Lakes Of Alberta
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Lakes Of Alberta
This is a list of lakes of 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 (geology), 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 Ecozone (CEC), 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 Drainage basin, watersheds collecting the water and removing it from the province:
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Peyto Lake From Lookout
Peyto may refer to: *Peyto Lake *Peyto Peak *Peyto Glacier *Peyto Hut *William Peyto (other) {{geodis ...
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Canada 39 Bg 061904
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, making it the world's second-largest country by total area, with the world's longest coastline. Its border with the United States is the world's longest international land border. The country is characterized by a wide range of both meteorologic and geological regions. With a population of over 41million people, it has widely varying population densities, with the majority residing in urban areas and large areas of the country being sparsely populated. 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 ...
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Drainage Basin
A drainage basin is an area of land in which all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the drainage divide, made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, " watershed" is used only in its original sense, that of the drainage divide line. A drainage basin's boundaries are determined by watershed delineation, a common task in environmental engineering and science. In a closed drainage basin, or endorheic basin, rather than flowing to the ocean, water converges toward the ...
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Edmonton
Edmonton is the capital city of the Provinces and territories of Canada, Canadian province of Alberta. It is situated on the North Saskatchewan River and is the centre of the Edmonton Metropolitan Region, which is surrounded by Central Alberta, Alberta's central region, and is in Treaty 6, Treaty 6 territory. It anchors the northern end of what Statistics Canada defines as the "Calgary–Edmonton Corridor". The area that later became the city of Edmonton was first inhabited by First Nations in Alberta, First Nations peoples and was also a historic site for the Métis in Alberta, Métis. By 1795, many trading posts had been established around the area that later became the Edmonton census metropolitan area. "Fort Edmonton", as it was known, became the main centre for trade in the area after the 1821 merger of the Hudson's Bay Company and the North West Company. It remained sparsely populated until the Canadian acquisition of Rupert's Land in 1870, followed eventually by the arri ...
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The University Of Alberta Press
University of Alberta Press (UAlberta Press) is a publishing house and a division of the University of Alberta that engages in academic publishing. Overview The offices of University of Alberta Press (UAlberta Press) are located in the Rutherford Library on the University of Alberta campus, in Edmonton, Alberta, Canada. Operating since 1969, UAlberta Press is a unit of the Library and Museums portfolio and reports to the Vice-Provost (Library and Museums) and Chief Librarian. UAlberta Press typically publishes between 15 and 25 books each year and has approximately 450 titles available as print editions and 650 titles available in digital editions, including audiobooks, as of 2022. The Press is funded by a combination of sales revenue, licensing fees, project grants, federal and provincial operating grants, research support subsidies, and institutional budget allocation. History UAlberta Press was originally established as a department of the University of Alberta in 1969, one o ...
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Palliser's Triangle
Palliser's Triangle (), or the Palliser Triangle, is a semi-arid steppe occupying a substantial portion of the Western Canadian Canadian Prairies, Saskatchewan, Alberta and Manitoba, within the Great Plains region. While initially determined to be unsuitable for crops outside of the fertile belt due to arid conditions and dry climate, expansionists questioned this assessment, leading to homesteading in the Triangle. Agriculture in the region has since suffered from frequent droughts and other such hindrances. History Before Western European interests and settlement expanded to the region, Palliser's Triangle was inhabited by a variety of Indigenous peoples, such as the Cree, Sioux, and the Blackfoot Confederacy. Their lifestyle was centred around the buffalo hunt, as the bountiful herds of buffalo made this a sustainable and effective means of feeding themselves, the meat of which was used to make pemmican. By the mid-1850s, however, the hunt had become an economic venture, ...
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Boreal Plains Ecozone (CEC)
The Boreal Plains Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a terrestrial Ecozones of Canada, ecozone in the western Canada, Canadian provinces of Manitoba, Saskatchewan and Alberta. It also has minor extensions into northeastern British Columbia and south-central Northwest Territories. The region extends over 779,471 km2, of which 58,981 km2 is conserved (7.6 percent). Wood Buffalo National Park, the largest national park in Canada, and Whooping Crane Summer Range, the only nesting and breeding area for the critically endangered whooping crane, are both located in the northern portion of this ecozone. Industry in this ecozone once consisted primarily of forestry and agriculture, but in 1967 Great Canadian Oil Sands, Great Canadian Oil Sands Limited began extracting bitumen from the Athabasca oil sands. Operations there have expanded significantly since 2003, and the oil sands are becoming an increasingly significant economic factor in ...
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Kettle (geology)
A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake and when the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acidic conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are ...
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Muskeg
Muskeg (; ; , lit. ''moss bog'') is a peat-forming ecosystem found in several northern climates, most commonly in Arctic and boreal ecosystem, boreal areas. Muskeg is approximately synonymous with bogland, bog or peatland, and is a standard term in Canada and Alaska. The term became common in these areas because it is of Cree language, Cree origin, () meaning "low-lying marsh". Muskeg consists of non-living organic material in various states of decomposition (as peat), ranging from fairly intact sphagnum moss, to sedge peat, to highly decomposed humus. Pieces of wood can make up five to fifteen percent of the peat soil. The water table tends to be near the surface. The sphagnum moss forming it can hold fifteen to thirty times its own weight in water, which allows the spongy wet muskeg to also form on sloping ground. Muskeg patches are ideal habitats for beavers, pitcher plants, agaricales, agaric mushrooms and a variety of other organisms. Composition Muskeg forms because pe ...
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Boreal Forest
Taiga or tayga ( ; , ), also known as boreal forest or snow forest, is a biome characterized by pinophyta, coniferous forests consisting mostly of pines, spruces, and larches. The taiga, or boreal forest, is the world's largest land biome. In North America, it covers most of inland Canada, Alaska, and parts of the northern contiguous United States. In Eurasia, it covers most of Sweden, Finland, much of Russia from Karelia in the west to the Pacific Ocean (including much of Siberia), much of Norway and Estonia, some of the Scottish Highlands, some lowland/coastal areas of Iceland, and areas of northern Kazakhstan, northern Mongolia, and northern Japan (on the island of Hokkaido). The principal tree species, depending on the length of the growing season and summer temperatures, vary across the world. The taiga of North America is mostly spruce; Scandinavian and Finland, Finnish taiga consists of a mix of Norway spruce, spruce, pines and Betula, birch; Russian taiga has spruces, ...
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Prairie
Prairies are ecosystems considered part of the temperate grasslands, savannas, and shrublands biome by ecologists, based on similar temperate climates, moderate rainfall, and a composition of grasses, herbs, and shrubs, rather than trees, as the dominant vegetation type. Temperate grassland regions include the Pampas of Argentina, Brazil and Uruguay, and the steppe of Romania, Ukraine, Russia, and Kazakhstan. Lands typically referred to as "prairie" (a French loan word) tend to be in North America. The term encompasses the lower and mid-latitude of the area referred to as the Interior Plains of Canada, the United States, and Mexico. It includes all of the Great Plains as well as the wetter, hillier land to the east. From west to east, generally the drier expanse of shortgrass prairie gives way to mixed grass prairie and ultimately the richer and wetter soils of the tallgrass prairie. In the U.S., the area is constituted by most or all of the states, from north to south, of North ...
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Canadian Rockies
The Canadian Rockies () 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 of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/ Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, being the northern segment of ...
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