Mount GEC
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Mount GEC
Mount GEC is a mountain located in the Sunwapta River Valley of Jasper National Park. Gec lies northwest of Diadem Peak. The mountain was named in 1961 after the first names of the three climbers who made the first ascent — George Ellen Chuck. See also * List of mountains in the Canadian Rockies A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the A ... References Mountains of Jasper National Park Three-thousanders of Alberta Winston Churchill Range {{AlbertaRockies-geo-stub ...
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Winston Churchill Range
The Winston Churchill Range is a mountain range in the central section of the Park Ranges of the Canadian Rockies located in Jasper National Park. The range was named after Sir Winston Churchill, former British prime minister. The eastern boundary of the range begins on the western side of Sunwapta River from the Jasper and Banff boundary and extends north to Sunwapta Falls. The western boundary of the range is defined by the Athabasca River valley to the east of Warwick Mountain. The valley narrows as it approaches the 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 ..., and separates Mt. Columbia from Mt. King Edward, the latter of which is not part of the range. This range includes the following mountains and peaks: References Ranges of the Cana ...
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Mount Smythe
Mount Smythe is a mountain in Jasper National Park, Alberta, Canada. It is located in the Winston Churchill Range, southwest of Gong Peak and north of Mount Nelson. It reaches a summit elevation of . The mountain was named after Francis Sydney Smythe, an international mountaineer who climbed in the Himalayas, Alps and the Canadian Rockies. Geology Mount Smythe is composed of sedimentary rock laid down during 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 Smythe is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. See also *List of mountains in the Canadian Rockies A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian R ...
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List Of Mountains Of Alberta
Most of Alberta's mountains are found on the western edge of the province of Alberta, consisting of the eastern slopes of the Canadian Rockies, which run through the province from Alberta's mid-point to its southern border with the United States. Other elevated spots can be found in the Caribou Mountains and the Cypress Hills. The peaks of the Canadian Rockies are majestic, many of them reaching a height of more than three kilometres above sea level. Alberta's southwestern boundary is traced on the Continental Divide, along the high ranges of the Rocky Mountains, and many peaks are located on the Alberta–British Columbia border. The peak of Mount Columbia, within Jasper National Park, is the highest point in Alberta, second highest in the Canadian Rockies and 28th highest in Canada. The Caribou Mountains are located in the northern extremity of Alberta, forming an elevated plateau in the northern plains and wetlands. They reach an altitude of 1,030 m, almost 700&n ...
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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 ...
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Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ...
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Jasper National Park
Jasper National Park is a national park in Alberta, Canada. It is the largest national park within Alberta's Rocky Mountains spanning . It was established as a national park in 1930 and declared a UNESCO World Heritage Site in 1984. Its location is north of Banff National Park and west of Edmonton. The park contains the glaciers of the Columbia Icefield, springs, lakes, waterfalls and mountains. History First Nations The territory encompassed by what is now Jasper National Park has been inhabited since time immemorial by Nakoda, Cree, Secwépemc, and Dane-zaa peoples. Plainview projectile points have been found at the head of Jasper Lake, dating back to between 8000 and 7000 BCE. In the centuries between then and the establishment of the park, First Nations land use has fluctuated according to climatic variations over the long term, and according to cyclical patterns of ungulate population numbers, particularly elk, moose, mule deer, and occasionally caribou. Starting ...
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National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mappi ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Sunwapta River
The Sunwapta River is a major tributary of the Athabasca River in Jasper National Park in Alberta, Canada. Course The headwaters of the Sunwapta River are near the Columbia Icefield in the valley west-northwest of Sunwapta Pass, which divides Jasper National Park from Banff National Park. Several kilometres down the valley from the pass is Sunwapta Lake, at the toe of the Athabasca Glacier, which is considered the nominal source for the river. The Sunwapta River then continues to run northwest through Jasper National Park, following the Icefields Parkway, and finally joins the Athabasca River shortly after Sunwapta Falls. ''Sunwapta'' is a Stoney language word meaning "turbulent river". Geologist A. P. Coleman named the river in 1892.Karamitsanis, Aphrodite (1991). ''Place Names of Alberta, Volume 1''. Calgary: University of Calgary Press, pg. 240 Tributaries *Kitchener Creek *Tangle Creek *Woolley Creek *Beauty Creek *Diadem Creek *Grizzly Creek *Jonas Creek *Poboktan Cree ...
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Diadem Peak
Diadem Peak is a peak located in the Sunwapta River Valley of Jasper National Park, Canada. Diadem Peak is essentially the high point of a ridge leading down from the slightly higher Mount Woolley (). This peak was the first 11,000er north of the Columbia Icefield to be climbed and one of the few peaks in the Canadian Rockies to be climbed before 1900. The mountain was named in 1898 by the first ascent team of J. Norman Collie, Hugh Stutfield and Hermann Woolley. Upon reaching the summit, they discovered a crown (diadem) of snow about high covering the almost flat layer of rocks on top. Climbing history In the summer of 1898, J. Norman Collie, Hugh Stutfield and Herman Woolley, had made their way up Woolley Creek and initially had their sights on reaching the top of Mount Woolley by climbing the icefield that separates Mt. Woolley from Diadem Peak. However, after a brief downpour which forced them to seek shelter among some rocks, they had just begun preparing the rope for a ...
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List Of Mountains In The Canadian Rockies
A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part ... Mountains, Rockies Mountains, Rockies ...
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Mountains Of Jasper National Park
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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