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Mount Foch
Mount Foch is a mountain summit located on the border of Alberta and British Columbia on the Continental Divide. It was named in 1918 after Marshall Ferdinand Foch. The first ascent of the mountain was made in 1930 by Kate (Katie) Gardiner and Walter Feuz. The duo also made the first ascents of nearby Mount Sarrail and Mount Lyautey that same year. __NOTOC__ Geology Mount Foch 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, Mount Foch 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. In terms of favorable weather, June through September are the best months to climb Mount Foch. See also * List of peaks on the British Columbia–Alberta border A ''list'' is any ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Park Ranges
The Park Ranges, also known as the Main Ranges, are a group of mountain ranges in the Canadian Rockies of southeastern British Columbia and southwestern Alberta, Canada. It is one of the three main subranges and the most central of the Continental Ranges, extending from southeast of Mount McGregor to the Fernie Basin. Subranges * Blackwater Range *Blue Range *Bow Range *Chaba Icefield * Clemenceau-Chaba *Columbia Icefield * Drummond Group *Freshfields * Harrison Group *Hooker Icefield *Kitchen Range * Le Grand Brazeau * McKale-Chalco Divide *Mitchell Range *Morkill Ranges *Ottertail Range * Rainbow Range *Royal Group * Selwyn Range *Spray Mountains *Sundance Range * The Ramparts *Trident Range *Van Horne Range * Vermilion Range *Wapta Icefield *Waputik Icefield *Waputik Mountains **President Range *Winston Churchill Range The Winston Churchill Range is a mountain range in the central section of the Park Ranges of the Canadian Rockies located in Jasper National Park. The range ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Sarrail
Mount Sarrail is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Sarrail is situated 1.0 kilometre north of the Continental Divide, within Peter Lougheed Provincial Park. Its nearest higher peak is Mount Foch, to the southeast. Mount Sarrail can be seen from Upper Kananaskis Lake and Alberta Highway 40. History The mountain was named in 1918 for General Maurice Sarrail (1856-1929), the commander of the French Third Army in World War I. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1930 by Kate (Katie) Gardiner and Walter Feuz. The duo also made the first ascents of nearby Mount Foch and Mount Lyautey that same year. Geology Mount Sarrail 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 Laramid ... [...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, Andes) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Peaks On The British Columbia–Alberta Border
A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby union club Other uses * Angle of list, the leaning to either port or starboard of a ship * List (information), an ordered collection of pieces of information ** List (abstract data type), a method to organize data in computer science * List on Sylt, previously called List, the northernmost village in Germany, on the island of Sylt * ''List'', an alternative term for ''roll'' in flight dynamics * To ''list'' a building, etc., in the UK it means to designate it a listed building that may not be altered without permission * Lists (jousting), the barriers used to designate the tournament area where medieval knights jousted * ''The Book of Lists'', an American series of books with unusual lists See also * The List (other) * Listing ( ... [...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 a ... [...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'' i ... [...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 and Farallon Plates were sliding under the North American plate. Most hypotheses propose ... [...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] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fos ... [...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 precipita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Lyautey
Mount Lyautey is a mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. Mount Lyautey is situated 2.0 kilometres east of the Continental Divide, within Peter Lougheed Provincial Park. Its nearest higher peak is Mount Joffre, to the south. Mount Lyautey can be seen from Upper Kananaskis Lake and Alberta Highway 40. History The mountain was named in 1918 for General Louis Hubert Gonzalve Lyautey (1854–1934), a French Army officer and Marshal of France in 1921. The mountain's name became official in 1924 by the Geographical Names Board of Canada. The first ascent of the mountain was made in 1930 by Kate (Katie) Gardiner and Walter Feuz. The duo also made the first ascents of nearby Mount Sarrail and Warrior Mountain that same year. Geology Mount Lyautey is primarily composed of limestone, which is a sedimentary rock that was laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kate Gardiner
Kate Gardiner (21 September 1885–29 January 1974) was a New Zealand mountaineer. She was born in Wavertree, Liverpool, Lancashire, England on 21 September 1885. She was the daughter of Frederick Gardiner who made the first ascent of Mount Elbrus. In 1930 she made first ascents with her guide Walter Feuz in the Canadian Rockies of Mount Lyautey, Mount Sarrail, Mount Foch, Mount Bogart, Warrior Mountain, and Mount Galatea. Other notable first ascents include Mount Prince Henry (1919), Mount Alcantara Mount Alcantara is a mountain summit located in British Columbia, Canada. Description Mount Alcantara is the highest point in the Blue Range, a subrange of the Canadian Rockies. This remote peak is situated west of the Continental Divide and s ... (1929), Foster Peak (1933), and White Pyramid (1939). She would eventually complete 33 first ascents in the Canadian Rockies. References External linksHistory of Gardiner Hut 1885 births 1974 deaths New Zealand mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
