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Yenisey River

Yenisei River
Enlarge picture
The Yenisei basin, including Lake Baikal
The Yenisei basin, including Lake Baikal
OriginTuva (Russia), Darkhad Valley (Mongolia)
MouthArctic Ocean
Basin countriesRussia, Mongolia
Length5,539 km (3,445 mi)
Avg. discharge19,600 m³/s (692,272 ft³/s)
Basin area2,580,000 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

Main article: Lake Baikal
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

Main article: 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.

Enlarge picture
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

1. ^ Vajda, Edward G.. The Ket and Other Yeniseian Peoples. Retrieved on 2006-10-27.
Tim Cope's Yenisei River journey was recorded at, [1]

External links

Coordinates Coordinates:
Lake type Continental rift lake
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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.

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The Darkhad valley (Mongolian: Дархадын хотгор) is a large valley in northwestern Khövsgöl aimag, Mongolia.
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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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"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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Earth's oceans
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Mississippi River

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Country | United States
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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
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Anthem
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Kara Sea (Russian: Ка́рское мо́ре) is part of the Arctic Ocean north of Siberia.
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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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