Mount Carnarvon
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Mount Carnarvon
Mount Carnarvon is a mountain summit located in the Kiwetinok River Valley of Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is The President (mountain), The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains. Mount Carnarvon is situated five kilometers northwest of Emerald Lake (British Columbia), Emerald Lake, but is hidden from view behind Emerald Peak (Yoho), Emerald Peak. However, Carnarvon is visible from Highway 1, the Trans-Canada Highway. The months July through September offer the most favorable weather for viewing or climbing Mount Carnarvon. History Originally known as ''Emerald Mountain'', the mountain was named in 1900 by Alexander MacKinnon Burgess (Commissioner of Public Lands) after Henry Herbert, 4th Earl of Carnarvon (1831-1890), who in 1867 authored the British North America Act 1867, British North America Act which conferred self-government on Can ...
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President Range
The President Range is a mountain range of the Canadian Rockies, located in the northwestern section of Yoho National Park. The range is named for the highest peak in the range, The President (mountain), The President. This range includes the following mountains and peaks: References

* Ranges of the Canadian Rockies Mountain ranges of British Columbia {{BritishColumbiaInterior-geo-stub ...
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Henry Herbert, 4th Earl Of Carnarvon
Henry Howard Molyneux Herbert, 4th Earl of Carnarvon, (24 June 1831 – 29 June 1890), known as Lord Porchester from 1833 to 1849, was a British politician and a leading member of the Conservative Party. He was twice Secretary of State for the Colonies and also served as Lord Lieutenant of Ireland. Origins Born at Grosvenor Square, London, Carnarvon was the eldest son and heir of Henry Herbert, 3rd Earl of Carnarvon (d.1849), by his wife Henrietta Anna Howard, a daughter of Lord Henry Howard-Molyneux-Howard, younger brother of Bernard Howard, 12th Duke of Norfolk. The Hon. Auberon Herbert was his younger brother. Youth He was educated at Eton College. In 1849, aged 18, he succeeded his father in the earldom. He attended Christ Church, Oxford, where his nickname was " Twitters", apparently on account of his nervous tics and twitchy behaviour, and where in 1852 he obtained a first in '' literae humaniores''. Early political career, 1854–66 Carnavon made his maiden speech i ...
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The Vice President
A vice president, also director in British English, is an officer in government or business who is below the president (chief executive officer) in rank. It can also refer to executive vice presidents, signifying that the vice president is on the executive branch of the government, university or company. The name comes from the Latin term ''vice'' meaning "in place of" and typically serves as ''pro tempore'' (Latin: ’for the time being’) to the president. In some countries, the vice president is called the ''deputy president''. In everyday speech, the abbreviation ''VP'' is used. In government In government, a vice president is a person whose primary responsibility is to act in place of the president on the event of the president's death, resignation or incapacity. Vice presidents are either elected jointly with the president as their running mate, or more rarely, appointed independently after the president's election. Most governments with vice presidents have one person ...
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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 ...
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Mount Carnarvon
Mount Carnarvon is a mountain summit located in the Kiwetinok River Valley of Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is The President (mountain), The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains. Mount Carnarvon is situated five kilometers northwest of Emerald Lake (British Columbia), Emerald Lake, but is hidden from view behind Emerald Peak (Yoho), Emerald Peak. However, Carnarvon is visible from Highway 1, the Trans-Canada Highway. The months July through September offer the most favorable weather for viewing or climbing Mount Carnarvon. History Originally known as ''Emerald Mountain'', the mountain was named in 1900 by Alexander MacKinnon Burgess (Commissioner of Public Lands) after Henry Herbert, 4th Earl of Carnarvon (1831-1890), who in 1867 authored the British North America Act 1867, British North America Act which conferred self-government on Can ...
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Kicking Horse River
The Kicking Horse River is in the Canadian Rockies of southeastern British Columbia, Canada. The river was named in 1858, when James Hector, a member of the Palliser Expedition, reported being kicked by his packhorse while exploring the river. Hector named the river and the associated pass as a result of the incident. The Kicking Horse Pass, which connects through the Rockies to the valley of the Bow River, was the route through the mountains subsequently taken by the Canadian Pacific Railway when it was constructed during the 1880s. The railway's Big Hill and associated Spiral Tunnels are in the Kicking Horse valley and were necessitated by the steep rate of descent of the river and its valley. Kicking Horse Pedestrian Bridge in Golden is the longest authentic covered timber-frame bridge in Canada. Planned as a community project by the Timber Framers Guild, local volunteers were joined by carpenters and timber framers from Canada, the United States and Europe. The bridge structu ...
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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 ...
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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 ...
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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 ...
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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 ...
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Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observation), Pa ...
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Dominion Land Survey
The Dominion Land Survey (DLS; french: links=no, arpentage des terres fédérales, ATF) is the method used to divide most of Western Canada into one-square-mile (2.6 km2) sections for agricultural and other purposes. It is based on the layout of the Public Land Survey System used in the United States, but has several differences. The DLS is the dominant survey method in the Prairie provinces, and it is also used in British Columbia along the Railway Belt (near the main line of the Canadian Pacific Railway), and in the Peace River Block in the northeast of the province. (Although British Columbia entered Confederation with control over its own lands, unlike the Northwest Territories and the Prairie provinces, British Columbia transferred these lands to the federal Government as a condition of the building of the Canadian Pacific Railway. The federal government then surveyed these areas under the DLS.)
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