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Whaleback Mountain
Whaleback Mountain is a summit in British Columbia, Canada. Description Whaleback Mountain is located in Yoho National Park, in the Waputik Mountains of the Canadian Rockies. Precipitation runoff from Whaleback drains into tributaries of the Yoho River which in turn is a tributary of the Kicking Horse River. Whaleback Mountain is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising 625 meters (2,050 ft) above Little Yoho River in . The peak is visible from Highway 1 (the Trans-Canada Highway). The nearest higher neighbor is Isolated Peak, to the northwest. History The mountain was named in 1901 by mountaineer Edward Whymper because the mountain's profile resembles the back of a whale. The mountain's descriptive name was then applied in 1916 by members of the Alberta-British Columbia Boundary Survey. The mountain's toponym was officially adopted on March 31, 1924, by the Geograp ... [...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 between Banff and Yoho National Park. Covering an area of , the range is located west of the Howse, Blaeberry and Amiskwi Rivers and east of the Bow and Mistaya Rivers and south to Kicking Horse Pass. Named in 1884 by George M. Dawson, "waputik" is the Stoney Indian word for white goat. Many of the highest peaks of the range are heavily glaciated as they sit within the 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 The Canadian Rockies are a segment of the North American Rocky Mountains found in the Canadian provinces of Alberta and British Columbia. List of ranges There is no universally accepted hierarchical division of the Canadian Rockies into subranges. ... References Mountain ranges of Alberta Mountain ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edward Whymper
Edward Whymper FRSE (27 April 184016 September 1911) was an English mountaineer, explorer, illustrator, and author best known for the first ascent of the Matterhorn in 1865. Four members of his climbing party were killed during the descent. Whymper also made important first ascents on the Mont Blanc massif and in the Pennine Alps, Chimborazo in South America, and the Canadian Rockies. His exploration of Greenland contributed an important advance to Arctic exploration. Whymper wrote several books on mountaineering, including '' Scrambles Amongst the Alps''. Early life Edward Whymper was born at Lambeth Terrace on Kennington Road in London on 27 April 1840 to the artist and wood engraver Josiah Wood Whymper and Elizabeth Whitworth Claridge. He was the second of eleven children, his older brother being the artist and explorer Frederick Whymper. He was trained to be a wood-engraver at an early age. In 1860, he made extensive forays into the central and western Alps to produce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Pollinger
Mount Pollinger is a summit in British Columbia, Canada. Description Mount Pollinger is located in the northern end of Yoho National Park, in the Waputik Mountains of the Canadian Rockies. Precipitation runoff from Pollinger drains west to the Amiskwi River, and east into Little Yoho River which in turn is a tributary of the Yoho River. Mount Pollinger is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 1,200 meters (3,937 ft) above the Amiskwi Valley in and 800 meters (2,625 ft) above Little Yoho River in . The Stanley Mitchell hut is east of the peak in the Little Yoho Valley, and the nearest higher neighbor is Kiwetinok Peak, to the southwest. History The first ascent of the mountain was made in 1901 by James Outram with guide Christian Kaufmann. Edward Whymper named this peak in 1901 for Joseph (Josef) Pollinger (1873–1943), an alpine guide from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The President (mountain)
The President is a mountain peak on ''The President/Vice-President Massif'' of the President Range, in eastern British Columbia. It is just north of Emerald Lake in Yoho National Park, near the Alpine Club of Canada's Stanley Mitchell hut. History The President was named ''Shaugnessy'' in 1904 by Edward Whymper after Thomas Shaugnessy, the president of the Canadian Pacific Railway. In 1907, the mountain was renamed by the Alpine Club of Canada, after it was discovered that the name had already been used on a mountain in the Selkirks. Climate Based on the 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, nota ..., The President is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trolltinder Mountain
Trolltinder Mountain is a mountain summit located immediately west of the Continental Divide, in the Waputik Range of the Canadian Rockies in British Columbia, Canada. It is situated in Yoho National Park, with its nearest higher peak being Mount Balfour, to the northeast, and Fairy Lake directly below its southern slope. History The mountain was named by Jean Habel in 1897 for its resemblance to a mountain in Norway. The translation is ''Witch's Peak''. Jean Habel was a German geographer who explored the Yoho Valley in 1896. The first ascent of the mountain was made in 1901 by James Outram and Edward Whymper, with guides Christian Kaufmann, Christian Klucker, and Joseph Pollinger. Outram described the climb in his book, ''"In the Heart of the Canadian Rockies"'' as follows: ''"On the 21st we had a little climb to a ruined tower on a serrated spur of Mt. Balfour, which had been called by Mr. Habel "Trolltinder," or the Witch's Peaks, after a famous and much pinnacled ridge ... [...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. Statis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whaleback Mountain Seen From Iceline Trail
] A whaleback was a type of cargo steamship of unusual design, with a hull that continuously curved above the waterline from vertical to horizontal. When fully loaded, only the rounded portion of the hull (the "whaleback" proper) could be seen above the waterline. With sides curved in towards the ends, it had a spoon bow and a very convex upper deck. It was formerly used on the Great Lakes of Canada and the United States, notably for carrying grain or ore. The sole surviving ship of the "whaleback" design is the , which is docked in Superior, Wisconsin as a museum ship. The term developed in common usage in response to the ship's appearance when fully loaded. A total of 44 such vessels were constructed from 1887 to 1898. All but two were built initially as lake freighters for service on the Great Lakes. Six were built at Duluth, Minnesota; 33 were built at West Superior, Wisconsin; 2 at Brooklyn, New York; one at Everett, Washington; and one at Sunderland, England. A number ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panorama Of Iceline Trail
A panorama (formed from Greek πᾶν "all" + ὅραμα "view") is any wide-angle view or representation of a physical space, whether in painting, drawing, photography, film, seismic images, or 3D modeling. The word was originally coined in the 18th century by the English (Irish descent) painter Robert Barker to describe his panoramic paintings of Edinburgh and London. The motion-picture term ''panning'' is derived from ''panorama''. A panoramic view is also purposed for multimedia, cross-scale applications to an outline overview (from a distance) along and across repositories. This so-called "cognitive panorama" is a panoramic view over, and a combination of, cognitive spaces used to capture the larger scale. History The device of the panorama existed in painting, particularly in murals, as early as 20 A.D., in those found in Pompeii, as a means of generating an immersive "panoptic" experience of a vista. Cartographic experiments during the Enlightenment era precede ... [...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] |
