Azouzetta Lake
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Azouzetta Lake
Azouzetta Lake, elevation 876m (2,874 ft), is a lake in the Hart Ranges of the Northern Rockies of British Columbia. The lake is situated adjacent the Pine Le Moray Provincial Park Pine Le Moray Provincial Park is a provincial park in British Columbia, Canada. The park, 70 km southwest of Chetwynd covers . It is located within the Hart Ranges ecosection An ecosection is a biogeographic unit smaller than an ecoregion that co .... The lake has been referred by different names within historical documents, from Summit Lake in 1870–80, to Pollen Lake in 1907 and finally Azzouzetta (Summit Lake) in 1917. References {{authority control Lakes of British Columbia Canadian Rockies Cariboo Land District ...
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Atunatche Creek
Atunatche Creek is a small river in the Hart Ranges of the Canadian Rockies, Northern Rockies of British Columbia. Atunatche Creek adopted 2 September 1954 on 93 O, as labelled on BC map 3C, 1923. Had been labelled "Tillicum Creek" on BC map 3E, 1922. "Atunatche Creek (not Tillicum)" identified in 1930 BC Gazetteer. Origin/significance not known. Tributaries *Declier Creek References {{Reflist Rivers of the Canadian Rockies Rivers of British Columbia ...
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Peace River
The Peace River (french: links=no, rivière de la Paix) is a river in Canada that originates in the Rocky Mountains of northern British Columbia and flows to the northeast through northern Alberta. The Peace River joins the Athabasca River in the Peace-Athabasca Delta to form the Slave River, a tributary of the Mackenzie River. The Finlay River, the main headwater of the Peace River, is regarded as the ultimate source of the Mackenzie River. The combined Finlay–Peace–Slave–Mackenzie river system is the 13th longest river system in the world. History The regions along the river are the traditional home of the Danezaa people, called the Beaver by the Europeans. The fur trader Peter Pond is believed to have visited the river in 1785. In 1788 Charles Boyer of the North West Company established a fur trading post at the river's junction with the Boyer River. In 1792 and 1793, the explorer Alexander Mackenzie travelled up the river to the Continental Divide. Mackenzie r ...
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Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ...
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Hart Ranges
The Hart Ranges are a major subrange of the Canadian Rockies located in northeastern British Columbia and western Alberta. The mountains constitute the southernmost portion of the Northern Rocky Mountains. The Hart Ranges were named in honour of British Columbia Premier John Hart, as is the highway which traverses the Pine Pass in the northern part of the range, connecting the north-central Interior of the province to the Peace River Regional District to the northeast. Geography The boundaries of the Hart Ranges are the Rocky Mountain Trench and the McGregor Plateau on the west/southwest, the Peace Reach of Williston Lake on the north, a certain line of demarcation with the Rocky Mountain Foothills to the east/northeast, and the Jarvis Creek to the south. The Hart Ranges is home to two ultra-prominent peaks, Mount Crysdale and Mount Ovington. Mount Ida and Mount Sir Alexander are south of Jarvis Creek and are in the Continental Ranges, which comprise the main and best-known ...
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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 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, bein ...
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British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost 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 third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ...
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Pine Le Moray Provincial Park
Pine Le Moray Provincial Park is a provincial park in British Columbia, Canada. The park, 70 km southwest of Chetwynd covers . It is located within the Hart Ranges ecosection An ecosection is a biogeographic unit smaller than an ecoregion that contains minor physiographic, macroclimatic or oceanographic variations. They are a virtual ecological zone in the Canadian province of British Columbia, which contains 139 ecosec ... near the Rocky Mountains. It is within the Engelmann Spruce-Subalpine Fir biogeoclimatic zone. Water courses include Link and Mountain Creeks, the Pine River, and Heart Lake. It provides habitat for trout, Arctic grayling, mountain whitefish, high elevation caribou, moose, wolverine, and grizzly bear. It is recognized by the province as an area traditionally used by First Nations people. Its topography has examples of Karst topography and alpine areas. It was created as Provincial Park in June 2000, with additional area added in 2001. The park can be used for ...
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Lakes Of British Columbia
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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