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Glacier Lake (Alberta)
Glacier Lake is the fourth largest lake in Banff National Park, in Alberta, Canada. Glacier Lake was named by Sir James Hector of the Palliser expedition in 1858 for the fact the lake is fed from glaciers, specifically the glaciers of the Lyell and Mons Icefields as well as the Forbes North Glacier. The lake is surrounded by Mount Outram, Division Mountain, and Mount Erasmus. The lake is fed and discharged by the Glacier River, which is a tributary of the Howse River. The lake can be accessed via a trail which starts near Saskatchewan River Crossing along the Icefields Parkway. Park at the Glacier Lake trailhead (at the end of a short unnamed road 1.1 km (0.7 mi) west of the Alberta Highway 11, David Thompson Highway turn-off). Climate Based on the Köppen climate classification, the lake experiences a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C in the winter. See ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Erasmus
Mount Erasmus is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Amery, to the north-northwest. Mount Erasmus can be seen from the Icefields Parkway west of Saskatchewan Crossing, with optimum photography conditions in morning light. History Mount Erasmus was named by James Hector in 1859 during the Palliser expedition for Peter Erasmus (1833-1931), who was an interpreter and guide for that exploration into the Canadian Rockies. Peter's skills as a Métis interpreter opened up the west for scientists, explorers, and government officials. The first ascent of the mountain was made in 1950 by John C. Oberlin and Fred Ayres. The mountain's name was officially adopted in 1957 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Mount Erasmus is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Lakes Of Alberta
This is a list of lakes in Alberta, Canada. Most of Alberta's lakes were formed during the last glaciation, about 12,000 years ago. There are many different types of lakes in Alberta, from glacial lakes in the Canadian Rockies to small shallow lakes in the prairies, brown water lakes in the northern boreal forest and muskeg, kettle holes and large lakes with sandy beaches and clear water in the central plains. Distribution of the lakes throughout the province of Alberta is irregular, with many water bodies in the wet boreal plains in the north, and very few in the semi-arid Palliser's Triangle in the southeast. __TOC__ River basins Most of Alberta's waters are drained in a general north or northeastern direction, with six major rivers forming four major watersheds collecting the water and removing it from the province: [...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] |
Alberta Highway 11
Alberta Provincial Highway No. 11, commonly referred to as Highway 11 and officially named the David Thompson Highway, is a provincial highway in central Alberta, Canada. It runs for from Highway 93 at Saskatchewan River Crossing near Mount Sarbach in Banff National Park east to Highway 12 near Nevis. It passes by Nordegg and through Rocky Mountain House, Sylvan Lake and Red Deer along its course. The highway is named after David Thompson, a British-Canadian fur trader, surveyor, and map-maker who explored the area between Rocky Mountain House and Kootenae House (near present-day Invermere, British Columbia) through Howse Pass. Route description The majority of Highway 11 is maintained by Alberta Transportation. The segment within Banff National Park is maintained by the Government of Canada, and within Red Deer limits the city has jurisdiction and is responsible for maintenance. It begins at the Icefields Parkway (Highway 93) and travel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Icefields Parkway
Highway 93 is a north–south highway in Alberta, Canada. It is also known as the Banff-Windermere Parkway south of the Trans-Canada Highway ( Highway 1) and the Icefields Parkway north of the Trans-Canada Highway. It travels through Banff National Park and Jasper National Park and is maintained by Parks Canada for its entire length. It runs from the British Columbia border at Vermilion Pass in the south, where it becomes British Columbia Highway 93, to its terminus at the junction with the Yellowhead Highway ( Highway 16) at Jasper. The route takes its number from U.S. Route 93, which runs uninterrupted south to central Arizona, and was initially designated as '93' in 1959. Route description Banff-Windermere Highway The southern portion of the route is part of the Banff-Windermere Highway, a highway that travels from British Columbia Highway 95 at Radium Hot Springs, through Kootenay National Park and Vermilion Pass across the Continental Divide, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saskatchewan River Crossing
Saskatchewan River Crossing is a locality in western Alberta, Canada. It is located within Banff National Park at the junction of Highway 93 (Icefields Parkway) and Highway 11 (David Thompson Highway). It is administered by Improvement District No. 9. It was named "The Crossing", when travellers and fur traders used this spot to cross the North Saskatchewan River on their way to British Columbia in the 19th century. Geography It lies as the confluence of the North Saskatchewan River with Howse River and Mistaya River in the Canadian Rockies and is the starting point for tours on the Columbia Icefield and other scenic hiking trails. - Icefields Parkway Drive Mount Wil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Howse River
The Howse River is a tributary of the North Saskatchewan River in western Alberta, Canada. The Howse River is a braided river, with several streams crossing in its flood plain. It is formed when Freshfield, Forbes, David and Lagoon Creek unite and flow north to discharge into the North Saskatchewan River at Saskatchewan River Crossing, Alberta, Saskatchewan River Crossing. From the headwaters of Forbes Creek, the river has a total length of 33 km. See also * List of rivers of Alberta Rivers of Alberta Banff National Park North Saskatchewan River {{Alberta-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Division Mountain
Division Mountain is located on the Continental Divide along the Alberta - British Columbia border of Canada. It also straddles the shared boundary of Banff National Park with Kootenay National Park in the Canadian Rockies. It was named in 1919 by Charles D. Walcott since the mountain divides the Lyell Icefield from the Mons Icefield. __NOTOC__ Geology The mountain 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, the mountain experiences a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C in the winter. See also *List of peaks on the British Columbia–Alberta border A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organiza ... [...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] |
Mount Outram
Mount Outram is a mountain summit located in the Howse River Valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Forbes, to the southwest. Glacier Lake is situated to the north, and the Sir James Glacier lies below the south aspect of the peak. Mount Outram can be seen from the Icefields Parkway southwest of Saskatchewan Crossing, with optimum photography conditions in morning light. History Mount Outram was named in 1920 for James Outram (1864-1925), a mountaineer who made numerous first ascents in the Canadian Rockies including Mount Assiniboine, Chancellor Peak, Cathedral Mountain, and Mount Wilson. The first ascent of the mountain was made in 1924 by F.V. Field, W.O. Field, and L. Harris, with guides Edward Feuz Jr. and J. Biner. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada. Geology Like other mountains in Banff Park, Mount Outram is composed of sedimentary ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
