Mount Weiss
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Mount Weiss
Mount Weiss is a mountain in Alberta, Canada located on the western side of the Sunwapta River valley of Jasper National Park, and is part of the Winston Churchill Range. The mountain was named in 1972 after Joe Weiss (1896-1993), who had spent 45 years of his life exploring and guiding in Jasper. See also * Geography of Alberta Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by t ... References {{DEFAULTSORT:Weiss Three-thousanders of Alberta Winston Churchill Range Mountains of Jasper National Park ...
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Gong Peak
Gong Peak is a mountain located in the Sunwapta River Valley of Jasper National Park in Alberta, Canada. The peak lies three km southeast of Mount Weiss Mount Weiss is a mountain in Alberta, Canada located on the western side of the Sunwapta River valley of Jasper National Park, and is part of the Winston Churchill Range. The mountain was named in 1972 after Joe Weiss (1896-1993), who had spent 45 .... The mountain was named in 1919 by the Interprovincial Boundary Survey after nearby Gong Lake. References Three-thousanders of Alberta Winston Churchill Range Mountains of Jasper National Park {{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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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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Jasper, Alberta
Jasper is a specialized municipality and townsite in western Alberta within the Canadian Rockies. The townsite is in the Athabasca River valley and is the commercial centre of Jasper National Park. History Established in 1813, Jasper House was first a fur trade outpost of the North West Company, and later Hudson's Bay Company, on the York Factory Express trade route to what was then called "New Caledonia" (now British Columbia) and Fort Vancouver on the lower Columbia River. Jasper House was 35 km north of today's town of Jasper. Jasper Forest Park was established in 1907. The railway siding at the location of the future townsite was established by the Grand Trunk Pacific Railway in 1911 and originally named Fitzhugh after a Grand Trunk vice president (along the Grand Trunk's "alphabet" line). The Canadian Northern Railway began service to its ''Jasper Park'' station in 1912, about 700 m from GTP's Fitzhugh station. The townsite was surveyed in 1913 by H. Math ...
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Geography Of Alberta
Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by the province of Saskatchewan for ; and at 60° north the Northwest Territories for . The southern half of the province borders British Columbia along the Continental Divide of the Americas on the peaks of the Rocky Mountains, while the northern half borders British Columbia along the 120th meridian west. Along with Saskatchewan it is one of only two landlocked provinces or territories. Terrain Alberta's landscape is marked by the impact of the Wisconsin Glaciation, about 75,000 to 11,000 years ago, when the entire future province was covered in ice. As the ice sheet receded, the landscape was changed, and large amounts of glacial till were left behind. The southern portion consists chiefly of plains that are almost entirely treeless. As ...
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Three-thousanders Of Alberta
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ...
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