Yenisei River (Енисей) | |
River | |
Bii-Hem and Ka-Hem near Kyzyl
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Tributaries | |
- right | Angara, Lower Tunguska |
Cities | Kyzyl, Shagonar, Sayanogorsk, Abakan, Divnogorsk, Krasnoyarsk, Yeniseysk, Lesosibirsk, Igarka, Dudinka |
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Source | Mungaragiyn-Gol |
- location | ridge Dod-Taygasyn-Noor, Mongolia |
- elevation | 3,351 m (10,994 ft) |
- length | 748 km (465 mi) |
- coordinates | |
Mouth | Yenisei Gulf |
- location | Kara Sea, Arctic ocean, Russia |
Length | 5,539 km (3,442 mi) |
Basin | 2,580,000 km² (996,144 sq mi) |
Discharge | for Yenisei Gulf[1] |
- average | 19,600 m3/s (692,167 cu ft/s) |
- max | 190,000 m3/s (6,709,787 cu ft/s) |
- min | 2,700 m3/s (95,350 cu ft/s) |
The Yenisei basin, including Lake Baikal
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Yenisei (Russian: Енисе́й), also written as Yenisey[2], is the greatest river system flowing to the Arctic Ocean. Rising in Mongolia, it follows a northerly course to the Yenisei Gulf in 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.
The maximum depth of the Yenisei River is 80 feet (24 m) and the average depth is 45 feet (14 m). The depth of river outflow is 106 feet (32 m) and inflow is 101 feet (31 m).
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See also:
The 200 mi (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(500 km) downstream, where the 407 ft (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 250 mi (400 km) of the Angara forms the 'tail'. There are newer dams almost as large at Ust-Ilimsk 155 mi (250 km) downstream (also damming the tributary Ilim river) and Boguchany a further 250 mi (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 31 mi (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 125 mi (200 km) north of Irkutsk and the extremely remote Verkhnechonskoye field 310 mi (500 km) north of Irkutsk on the Central Siberian Plateau.
The Great Kaz joins the Yenisei 186 mi (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 1,120 mi (1,800 km) Stony (Podkamennaya) Tunguska, and the 1,860 mi (3,000 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 territory.
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 31 mi (50 km) estuary, the Yenisei Gulf, for its final 155 mi (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)
The Yenisei River valley is habitat for numerous flora and fauna, with Siberian pine and Siberian larch being notable tree species. In prehistoric times Scots pine, Pinus sylvestris was abundant in the Yenisei River valley circa 6000 BC.[3] There are also numerous bird species present in the watershed, including, for example the Hooded crow, Corvus cornix.[4]
The first team to navigate the Yenisey'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[5], and a documentary was produced for National Geographic Television.
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.[6]
Russians first reached the upper Yenisei in 1605, travelling from the Ob River, up the Ket River, portaging and then down the Yenisei as far as the Sym River. In 1607 they went east up the Angara River and in 1608 south towards Krasnoyarsk. Yeniseisk at the Ket-Angara junction was founded in 1619 and Krasnoyarsk upriver in 1628. In 1607 the lower Yenisei was reached from Mangazeya, with the founding Turukhansk at the mouth of the Lower Tunguska. The mouth of the Yenisey was reached in 1610 and the Stony Tunguska some time before 1626.
During World War II, Nazi Germany and the Japanese Empire agreed to divide Asia along a line that followed the Yenisei River to the border of China, and then along the border of China and the Soviet Union, the northern and western borders of Afghanistan, and the border between Iran and India (what is now Pakistan was then part of India). Nazi Germany planned to establish a Reichskommissariat West Sibirien between the Ural Mountains and the Yenisei River for housing in concentration camps as slave labor for industrial enterprises those Slavs who were not being worked as slaves on the estates of the German farmers west of the Urals. [7] Since the Axis lost World War II, this plan was never implemented.
the bridge over the Yenisei in Krasnoyarsk, Russia, view from the left bank |
Vantovyjj most, the bridge in Krasnoyarsk, Russia, view from the left bank |
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Tim Cope's Yenisei River journey was recorded at, http://www.timcopejourneys.com/index.pl?page=44
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