| Yenisei River
|
| The Yenisei basin, including Lake Baikal |
| Origin | Tuva (Russia), Darkhad Valley (Mongolia) |
| Mouth | Arctic Ocean |
| Basin countries | Russia, Mongolia |
| Length | 5,539 km (3,445 mi) |
| Avg. discharge | 19,600 m³/s (692,272 ft³/s) |
| Basin area | 2,580,000 km² (996,138 mi²) |
Yenisey (
Russian:
Енисе́й) is the greatest
river system flowing to the
Arctic Ocean, and at 5,539 km (3,445 mi) is the
fifth longest river in the world. It is slightly shorter but with 1.5 times the flow of the
Mississippi-
Missouri. Rising in
Mongolia, it follows a northerly course to the
Kara Sea, draining a large part of central
Siberia, the longest stream following the Yenisei-Angara-Selenga-Ider.
The upper reaches, subject to rapids and flooding, pass through sparsely populated areas. The middle section is controlled by a series of massive hydroelectric dams fuelling significant Russian
primary industry. Partly built by
gulag labor in Soviet times, industrial contamination remains a serious problem in an area hard to police. Moving on through sparsely-populated
taiga, the Yenisei swells with numerous tributaries and finally reaches the Kara Sea in desolate
tundra where it is icebound for more than half the year.
Upper Yenisei
The Yenisey rises in two major headstreams: the Bolshoi (greater) Yenisei also known as the Bii-Khem (Бии-Хем) rises in the
Tuva region on the S flank of the Eastern
Sayan Mountains and north of the
Tannu-Ola Mountains at
; the Malyy (lesser) Yenisei also known as the Kaa-Khem (Каа-Хем) rises in the
Darkhad (
rift) valley in
Mongolia. Recent research has shown that the narrow exit to the Darkhad Valley has regularly been blocked by ice producing a lake as large as neighbouring
Lake Khövsgöl. When the glaciers retreated (the last time 9300 years BP) as much as 500 km³ of water would have escaped, possibly catastrophically.
Lake Baikal Headwaters
The 320 km (partly navigable)
Upper Angara River feeds into the northern end of
Lake Baikal from the
Buryat Republic but the largest inflow is from the
Selenga which forms a delta on the south-eastern side. The longest tributaries rise on the eastern slopes of central Mongolia's
Khangai Mountains. Another tributary, the
Tuul passes through the Mongolian capital,
Ulan Bator while the
Egiin Gol drains
Lake Khövsgöl.
Angara River
The
Angara River (
Ангара́) river drains
Lake Baikal and runs 1840 km from the regional capital
Irkutsk to converge with the Yenisei at
Strelka (
). It is dammed in four places to power local industry. The 44m dam at Irkutsk produces 650 MW.
Bratsk lies 500 km downstream, where the 124 m
dam built in the 1960s produces 4500 MW. The resultant reservoir is nicknamed
Dragon Lake because of its outline. The tributary Oka and Iya rivers, which rise on the north slopes of the Eastern
Sayan Mountains, form the 'jaws' and 400 km of the Angara form the 'tail'. There are newer dams almost as large at
Ust-Ilimsk 250 km downstream (also damming the tributary Ilim river) and Boguchany a further 400 km downstream (not operational). Further dams are planned but the environmental consequences of completely taming the Angara are leading to protests which may prevent funding.
Angarsk, the center of the expanding Eastern Siberian oil industry and site of a huge
Yukos-owned refinery, lies 50 km downstream of Irkutsk. A major pipeline takes oil west, and a new one is being built to carry oil east for supply to Japan from the
Sea of Japan port of
Nakhodka. The exact potential of Eastern Siberia is unknown, but two new major fields are the Kovyktinskoye field near Zhigalovo 200 km north of Irkutsk and the extremely remote Verkhnechonskoye field 500 km north of Irkutsk on the
Central Siberian Plateau.


The river as seen from the trans-Siberian railway near Krasnoyarsk
Lower Yenisei
The Great Kaz joins the Yenisei 300 km downstream from Strelka. It is noteworthy for its connection to the
Ob via
Ob-Yenisei canal and Ket River. The river starts to widen, its bed being littered with islands as numerous rivers augment its flow, in particular 1800 km Stony (Podkamennaya) Tunguska, and the 3000 km Lower (Nizhnyaya) Tunguska at
Turukhansk draining the desolate central Siberian Plateau from the east. The remote Tunguska (Тунгуска) region is most famous for the
1908 meteorite impact, but is now being explored for oil. Beyond Turukhansk, the river enters
tundra.
The river is icebound for more than half the year, and if unchecked ice could dam the river causing major flooding. Explosives are used to keep the water flowing. The final town is
Dudinka which is connected to Krasnoyarsk by regular passenger boat. The river widens to a 50 km estuary for its final 250 km and the shipping lanes are kept open by icebreaker.
During the
ice age, the route to the arctic was blocked by ice. Though the exact details are unclear, the Yenisei is believed to have flowed into a huge lake filling much of western Siberia, eventually flowing into the
Black Sea. (See
West Siberian Glacial Lake of the early
Weichselian Glaciation)
Navigation
The first team to navigate the Yenisei's entire length, including its violent upper
tributary in Mongolia, was an Australian-Canadian effort completed in September 2001.
Ben Kozel, Tim Cope,
Colin Angus and Remy Quinter were on this team. Both Kozel and Angus wrote books detailing this expedition, and a documentary was produced for National Geographic Television.
History
Ancient nomadic tribes such as the
Ket people and the
Yugh people lived along its banks. The Ket, numbering about 1000, are the only survivors today of those who originally lived throughout central southern Siberia near the river banks. Their extinct relatives included the Kotts, Assans, Arins, Baikots, and Pumpokols who lived further upriver to the south. The modern Ket lived in the eastern middle areas of the river before being assimilated politically into Russia during the 17th through 19th centuries.
[1]
Notes
Tim Cope's Yenisei River journey was recorded at,
[1]
External links
Coordinates Coordinates:
Lake type Continental rift lake
Primary sources
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Headstream is the origin of water flow that initiates the subject watercourse. It is the start of the river or stream.
The source of a river or stream may be a lake, a marsh, a spring, glacier, or a collection of headwaters.
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AnthemHymn of the Russian Federation
Capital(and largest city) Moscow
..... Click the link for more information. The Darkhad valley (Mongolian: Дархадын хотгор) is a large valley in northwestern Khövsgöl aimag, Mongolia.
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Anthem
"Монгол улсын төрийн дуулал"
National anthem of Mongolia
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Earth's oceans(World Ocean)
- Arctic Ocean
- Atlantic Ocean
- Indian Ocean
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- Southern Ocean
The
Arctic Ocean, located in the northern hemisphere and mostly in the Arctic north polar region, is the smallest of the world's five
..... Click the link for more information. A drainage basin is a region of land where water from rain or snow melt drains downhill into a body of water, such as a river, lake, dam, estuary, wetland, sea or ocean. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from
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AnthemHymn of the Russian Federation
Capital(and largest city) Moscow
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"Монгол улсын төрийн дуулал"
National anthem of Mongolia
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In hydrology, the discharge of a river is the volume of water transported by it in a certain amount of time. The unit used is usually m³/s (cubic meters per second, or cumecs). For example, the average discharge of the Rhine river is 2200 m³/s.
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river is a natural waterway that transits water through a landscape from higher to lower elevations. It is an integral component of the water cycle. The water within a river is generally collected from precipitation through surface runoff, groundwater recharge (as seen at baseflow
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Earth's oceans(World Ocean)
- Arctic Ocean
- Atlantic Ocean
- Indian Ocean
- Pacific Ocean
- Southern Ocean
The
Arctic Ocean, located in the northern hemisphere and mostly in the Arctic north polar region, is the smallest of the world's five
..... Click the link for more information. list of the longest rivers on Earth. It includes river systems over 1,000 kilometers.
Definition of length
The length of a river is not always easy to calculate. It depends on the identification of the source, the identification of the mouth, and the precise measurement of
..... Click the link for more information. Mississippi River Mississippi River in New Orleans.
Country | United States
States |..... Click the link for more information. Origin Confluence of Madison, Gallatin and Jefferson in Montana.
Mouth Mississippi River near St. Louis, Missouri
Basin countries USA, Canada
Length 2,341 miles (3,767 km)
Source elevation 4,045 ft
Mouth elevation 400 ft
Avg.
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Anthem
"Монгол улсын төрийн дуулал"
National anthem of Mongolia
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Kara Sea (Russian: Ка́рское мо́ре) is part of the Arctic Ocean north of Siberia.
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Siberia (Russian: Сиби́рь, Sibir); is a vast region on the eastern and North-Eastern part of the Russian Federation constituting almost all of Northern Asia and comprising a large part of the
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Gulag ( (help) , Russian: ГУЛАГ
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Taiga (IPA pronunciation: /ˈtaɪgə/ or /taɪˈga/, from Mongolian) is a biome characterized by coniferous forests.
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In physical geography, tundra is an area where the tree growth is hindered by low temperatures and short growing seasons. The term "tundra" comes from Kildin Sami tūndâr 'uplands, tundra, treeless mountain tract'.
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Sayan Mountains (Russian: Саяны, Sayany; Kokmen Mountains during the period of the Göktürks[1]) are a mountain range in southern Siberia, Russia.
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The Tannu-Ola mountains (Tuvan: Таңды-Уула Tangdy-Uula mountains) is a mountain range in southern Siberia, in the Tuva Republic of Russia.
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The Darkhad valley (Mongolian: Дархадын хотгор) is a large valley in northwestern Khövsgöl aimag, Mongolia.
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rift is a place where the Earth's crust and lithosphere are being pulled apart. Typical features are a central linear downdropped fault segment, called a graben, with parallel normal faulting and rift-flank uplifts on either side forming a rift valley.
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Anthem
"Монгол улсын төрийн дуулал"
National anthem of Mongolia
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