British Mountains (Yukon)

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The British Mountains are a mountain range in Yukon Territory, Canada. [1]

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<span class="mw-page-title-main">Geography of Canada</span>

Canada has a vast geography that occupies much of the continent of North America, sharing a land border with the contiguous United States to the south and the U.S. state of Alaska to the northwest. Canada stretches from the Atlantic Ocean in the east to the Pacific Ocean in the west; to the north lies the Arctic Ocean. Greenland is to the northeast with a shared border on Hans Island. To the southeast Canada shares a maritime boundary with France's overseas collectivity of Saint Pierre and Miquelon, the last vestige of New France. By total area, Canada is the second-largest country in the world, after Russia. By land area alone, however, Canada ranks fourth, the difference being due to it having the world's largest proportion of fresh water lakes. Of Canada's thirteen provinces and territories, only two are landlocked while the other eleven all directly border one of three oceans.

<span class="mw-page-title-main">Whitehorse</span> Capital and largest city of Yukon, Canada

Whitehorse is the capital of the Yukon, and the largest city in Northern Canada. It was incorporated in 1950 and is located at kilometre 1426 on the Alaska Highway in southern Yukon. Whitehorse's downtown and Riverdale areas occupy both shores of the Yukon River, which rises in British Columbia and meets the Bering Sea in Alaska. The city was named after the White Horse Rapids for their resemblance to the mane of a white horse, near Miles Canyon, before the river was dammed.

<span class="mw-page-title-main">Yukon</span> Territory of Canada

Yukon is the smallest and westernmost of Canada's three territories. It is the third-least populated province or territory in Canada, with a population of 45,750 as of 2024. However, Whitehorse, the territorial capital, is the largest settlement in any of the three territories.

<span class="mw-page-title-main">Extreme points of Canada</span>

The following lists include extreme and significant points of the geography of Canada.

<span class="mw-page-title-main">Liard River</span> River in Canada

The Liard River of the North American boreal forest flows through Yukon, British Columbia and the Northwest Territories, Canada. Rising in the Saint Cyr Range of the Pelly Mountains in southeastern Yukon, it flows 1,115 km (693 mi) southeast through British Columbia, marking the northern end of the Rocky Mountains and then curving northeast back into Yukon and Northwest Territories, draining into the Mackenzie River at Fort Simpson, Northwest Territories. The river drains approximately 277,100 km2 (107,000 sq mi) of boreal forest and muskeg.

<span class="mw-page-title-main">Mount Nirvana</span> Highest mountain in NWT, Canada

Mount Nirvana, at 2,773 m (9,098 ft) is the unofficial name of the highest mountain in the Northwest Territories, Canada. Currently the Canadian government is working to officially recognize the name Thunder Mountain, reflecting the local Dehcho First Nation name for the mountain. Today, the name Mt. Nirvana is commonly depicted in alpine literature.

Komakuk Beach was the site of a DEW Line station, located on the Arctic coast of Yukon, Canada. The station was closed in 1993 pursuant to the general policy of dismantling such stations that was adopted following the collapse of the Soviet Union, which effectively ended the Cold War and obviated the need to maintain these installations.

<span class="mw-page-title-main">Tungsten, Northwest Territories</span> Abandoned company town in the Northwest Territories, Canada

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<span class="mw-page-title-main">Mackenzie Mountains</span> Mountain range in northwestern Canada

The Mackenzie Mountains are a Canadian mountain range forming part of the Yukon-Northwest Territories boundary between the Liard and Peel rivers. The range is named in honour of Canada's second prime minister, Alexander Mackenzie. Nahanni National Park Reserve and Nááts'ihch'oh National Park Reserve are in the Mackenzie Mountains.

<span class="mw-page-title-main">Geography of Yukon</span>

Yukon is in the northwestern corner of Canada and is bordered by Alaska, British Columbia and the Northwest Territories. The sparsely populated territory abounds with natural scenery, snowmelt lakes and perennial white-capped mountains, including many of Canada's highest mountains. The territory's climate is Arctic in territory north of Old Crow, subarctic in the region, between Whitehorse and Old Crow, and humid continental climate south of Whitehorse and in areas close to the British Columbia border. Most of the territory is boreal forest with tundra being the main vegetation zone only in the extreme north and at high elevations.

<span class="mw-page-title-main">Ibex Valley</span>

The Ibex Valley is a valley approximately 16 kilometres (9.9 mi) west of the City of Whitehorse, Yukon, Canada. The valley and the surrounding area is governed by five elected councilors from the Ibex Valley Hamlet. The valley is rural with a mixture of farms and country residential. The population of the Hamlet in 2021 was 523.

<span class="mw-page-title-main">Ibex Valley, Yukon</span>

Ibex Valley is a hamlet in Canada's Yukon. The hamlet is considered a local advisory area with an advisory council providing local government. Its population in 2021 according to the 2021 Canadian Census was 523.

<span class="mw-page-title-main">Old Crow Flats</span> Canadian wetland & archaeological site

Old Crow Flats is a 6,170 km2 (2,382 sq mi) wetland complex in northern Yukon, Canada along the Old Crow River. It is north of the Arctic Circle and south of the Beaufort Sea, and is nearly surrounded by mountains.

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The following outline is provided as an overview of and topical guide to Canada:

Kusawa Lake is a lake in the southern Yukon, Canada. Kusawa means "long narrow lake" in the Tlingit language. The Kusawa Lake is a lake in Canada's Yukon Territory. It is located at an altitude of 671 m (2,201 ft) and is 60 km (37 mi) southwest of Whitehorse near the British Columbia border. It meanders over a length of 75 km (47 mi) with a maximum width of about 2.5 km (1.6 mi) through the mountains in the north of the Boundary Ranges. It is fed by the Primrose River and Kusawa River. The Takhini outflows to the Yukon River from the northern tip of Kusawa Lake. Kusawa Lake has an area of 142 km2 (55 sq mi). The lake has a maximum depth of 140 m (460 ft) and is of glacial origin. It is a common tourist destination and is also popular for fishing.

<span class="mw-page-title-main">Interior Alaska–Yukon lowland taiga</span> Taiga ecoregion of Canada and the United States

The interior Alaska–Yukon lowland taiga is an ecoregion in the taiga and boreal forests biome, of far northern North America.

<span class="mw-page-title-main">Peel watershed</span> River in Canada

The Peel watershed drains 14% of the Yukon Territory Canada and flows into the Beaufort Sea via the Peel and then Mackenzie Rivers. While the lower part of the Peel River and its confluence with the Mackenzie River are in the North West Territories, most of the watershed, 68,000 km2 out of 77,000 km2 is in the Yukon. Six major tributaries and numerous smaller streams feed the Peel. The Yukon portion of the watershed is undergoing land use planning, a process laid out in Chapter 11 of the Yukon Land Claims Agreement and is called the Peel Watershed Planning Region (PWPR). This article is confined to the PWPR.

<span class="mw-page-title-main">Brooks–British Range tundra</span> Tundra ecoregion of Canada and the United States

The Brooks–British Range tundra is an ecoregion spanning North America and Canada, and is one of the WWF Global 200 ecoregions.

<span class="mw-page-title-main">Ogilvie–MacKenzie alpine tundra</span> Tundra ecoregion of Canada and the United States

The Ogilvie–MacKenzie alpine tundra ecoregion covers the mountainous middle of the Yukon Territory in Canada, with extensions into the Northwest Territories. The vegetation is alpine and subalpine open forest of stunted spruce, fir and pine. The area is rugged but sections appear to have been unglaciated in the late Pleistocene and there are therefore relic species in the region. The area is remote and supports large, sustainable predator-prey systems.

References

  1. Yukon Ecoregions Working Group (2004). Smith, C.A.S.; Meikle, J.C.; Roots, C.F. (eds.). Ecoregions of the Yukon Territory: Biophysical properties of Yukon landscapes (PDF). PARC Technical Bulletin No. 04-01. Agriculture and Agri-Food Canada. pp. 97–122. ISBN   0-660-18828-7. Archived (PDF) from the original on 10 September 2021.

69°04′N140°04′W / 69.06°N 140.06°W / 69.06; -140.06