Moose Lake (Alberta)

Moose Lake is a relatively small lake in North-eastern Alberta, Canada, which drains north into the Beaver River (Canada). It is located just a few kilometres west of the town of Bonnyville. Despite dense green and blue-green algae blooms in summer, the lake is a popular recreational area for local residents.

It is unclear whether the name (translated from the French: Lac d'Orignal) was given because of the large moose population of the area or because the shape of the lake resembles a moose's head - Franchere Bay and Vezeau Bay being the antlers, Bonnyville Beach the chin, and Island Bay the nose (complete with a large island for a nostril).

Around 1768 William Pink passed the mouth of the Mooselake River. In 1789 Angus Shaw of the North West Company built a post on the northwest shore of the lake called Fort Lac L'Orignal or Shaw House. It was on the northwest side on a large point southeast of the lake's outlet. The river was so shallow that canoes were taken up the river empty and goods portaged overland. It was in good beaver country and within easy reach of Fort George 35 miles to the south on the North Saskatchewan. Buffalo pemmican was carried north to the lake and then via the Beaver River to Lac Île-à-la-Crosse to feed the voyageurs on their long journey to Lake Athabasca. In the 1792-93 season Moose Lake produced 64 of the 392 total packs of beaver produced by the Churchill River Department. In 1798 David Thompson (explorer) reached the lake from Fort George.

Moose Lake

Moose Lake may refer to:

Communities

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In the United States:

Lakes

In Canada:

In the United States:

Lake

A lake is an area of variable size filled with water, localized in a basin, that is surrounded by land, apart 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 (except for sea lochs in Scotland and Ireland), and therefore are distinct from lagoons, and are also larger and deeper than ponds, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which are usually flowing. However 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. In some parts of the world there are many lakes because of chaotic drainage patterns left over from the last Ice Age. All lakes are temporary over geologic time scales, as they will slowly fill in with sediments or spill out of the basin containing them.

Many lakes are artificial and are constructed for industrial or agricultural use, for hydro-electric power generation or domestic water supply, or for aesthetic or recreational purposes.

Moose

The moose (North America) or elk (Eurasia), Alces alces, is the largest extant species in the deer family. Moose are distinguished by the palmate antlers of the males; other members of the family have antlers with a dendritic ("twig-like") configuration. Moose typically inhabit boreal and mixed deciduous forests of the Northern Hemisphere in temperate to subarctic climates. Moose used to have a much wider range but hunting and other human activities have greatly reduced it. Moose have been reintroduced to some of their former habitats. Currently, most moose are found in Canada, Alaska, Scandinavia, Latvia, Estonia, New England and Russia. Their diet consists of both terrestrial and aquatic vegetation. The most common moose predators are wolves, bears and humans. Unlike most other deer species, moose are solitary animals and do not form herds. Although generally slow-moving and sedentary, moose can become aggressive and move quickly if angered or startled. Their mating season in the autumn can lead to spectacular fights between males competing for a female.

Canadian Rockies

The Canadian Rockies comprise the Canadian segment of the North American Rocky Mountains. They are the eastern part of the Canadian Cordillera, which is a system of multiple ranges of mountains which runs from the Canadian Prairies to the Pacific Coast. The Canadian Rockies mountain system comprises the southeastern part of this system, laying between the Interior Plains of Alberta and Northeastern British Columbia on the east to the Rocky Mountain Trench of BC on the west. The southern end borders Idaho and Montana of the USA. In geographic terms the boundary is at the Canada/US border, but in geological terms it might be considered to be at Marias Pass in northern Montana. The northern end is at the Liard River in northern British Columbia.

The Canadian Rockies have numerous high peaks and ranges, such as Mount Robson (3,954 m (12,972 ft)) and Mount Columbia (3,747 m (12,293 ft)). The Canadian Rockies are composed of shale and limestone. Much of the range is protected by national and provincial parks, several of which collectively comprise a World Heritage Site.