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Mount Shanks
Mount Shanks is a mountain summit located in British Columbia, Canada. Description Mount Shanks is situated west of the Continental Divide on the boundary that Kootenay National Park shares with Mount Assiniboine Provincial Park. The peak is part of the Ball Range which is a sub-range of the Canadian Rockies. Precipitation runoff from the peak's north and east slopes flows into tributaries of the Simpson River, whereas the west slope drains into the Vermilion River. Topographic relief is significant as the summit rises 1,600 metres (5,249 ft) above the Vermilion River in and 1,340 metres (4,396 ft) above the Simpson River in . History This landform's original local name was "Folding Mountain" until the mountain was renamed in 1927 by Dominion Land Survey staff in honor of their colleague, the late Thomas Shanks, Assistant Director General of Surveys of Canada. The mountain's toponym was officially adopted on July 31, 1927, by the Geographical Names ... [...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] |
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] |
Mount Verendrye
Mount Verendrye is a mountain summit located in British Columbia, Canada. Description Mount Verendrye is situated on the western boundary of Kootenay National Park near the southern end of the Vermilion Range (British Columbia), Vermilion Range, which is a sub-range of the Canadian Rockies. The peak is the southern end of what is known as the Rockwall which is an escarpment of the Vermilion Range. The Rockwall Trail is a scenic 55 kilometer (34 mile) traverse of alpine passes, subalpine meadows, hanging glaciers, and limestone cliffs, in some places in excess of above the trail. Neighbors include Floe Peak six kilometers to the northwest and Mount Wardle six kilometers to the southeast. Topographic relief is significant as the summit rises 1,820 meters (5,970 feet) above the Banff–Windermere Highway in six kilometers (3.7 miles). A roadside pullout along the highway near Verendrye Creek provides a view of the mountain and the scorched Verendrye Creek valley which bur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wardle
Mount Wardle is a mountain summit located in British Columbia, Canada. Description Mount Wardle is situated in Kootenay National Park at the southern end of the Vermilion Range, which is a sub-range of the Canadian Rockies. Mount Wardle is home to the largest population of mountain goats within the national park. Topographic relief is significant as the summit rises 1,600 meters (5,250 feet) above the Banff–Windermere Highway in three kilometers (1.9 mile). Mount Wardle is composed of Ottertail limestone, a sedimentary rock laid down during the Cambrian period and pushed east and over the top of younger rock during the Laramide orogeny. Precipitation runoff from the mountain drains east into Wardle Creek which is a tributary of the Vermilion River, and west into Lost Creek, a tributary of the Kootenay River. History The first ascent of the summit was made in 1922 by a Topographical Survey party. The mountain's toponym was applied by Morrison P. Bridgland ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Monarch (Canadian Rockies)
The Monarch is a mountain summit located in the Ball Range of the Canadian Rockies in British Columbia, Canada. The Monarch is situated on the boundary between Kootenay National Park and Mount Assiniboine Provincial Park, four kilometres to the west side of the Continental Divide. Although not visible from roads, The Monarch is a prominent feature seen from the slopes above Sunshine Village ski resort. Its nearest higher peak is Mount Bourgeau, to the north-northeast. History The first ascent of the mountain was made in 1913 by Conrad Kain with Interprovincial Boundary Survey. In a report by the Interprovincial Boundary Survey, the mountain is referred to as Monarch Mountain, a fine piece of mountain architecture dominating the Simpson Pass area. The mountain's toponym was officially adopted in 1924 by the Geographical Names Board of Canada. Geology The Monarch is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scarab Peak (Canada)
Scarab Peak is a mountain summit located on the Continental Divide, on the shared border between Banff and Kootenay national parks in Canada. Scarab Peak is part of the Ball Range in the Canadian Rockies. The peak is situated one kilometre east-southeast of Haiduk Peak and southeast of Mount Ball. The mountain's name scarab was in keeping with the Egyptian theme of the immediate area, e.g., Egypt Lake, Mummy Lake, Pharaoh Peaks, names which were applied in 1922 by Arthur O. Wheeler of the Interprovincial Boundary Survey. Wheeler regarded the area particularly beautiful when he wrote: ''"After 30 years of exploration, surveys and mapping the main ranges of the Canadian Rockies, the writer ... can safely say that outstanding among them for scenic charm and interest may be classed the group of peaks, lakes and alpine meadows of the Egypt Lake area."''Banff - Assiniboine: a beautiful world : a guide to the trails and the rich history of Banff National Park from Palliser Pass to V ... [...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] |
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] |
