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Location of the Yukon River and watershed


The Yukon River is a major watercourse of northwestern North America. The source of the river is located in British Columbiamarker, Canadamarker. The next portion lies in, and gives its name to Canada's Yukonmarker Territory. Then, more than the lower half of the river lies in the U.S. state of Alaskamarker. The river is 3,185 km (1,980 mi) long and empties into the Bering Seamarker at the Yukon-Kuskokwim Deltamarker. The average flow is 6,430 m³/s (227,000 ft³/s). The total drainage area is 832,700 km² (321,500 mi²), of which 323,800 km² (126,300 mi²) is in Canada. By comparison, the total area is more than 25% larger than Texasmarker or Albertamarker.

The longest river in Alaska and the Yukon Territory, it was one of the principal means of transportation during the 1896–1903 Klondike Gold Rush. Paddle-wheel riverboats continued to ply the river until the 1950s, when the Klondike Highway was completed.

Yukon means "great river" in Gwich'in. The river was called Kwiguk, or "large stream", in Yupik. The Lewes River is the former name of the upper course of the Yukon, from Marsh Lakemarker to the confluence of the Pelly Rivermarker at Fort Selkirkmarker.

The Yukon River has had a history of pollution from gold mining, military installations, dumps, wastewater, and other sources. However, the Environmental Protection Agency does not list the Yukon River among its impaired watersheds, and water quality data from the U.S. Geological Survey shows relatively good levels of turbidity, metals, and dissolved oxygen.

The Yukon River Inter-Tribal Watershed Council, a cooperative effort of 64 First Nations and tribes in Alaska and Canada, has the goal of making the river and its tributaries safe to drink from again by supplementing and scrutinizing Government data.

Course

Map of the Yukon River watershed


The generally accepted source of the Yukon River is the Llewellyn Glacier at the southern end of Atlin Lakemarker in British Columbiamarker. Others suggest that the source is Lake Lindeman at the northern end of the Chilkoot Trailmarker. Either way, Atlin Lake flows into Tagish Lakemarker (via the Atlin River), as eventually does Lake Lindeman after flowing into Bennett Lakemarker. Tagish Lake then flows into Marsh Lakemarker (via the Tagish River). The Yukon River proper starts at the northern end of Marsh Lake, just south of Whitehorsemarker. Some argue that the source of the Yukon River should really be Teslin Lakemarker and the Teslin Rivermarker, which has a larger flow when it reaches the Yukon at Hootalinqua. The upper end of the Yukon river was originally known as the Lewes River until it was established that it actually was the Yukon. North of Whitehorse, the Yukon River widens into Lake Labergemarker, made famous by Robert W. Service's "The Cremation of Sam McGee." Other large lakes that are part of the Yukon River system include Kusawa Lake (into the Takhini Rivermarker) and Kluane Lakemarker (into the Kluane and then White River).

The river passes through the communities of Whitehorsemarker, Carmacksmarker, (just before the Five Finger Rapidsmarker) and Dawson Citymarker in the Yukon Territorymarker, and crossing Alaskamarker into Eagle, Circlemarker, Fort Yukonmarker, Stevens Villagemarker, Tananamarker, Rubymarker, Galenamarker, Nulatomarker, Graylingmarker, Holy Crossmarker, Russian Missionmarker, Marshallmarker, Pilot Stationmarker, St. Marysmarker (which is accessible from the Yukon at Pilot Point), and Mountain Villagemarker. After Mountain Villagemarker, the main Yukon channel frays into many channels, sprawling across the delta. There are a number of communitites after the "head of passes," as the channel division is called locally: Nunum Iqua, Alakanukmarker, Emmonakmarker, and Kotlikmarker. Of those delta communities, Emmonakmarker is the largest with roughly 760 people in the 2000 census. Emmonakmarker's gravel airstrip is the regional hub for flights.

Hazards



Volcanoes near the Yukon River, such as Volcano Mountainmarker in the Fort Selkirk Volcanic Fieldmarker, may have once partly blocked or at least altered the Yukon River by lava flows. Any future activity in this area could disrupt the course of the river and could have serious impacts on people living or working downstream.

Navigational obstacles on the Yukon River are the Five Finger Rapidsmarker and Rink Rapids downstream from Carmacks.

Bridges

Despite its length, there are only four vehicle-carrying bridges across the river:

A car ferry crosses the river at Dawson City in the summer; it is replaced by an ice bridge over the frozen river during the winter. Plans to build a permanent bridge were announced in March 2004, although they are currently on hold because bids came in much higher than budgeted.

There are also 2 pedestrian-only bridges in Whitehorse, as well as a dam across the river and a hydroelectric generating station. The construction of the dam flooded the White Horse Rapids, which gave the city its name, and created Schwatka Lakemarker.

The river flows into several parklands and refuges including:
Canoeing the Yukon River


Tributaries

Yukon Territory



Alaska

(tributaries in the Yukon)
(tributaries in Alaska)


Geography and ecology

Some of the upper slopes of this watershed (e.g. Nulato Hills) are forested by Black Spruce. This locale near the Seward Peninsulamarker represents the near westernmost limit of the Black Spruce, Picea mariana, one of the most widespread conifers in northern North America.

See also



References

External links




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