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Hewitt Peak
Hewitt Peak is a mountain summit located on the western border of Kootenay National Park, in the Canadian Rockies of British Columbia, Canada. The peak is also known locally as Mammoth Peak, and originally as Mount 10060. The alternate names derive from its outline profile resembling a mammoth, and its elevation as measured in feet. No name for this mountain has been officially adopted yet. Its nearest higher peak is Tumbling Peak, to the north-northwest, and both are part of the Vermilion Range. Park visitors can catch a glimpse of the peak from Highway 93, also known as the Banff–Windermere Highway. History The first ascent of the mountain was made in 1906 by members of the Dominion Land Survey. It was first named Mount 10060 by Kate Gardiner and party in 1933, when they climbed nearby Foster Peak and Mount 10240 (now known as Tumbling Peak). Hewitt Peak may be named for Hewitt Bostock, Martin Hewitt or James J. Hewitt. Geology Hewitt Peak is composed of limeston ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vermilion Range (British Columbia)
The Vermilion Range is a mountain range of the Canadian Rockies, in British Columbia, Canada. The range is west of the Vermilion River (British Columbia), Vermilion River and east of the headwaters of the Kootenay River. This range includes the following mountains and peaks: __NOTOC__ References {{reflist See also * Geography of British Columbia Mountain ranges of British Columbia Ranges of the Canadian Rockies Kootenay Land District ... [...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 (1929), Foster Peak (1933), and White Pyramid The White Pyramid ( ar, الهرم الأبيض, al-Haram al'Abyad) of Amenemhat II is located in the pyramid field at Dahshur, Egypt, and is now nothing more than a pile of rubble, having been heavily quarried for stone. The remaining limestone r ... (1939). She would eventually complete 33 first ascents in the Canadian Rockies. References External linksHistory of Gardiner Hut 1885 births 1974 deaths New Zealand mountain cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kootenay River
The Kootenay or Kootenai river is a major river in the Northwest Plateau, in southeastern British Columbia, Canada, and northern Montana and Idaho in the United States. It is one of the uppermost major tributaries of the Columbia River, the largest North American river that empties into the Pacific Ocean. The Kootenay River runs from its headwaters in the Kootenay Ranges of the Canadian Rockies, flowing from British Columbia's East Kootenay region into northwestern Montana, then west into the northernmost Idaho Panhandle and returning to British Columbia in the West Kootenay region, where it joins the Columbia at Castlegar. The river is known as the Kootenay in Canada and by the Ktunaxa Nation, and Kootenai in the United States and by the Confederated Salish and Kootenai Tribes and Kootenai Tribe of Idaho. Fed mainly by glaciers and snow melt, the river drains a rugged, sparsely populated region of more than ; over 70 percent of the basin is in Canada. From its hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vermilion River (British Columbia)
The Vermilion River, in Kootenay National Park, is headwatered at Vermilion Pass and flows through Vermilion Valley in British Columbia, Canada. Its tributaries include the Simpson River, Tokumm Creek, and Verendrye Creek. It is a major tributary of the Kootenay River. First visited (by a non- Aboriginal) by Sir George Simpson in 1841. Numa Falls Numa Falls is a waterfall of the Vermilion River located in Kootenay National Park, British Columbia, Canada. It is accessible via a short drive off the Banff–Windermere Highway 93 that connects Banff National Park and Radium Hot Springs ... on the river is directly accessible from Highway 93 in Kootenay National Park. References Historic Milestones of Kootenay National Park [...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] |
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] |
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 fossil ... [...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 precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jim Hewitt
James J. Hewitt (born January 28, 1933) was a Canadian politician, who represented the riding of Boundary-Similkameen Boundary-Similkameen is a provincial riding formed in 2008. It includes the populations of Penticton-Okanagan Valley, West Kootenay-Boundary and Yale-Lillooet. The riding's name corresponds to that of a former riding in the same area, with sim ... in the Legislative Assembly of British Columbia from 1975 to 1988 as a member of the British Columbia Social Credit Party, Social Credit Party. He held several roles in the Executive Council of British Columbia during his term as an MLA, including Minister of Agriculture, Minister of Energy and Minister of Consumer and Corporate Affairs. Although retired from elected politics, Hewitt actively campaigned against the province's 2009 British Columbia electoral reform referendum, 2009 electoral reform referendum. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
