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Nub Peak
Nub Peak is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Nestor Peak, to the west. The mountain is situated north of Sunburst Peaks, with Elizabeth Lake and Cerulean Lake in between. The Continental Divide and Assiniboine Pass are situated to the east. Nub Peak is famous for its panoramic view of Mount Assiniboine with its surrounding lakes and peaks. The mountain's descriptive name was officially adopted in 1924. An arm extending southwest from Nub is officially known as Chucks Ridge, and an arm extending southeast is officially called Nublet. Nub Peak is composed of sedimentary rock laid down during the Cambrian period and pushed east over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Nub Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Assiniboine Provincial Park
Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. History The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). World Heritage Site In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils. Conservation The park aims to protect a large variety of species. Eighty-four species of birds inhabit the park environs, based on sightings. Co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sunburst Peaks
Sunburst Peaks is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Wedgwood Peak, to the south. The mountain is situated immediately southeast of Sunburst Lake, west of Lake Magog, and south of Cerulean Lake. History The first ascent of the peak was made in 1910 by Katherine Longstaff and her brother Dr. Tom Longstaff, with Rudolph Aemmer as their guide. The mountain was named Sunburst Peak in 1953 after Sunburst Lake, which had been named by the Interprovincial Boundary Survey. The name was officially changed by the Geographical Names Board of Canada to Sunburst Peaks (plural) on February 15, 1983 with the intention extended to apply to three peaks. Geology Sunburst Peak is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Nub Peak
Climbing is the activity of using one's hands, feet, or any other part of the body to ascend a steep topographical object that can range from the world's tallest mountains (e.g. the eight thousanders), to small boulders. Climbing is done for locomotion, sporting recreation, and for competition, and is also done in trades that rely on ascension; such as emergency rescue and military operations. Climbing is done indoors and outdoors and on natural (e.g. rock and ice) and artificial surfaces. Professional mountain guides or rock climbing guides (e.g. the UIAGM), were a significant element in developing the popularity of the sport in the natural environment, and remain so today. Since the 1980s, the development of competition climbing and the availability of artificial climbing walls have dramatically increased the popularity of rock climbing as a sport and led to the emergence of professional rock climbers, such as Wolfgang Güllich, Chris Sharma, Lynn Hill and Cath ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nub Peak Panorama
Nub or NUB may refer to: *Nub, an analog controller on Pandora and PlayStation Portable *ISO 639-2 code for the Nobiin language of Nubia *Northern University, Bangladesh * National University, Bangladesh *NUb, brand of Oliva Cigar Co. * National Union of Blastfurnacemen, Ore Miners, Coke Workers and Kindred Trades, former UK trades union *Nub, colloquialism for pointing stick on a laptop * Nahda University, Egypt Entertainment *Vernon, Florida (film), a 1981 film originally titled ''Nub City'' *NUB, female bodyguard organisation in novel ''Nobody Lives for Ever ''Nobody Lives for Ever'' (published in American editions as ''Nobody Lives Forever''), first published in 1986, was the fifth novel by John Gardner featuring Ian Fleming's secret agent, James Bond. Carrying the Glidrose Publications copyrigh ...'' *Nub, a song on Jesus Lizard's 1991 album '' Goat'' *Nub, guitarist from children's TV series '' Generation O!'' * Nub Kleinke (1911–1950), Major League Baseball play ... [...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 rock types and ages hint at the complex geology, which is still undergoing revision despite a century of exploration and mapping. The country's most prominent geological features are 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 found in central British Columbia. Rather than use facies changes or seaways (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 theory was then developed by Porter Irwin and Davy Jones of the US ... [...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. Statist ... [...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] |
Mount Assiniboine
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At , it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mount Assiniboine rises nearly above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mount Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mount Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of the Assiniboine people. Mount Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The mountain can be reached only by a six-hour hike or horse-pack , three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. Climbing Mt. Assiniboi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Divide Of The Americas
The Continental Divide of the Americas (also known as the Great Divide, the Western Divide or simply the Continental Divide; ) is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and (in northern North America) Arctic oceans (including those that drain into the Gulf of Mexico, the Caribbean Sea and Hudson Bay). Although there are many other hydrological divides in the Americas, the Continental Divide is by far the most prominent of these because it tends to follow a line of high peaks along the main ranges of the Rocky Mountains and Andes, at a generally much higher elevation than the other hydrological divisions. Geography Beginning at the westernmost point of the Americas’ mainland (Cape Prince of Wales, just south of the Arctic Circle), the Conti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
