route is via the west ridge (III 5.4) which features route finding challenges. Early summer is not recommended due to avalanche hazard from snow on the NW face. Geology Mount Hungabee 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 Lar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow Range
The Bow Range is a mountain range of the Canadian Rockies in Alberta and British Columbia, Canada. The range is named in associated with the Bow River and was officially adopted on March 31, 1917 by the Geographic Board of Canada. It is a part of the Banff- Lake Louise Core Area of the Southern Continental Ranges, located on the Continental Divide, west of the Bow River valley, in Banff National Park and Kootenay National Park. The Bow Range covers a surface area of 717 km2 (277 mi2), has a length of 34 km (from north to south) and a maximum width of 43 km. The highest peak is Mount Temple, with an elevation of . The range also covers the Valley of the Ten Peaks, with the tallest of the ten being Mount Hungabee at 3492 metres. The range also has hiking areas such as the Consolation Lakes, Sentinel Pass-Larch Valley, Wenkchenma Pass-Eiffel Lake, the Beehive plain of the Six Glaciers system and Saddle Back Pass. __NOTOC__ Peaks and mountains See also * R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christian Kaufmann (alpine Guide)
Christian Kaufmann (March 7, 1872 – January 12, 1939) was a Swiss mountain guide who climbed in the Alps, the Canadian Rockies, the Selkirk Mountains, Selkirks, the Himalayas, and List of mountains in Norway by height, Norway, accomplishing several dozen first-ascents. Family and early life (1872–1892) Christian (a.k.a. Christen) was born on March 7, 1872, in Grindelwald to Peter Kaufmann (1832-1903) and Margaretha (née Baumann, 1839-1903). His father, called ''Graben-Peter'' or ''Grabi-Peter'', was a well-established certified mountain guide during the Golden age of alpinism, Golden Age of Alpinism. Christian was the eleventh of seventeen children in the family. His brother Friedrich (Fritz) Kaufmann (born 1878), brothers Rudolf (born 1875) and Hans Kaufmann (alpine guide), Hans (Johann) Kaufmann (1875-1930) as well as his half-brother Peter Kaufmann (Alpine guide), Peter Kaufmann (1858-1924) all became mountain guides. From an early age, Christian and his brothers tend ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borders Of Alberta
A border is a geographical boundary. Border, borders, The Border or The Borders may also refer to: Arts, entertainment and media Film and television * ''Border'' (1997 film), an Indian Hindi-language war film * ''Border'' (2018 Swedish film), a fantasy film * ''Border'' (2018 Bhojpuri film), a war film * ''The Border'' (1982 film), an American drama * ''The Border'' (1996 film), an Italian war drama * ''The Border'' (2007 film), a Finnish-Russian war drama * ''The Border'' (2009 film), a Slovak documentary * ''The Border'' (TV series) a 2008–10 Canadian drama series Literature * "The Border", a 2004 short story by Richard Harland * "The Border", a 2019 novel by Don Winslow Music * "Border" (song), by Years & Years, 2015 * "Borders" (Feeder song), 2012 * "Borders" (M.I.A. song), 2015 * "Borders" (The Sunshine Underground song), 2007 * ''The Border'', soundtrack to the 1982 film, by Ry Cooder * "The Border" (America song), 1983 * "The Border" (Mr. Mister song), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borders Of British Columbia
A border is a geographical boundary. Border, borders, The Border or The Borders may also refer to: Arts, entertainment and media Film and television * ''Border'' (1997 film), an Indian Hindi-language war film * ''Border'' (2018 Swedish film), a fantasy film * ''Border'' (2018 Bhojpuri film), a war film * ''The Border'' (1982 film), an American drama * ''The Border'' (1996 film), an Italian war drama * ''The Border'' (2007 film), a Finnish-Russian war drama * ''The Border'' (2009 film), a Slovak documentary * ''The Border'' (TV series) a 2008–10 Canadian drama series Literature * "The Border", a 2004 short story by Richard Harland * "The Border", a 2019 novel by Don Winslow Music * "Border" (song), by Years & Years, 2015 * "Borders" (Feeder song), 2012 * "Borders" (M.I.A. song), 2015 * "Borders" (The Sunshine Underground song), 2007 * ''The Border'', soundtrack to the 1982 film, by Ry Cooder * "The Border" (America song), 1983 * "The Border" (Mr. Mister song), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Yoho National Park
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of British Columbia
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of Alberta
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Banff National Park
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Peaks On The Alberta–British Columbia Border
This is a list of peaks on the Alberta–British Columbia border, being the spine of the Continental Divide from the Canada–United States border to the 120th meridian, which is where the boundary departs the Continental Divide and goes due north to the 60th parallel. Peaks are listed from north to south and include the four peaks not on the Continental Divide but which are on the 120th Meridian, stretching approximately due north from Intersection Mountain, which as its name implies is located at the intersection of the Divide and the Meridian. See also *List of Boundary Peaks of the Alaska-British Columbia/Yukon border *Extreme points of British Columbia References {{DEFAULTSORT:List Of Peaks On The British Columbia-Alberta Border * * Peaks Peaks Peak or The Peak may refer to: Basic meanings Geology * Mountain peak ** Pyramidal peak, a mountaintop that has been sculpted by erosion to form a point Mathematics * Peak hour or rush hour, in traffic conges ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a 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° to 70°N, poleward of the humid continental climates. 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 one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. 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'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laramide Orogeny
The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 70 to 80 million years ago, and ended 35 to 55 million years ago. The exact duration and ages of beginning and end of the orogeny are in dispute. The Laramide orogeny occurred in a series of pulses, with quiescent phases intervening. The major feature that was created by this orogeny was deep-seated, thick-skinned deformation, with evidence of this orogeny found from Canada to northern Mexico, with the easternmost extent of the mountain-building represented by the Black Hills of South Dakota. The phenomenon is named for the Laramie Mountains of eastern Wyoming. The Laramide orogeny is sometimes confused with the Sevier orogeny, which partially overlapped in time and space. The orogeny is commonly attributed to events off the west coast of North America, where the Kula Plate, Kula and Farallon Plates were sliding under the North American plate. Most hypothes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
