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 Columbia
, Canada
.
The next
portion lies in, and gives its name to Canada's Yukon
Territory. Then, more than the lower half of the river
lies in the U.S. state of Alaska
.
The river
is 3,185 km (1,980 mi) long and empties into the Bering Sea
at the Yukon-Kuskokwim Delta
. 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 Texas
or Alberta
.
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 Lake
to the confluence of the Pelly River
at Fort
Selkirk
.
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 Lake
in British Columbia
. Others suggest that the source is Lake
Lindeman at the northern end of the Chilkoot Trail
. Either way, Atlin Lake flows into Tagish Lake
(via the Atlin River), as eventually does Lake
Lindeman after flowing into Bennett Lake
. Tagish Lake then flows into Marsh Lake
(via the Tagish River). The Yukon River
proper starts at the northern end of Marsh Lake, just south of
Whitehorse
. Some argue that the source of the Yukon
River should really be Teslin Lake
and the Teslin River
, 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
Laberge
, 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
River
) and Kluane
Lake
(into the Kluane and then White
River).
The river
passes through the communities of Whitehorse
, Carmacks
, (just before the Five Finger Rapids
) and Dawson City
in the Yukon
Territory
, and crossing Alaska
into
Eagle, Circle
, Fort
Yukon
, Stevens Village
, Tanana
, Ruby
, Galena
, Nulato
, Grayling
, Holy Cross
, Russian Mission
, Marshall
, Pilot Station
, St. Marys
(which is accessible from the Yukon at Pilot
Point), and Mountain Village
. After Mountain Village
, 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, Alakanuk
, Emmonak
, and Kotlik
.
Of those
delta communities, Emmonak
is the largest with roughly 760 people in the 2000
census. Emmonak
's gravel airstrip is the regional hub for
flights.
Hazards
Volcanoes near the Yukon River, such as Volcano
Mountain
in the Fort Selkirk Volcanic Field
, 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
Rapids
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 Lake
.
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
Peninsula
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