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Trapper Peak (Canada)
Trapper Peak is a mountain in Alberta and British Columbia, Canada, located on their border along the Continental Divide in the Wapta Icefield. Trapper Peak has two summits, one accessible from Baker. Peyto Peak is located to the north-east. The peak was originally named in 1892 by Walter D. Wilcox to honor his guide, trapper Bill Peyto, and the first ascent was in 1933 by Conrad Kain and party. Geology Trapper Peak 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, Trapper Peak is located in a 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, g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waputik Mountains
The Waputik Mountains are a mountain range of the Canadian Rockies, located on the Continental Divide of the Americas, Continental Divide between Banff National Park, Banff and Yoho National Park. Covering an area of , the range is located west of the Howse River, Howse, Blaeberry River, Blaeberry and Amiskwi Rivers and east of the Bow River, Bow and Mistaya Rivers and south to Kicking Horse Pass. Named in 1884 by George Mercer Dawson, George M. Dawson, "waputik" is the Nakoda (Stoney), Stoney Indian word for Mountain goat, white goat. Many of the highest peaks of the range are heavily glaciated as they sit within the Waputik Icefield, Waputik and Wapta Icefields. The range is further divided into the President Range and Waputik Range This range includes the following mountains and peaks: See also * Ranges of the Canadian Rockies References Mountain ranges of Alberta Mountain ranges of British Columbia Ranges of the Canadian Rockies Ranges of the Rocky Mountains Al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...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] |
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] |
Two-thousanders Of British Columbia
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of Alberta
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
American Alpine Club
The American Alpine Club (AAC) is a non-profit member organization with more than 24,000 members. Its vision is to create "a united community of competent climbers and healthy climbing landscapes." The Club is housed in the American Mountaineering Center (AMC) in Golden, Colorado. Through its members, the AAC advocates for American climbers domestically and around the world; provides grants and volunteer opportunities to protect and conserve climbing areas; hosts local and national climbing festivals and events; cares for the nation's leading climbing library and mountaineering museum; manages the Hueco Rock Ranch, New River Gorge Campground, and Grand Teton Climbers' Ranch as part of a larger lodging network for climbers; and annually gives about $100,000 toward climbing, conservation, and research grants that fund adventurers who travel the world. It also maintains regional sections—with both regional staff and volunteers—throughout the United States. The AAC publishes two ... [...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] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
