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Ursus Minor Mountain
Ursus Minor Mountain is a mountain summit located in Glacier National Park, in the Hermit Range of the Selkirk Mountains in British Columbia, Canada. Ursus Minor Mountain is situated northeast of Revelstoke, and west of Golden. It is also set northwest of Cheops Mountain, and west of Rogers Pass. Its nearest higher peak is Grizzly Mountain, to the east-northeast. The first ascent of the mountain was made in 1907 by Rupert W. Haggen, with guide Edouard Feuz Jr. The mountain's name was adopted in 1906, then re-approved September 8, 1932, by the Geographical Names Board of Canada. It was so-named because of its proximity above Bear Creek (since renamed Connaught Creek), and in keeping with the bear theme of other nearby features such as Ursus Major Mountain, Grizzly Mountain, Bruins Pass, and Balu Pass. Climate Based on the Köppen climate classification, Ursus Minor Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hermit Range
A hermit, also known as an eremite (adjectival form: hermitic or eremitic) or solitary, is a person who lives in seclusion. Eremitism plays a role in a variety of religions. Description In Christianity, the term was originally applied to a Christian who lives the eremitic life out of a religious conviction, namely the Catholic spirituality#Desert spirituality, Desert Theology of the Old Testament (i.e., the 40 years wandering in the Zin Desert, desert that was meant to bring about a change of heart). In the Christian tradition the eremitic life is an early form of Monk, monastic living that preceded the monastic life in the cenobium. In chapter 1, the Rule of St Benedict lists hermits among four kinds of monks. In the Roman Catholic Church, in addition to hermits who are members of religious institutes, the Canon law (Catholic Church), Canon law (canon 603) recognizes also Consecrated life#Other forms of consecrated life, diocesan hermits under the direction of their diocesan b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rupert Haggen
Rupert Williams Haggen (July 29, 1887 – July 19, 1962) was a Canadian politician, who represented the electoral district of Grand Forks-Greenwood in the Legislative Assembly of British Columbia from 1949 to 1956. He had previously been an unsuccessful candidate in the electoral district of Cariboo in the 1933 provincial election and in the electoral district of Rossland-Trail in the 1945 provincial election. He was a member of the Co-operative Commonwealth Federation. He was born in New Zealand and came to Canada in 1901. Haggen finished his education, qualifying as an engineer and was hired by the Canadian Pacific Railway. From 1909 to 1934, he practised as a mining and civil engineer. He also was qualified as a Dominion and B.C. Land Surveyor and served as president of the B.C. Land Surveyors' Association. In 1935, he moved to the Kootenay region, settling in Rossland. Later, Haggen became a notary public, opening offices in Rossland, Grand Forks and Kelowna. He retire ... [...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] |
Ursus Minor Mountain And Grizzly Mountain
Ursus is Latin for bear. It may also refer to: Animals * ''Ursus'' (mammal), a genus of bears People * Ursus of Aosta, 6th-century evangelist * Ursus of Auxerre, 6th-century bishop * Ursus of Solothurn, 3rd-century martyr * Ursus (''praefectus urbi'') of Constantinople in 415-416 * Reimarus Ursus, an astronomer and imperial mathematician to Rudolf II * Ursus, a pen-name of Ambrose Bierce Fictional characters * Ursus, the bodyguard of Ligia, a minor character in the novel ''Quo Vadis'' * Ursus, a character in Victor Hugo's novel ''The Man Who Laughs'' * General Ursus (Planet of the Apes), a character in ''Beneath the Planet of the Apes'' * Ursus (film character), a character in a series of 1960s Italian adventure films Arts * ''Ursus'' (film), 1961 Italian film Science and technology * ''Ursus'' (journal), a scientific journal published by the International Association for Bear Research and Management * Ursus Factory, Polish manufacturer of heavy vehicles ** Ursus A, a se ... [...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] |
Beaver River (Columbia River Tributary)
The Beaver River, also known as the Beavermouth Creek or Beaver Creek, is a tributary of the Columbia River in British Columbia, Canada, joining that river in the Rocky Mountain Trench northwest of the town of Golden. It enters the Columbia via Kinbasket Lake. The Beaver River is the eastern egress from the Rogers Pass and its valley is the route of the Trans-Canada Highway and Canadian Pacific Railway on that side of the pass, and it is located in Glacier National Park. Its lower reaches are officially named Beaver Canyon. The pass between the Beaver River and the Duncan River forms the dividing line between the Selkirks and the Purcell Mountains. A semi-decommissioned hiking trail follows the Beaver from the Trans-Canada highway for much of its length, including now-abandoned spurs to Copperstain Pass and Glacier Circle. The trail no longer receives maintenance from Parks Canada, which closed remaining stream crossings in 2009. See also *List of tributaries of the Columbia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Illecillewaet River
The Illecillewaet River is a tributary of the Columbia River located in British Columbia, Canada. Fed by the Illecillewaet Glacier in Glacier National Park, the river flows approximately to the southwest,About the Illecillewaet Watershed , Columbia Mountains Institute where it flows into the north end of at Revelstoke. The river's is . History The Illecillewaet has been of impor ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...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] |
Baloo
Baloo (from hi, भालू ur, بھالو ''bhālū'' "bear") is a main fictional character featured in Rudyard Kipling's ''The Jungle Book'' from 1894 and ''The Second Jungle Book'' from 1895. Baloo, a sloth bear, is the strict teacher of the cubs of the Seeonee wolf pack. His most challenging pupil is the "man-cub" Mowgli. Baloo and Bagheera, a panther, save Mowgli from Shere Khan the tiger, and endeavor to teach Mowgli the Law of the Jungle in many of ''The Jungle Book'' stories. Name and species He is described in Kipling's work as "the sleepy brown bear". Robert Armitage Sterndale, from whom Kipling derived most of his knowledge of Indian fauna, used the Hindi word "''Bhalu''" for several bear species, though Daniel Karlin, who edited the Penguin reissue of ''The Jungle Book'' in 1987, states that, with the exception of colour, Kipling's descriptions of Baloo are consistent with the sloth bear, as brown bears and Asian black bears do not occur in the Seoni area where ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
