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Naiset Point
Naiset Point is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. The mountain is situated southeast of Lake Magog, and at the end of the ridge extending north from Terrapin Mountain. Naiset Point is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. History The mountain was named in 1913 by The Interprovincial Boundary Survey for the word ''naiset'' which translates from the First Nations in Canada, First Nations word for ''sunset''. The first ascent of Naiset Point was made in 1920 by H.E. Bulyea, N. Allen, M. Gold, D.J. McGeary, J. Stewart, E.L. Tayler, and C.G. Wates. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Naiset Point is located in a subarctic cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost Provinces and territories of Canada, province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's Population of Canada by province and territory, third-most populous province. The capital of British Columbia is Victoria, British Columbia, Victoria and its largest city is Vancouver. Vancouver is List of census metropolitan areas and agglomerations in Canada, the third-largest metropolitan area in Canada; the 2021 Canadian census, 2021 census recorded 2.6million people in Metro Vancouver Regional District, Metro Vancouver. The First Nations in Canada, first known human inhabi ... [...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] |
Nub Peak
Nub Peak is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Nestor Peak, to the west. The mountain is situated north of Sunburst Peaks, with Elizabeth Lake and Cerulean Lake in between. The Continental Divide and Assiniboine Pass are situated to the east. Nub Peak is famous for its panoramic view of Mount Assiniboine with its surrounding lakes and peaks. The mountain's descriptive name was officially adopted in 1924. An arm extending southwest from Nub is officially known as Chucks Ridge, and an arm extending southeast is officially called Nublet. Nub Peak is composed of sedimentary rock laid down during the Cambrian period and pushed east over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Nub Peak is located in a subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sunburst Peaks
Sunburst Peaks is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Wedgwood Peak, to the south. The mountain is situated immediately southeast of Sunburst Lake, west of Lake Magog, and south of Cerulean Lake. History The first ascent of the peak was made in 1910 by Katherine Longstaff and her brother Dr. Tom Longstaff, with Rudolph Aemmer as their guide. The mountain was named Sunburst Peak in 1953 after Sunburst Lake, which had been named by the Interprovincial Boundary Survey. The name was officially changed by the Geographical Names Board of Canada to Sunburst Peaks (plural) on February 15, 1983 with the intention extended to apply to three peaks. Geology Sunburst Peak is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wedgwood Peak
Wedgwood Peak is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is Mount Assiniboine, to the south. The mountain is situated northwest of Lake Magog and south of Sunburst Peaks. __NOTOC__ History The first ascent of Wedgwood Peak was made in 1910 by Katherine Longstaff and her brother Dr. Tom George Longstaff, with Rudolph Aemmer as their guide. The mountain was named in 1918 by Katherine Longstaff Wedgwood for Arthur Felix Wedgwood (1877–1917), her late husband who was killed in World War I. Arthur Felix Wedgwood was also a fifth-generation descendant of Josiah Wedgwood. First recognized as ''Mount Wedgwood'' in 1924, the mountain's present name Wedgwood Peak became official on March 31, 1966 when approved by the Geographical Names Board of Canada. Geology Wedgwood Peak is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Magog
Mount Magog is located on the border of Alberta and British Columbia on the Continental Divide in the Canadian Rockies. It also straddles the shared boundary of Banff National Park with Mount Assiniboine Provincial Park. It was named in 1930 after references in the Bible. __NOTOC__ Geology Mount Magog is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, Mount Magog is located in a 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, ge ... with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors below -30°C. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Divide
A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, not connected to the open sea. Every continent on earth except Antarctica (which has no known significant, definable free-flowing surface rivers) has at least one continental drainage divide; islands, even small ones like Killiniq Island on the Labrador Sea in Canada, may also host part of a continental divide or have their own island-spanning divide. The endpoints of a continental divide may be coastlines of gulfs, seas or oceans, the boundary of an endorheic basin, or another continental divide. One case, the Great Basin Divide, is a closed loop around an endoreic basin. The endpoints where a continental divide meets the coast are not always definite since the exact border between adjacent bodies of water is usually not clearly defined. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Towers (Canada)
The Towers is a mountain located on the border of Alberta and British Columbia on the Continental Divide. It also straddles the shared boundary of Banff National Park with Mount Assiniboine Provincial Park. It was named in 1917 by Arthur O. Wheeler. Its nearest higher peak is Mount Magog, to the west. Geology The Towers is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classification, The Towers is located in a 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, ge ... with cold, snowy winters, and mild summers. Temperatures can drop below -20°C with wind chill factors be ... [...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 ... [...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] |
List Of Mountains Of Canada
Most mountain peaks of Canada lie in the west, specifically in British Columbia, Alberta, and the Yukon. Mountains can be found all over British Columbia while those in Alberta are mainly situated on the eastern side of the Canadian Rockies. The Saint Elias Mountains in the Yukon hold some of country's highest mountains, including the highest, Mount Logan at . Alberta ;Highest peaks Mts. Columbia & King Edward.jpg, Mount Columbia & King Edward in background The Twins - South and North (l-r).jpg, The Twins massif - South Twin and North Twin (l-r) Mount Assiniboine massif.jpg, Mount Assiniboine seen from above Lake Magog Columbia Icefields - panoramio (1).jpg, Snow Dome seen from Icefields Parkway British Columbia Mount Assiniboine.jpg, Mount Assiniboine Mount Robson South.jpg, Mount Robson, highest in Canadian Rockies Garibaldi black tusk.jpg, The Black Tusk Snow Dome+Dome Glacier.jpg, Snow Dome and Dome Glacier Mount Mackenzie from Mount Revelstoke NP.jpg, Moun ... [...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] |
