The Yenisey (Енисе́й, jɪnjɪˈsjej), also romanised as Yenisei or Jenisej, is the fifth-longest river system in the world, and the largest to drain into the Arctic Ocean.
Rising in Mungaragiyn-gol in Mongolia, it follows a northerly course through Lake Baikal and the Krasnoyarsk Dam before draining into the Yenisey Gulf in the Kara Sea. The Yenisey divides the Western Siberian Plain in the west from the Central Siberian Plateau to the east; it drains a large part of central Siberia.
It is the central one of three large Siberian rivers that flow into the Arctic Ocean (the other two being the Ob and the Lena). The maximum depth of the Yenisey is and the average depth is .
The Yenisey proper, from the confluence of its source rivers Great Yenisey and Little Yenisey at Kyzyl to its mouth in the Kara Sea, is long. From the source of its tributary Selenga, it is long. It has a drainage basin of . The Yenisey flows through the Russian federal subjects Tuva, Khakassia and Krasnoyarsk Krai. The city of Krasnoyarsk is situated on the Yenisey.
The largest tributaries of the Yenisey are, from source to mouth:
Little Yenisey (left)
Great Yenisey (right)
Khemchik (left)
Kantegir (left)
Abakan (left)
Tuba (right)
Mana (right)
Bazaikha (right)
Kacha (left)
Kan (right)
Angara (right)
Kem (left)
Bolshoy Pit (right)
Sym (left)
Dubches (left)
Podkamennaya Tunguska (right)
Bakhta (right)
Yeloguy (left)
Nizhnyaya Tunguska (right)
Turukhan (left)
Kureyka (right)
Khantayka (right)
Bolshaya Kheta (left)
Tanama (left)
Lake Baikal
A significant feature of the Upper Yenisei is Lake Baikal, the deepest and oldest lake in the world.
The Brekhovskie Islands (Russian-language article: Бреховские острова) lie in the Yenisey estuary and have an area of some 1,400,000 hectares. They provide a wetland habitat for rare and endangered birds and are an internationally important nesting and breeding area for several types of waterfowl. The most north-easterly of the islands, Nosonovskij Ostrov ("Nose Island") was visited by Fridtjof Nansen in 1913.
This page is automatically generated and may contain information that is not correct, complete, up-to-date, or relevant to your search query. The same applies to every other page on this website. Please make sure to verify the information with EPFL's official sources.
Lake Baikal, with a depth of 1637 m, is characterized by deep-water intrusions that bridge the near-surface layer to the hypolimnion. These episodic events transfer heat and oxygen over large vertical scales and maintain the permanent temperature stratifie ...
Lake Baikal (baɪˈkɑːl,_-ˈkæl ; Ozero Baykal ˈozjɪrə bɐjˈkaɫ; Baigal dalai) is a rift lake in Russia. It is situated in southern Siberia, between the federal subjects of Irkutsk Oblast to the northwest and the Republic of Buryatia to the southeast. With of water, Lake Baikal is the world's largest freshwater lake by volume, containing 22–23% of the world's fresh surface water, more than all of the North American Great Lakes combined. It is also the world's deepest lake, with a maximum depth of , and the world's oldest lake, at 25–30 million years.
Krasnoyarsk Krai (Krasnoyarskiy kray, krəsnɐˈjarskjɪj ˈkraj) is a federal subject of Russia (a krai) located in Siberia. Its administrative center is the city of Krasnoyarsk, the third-largest city in Siberia, after Novosibirsk and Omsk. Comprising half of the Siberian Federal District, Krasnoyarsk Krai is the largest krai in Russia, the second-largest federal subject in the country after neighboring Sakha, and the third-largest country subdivision by area in the world.
The Trans-Siberian Railway, historically known as the Great Siberian Route and often shortened to Transsib, is a large railway system that connects European Russia to the Russian Far East. Spanning a length of over , it is the longest railway line in the world. It runs from the city of Moscow in the west to the city of Vladivostok in the east. During the period of the Russian Empire, government ministers—personally appointed by Alexander III and his son Nicholas II—supervised the building of the railway network between 1891 and 1916.