Related Items
Encarta Search
Search Encarta about Yenisey

Windows Live® Search Results

  • Yenisey

    One of the main rivers in Russia, rising in the Sayan Mountains in the Asian Tuva region and flowing generally north through the Central Siberian Plateau into the Arctic Ocean ...

  • Yenisey - Hutchinson encyclopedia article about Yenisey

    Yenisey. One of the main rivers in Russia, rising in the Sayan Mountains in the Asian Tuva region and flowing generally north through the Central Siberian Plateau into the Arctic ...

  • Yenisey

    Yenisey. Yenisey was a 90 m long Russian mine-layer ship, launched in 1910. On June 4, 1915, she was torpedoed by the German submarine U-26 off the Estonian coast, which at ...

See all search results in
Windows Live® Search Results

Yenisey

Encyclopedia Article
Multimedia
Russian Barge on the Yenisey RiverRussian Barge on the Yenisey River
Dynamic Map
Map of Yenisey

Yenisey, river, central Siberian Russia, about 4,093 km (2,543 mi) long. It is formed in the Sayan Mountains by the union of the Biy-Khem (Greater Yenisey) and the Ka-Khem (Little Yenisey), in the eastern part of Tuva, and flows generally north. The Yenisey flows swiftly through a deep gorge in the Sayan Mountains. Less turbulent just south of Krasnoyarsk, it traverses successively a grain-growing region; the taiga, a region of coniferous forests; and the tundra. It empties into Yenisey Gulf, an arm of the Kara Sea; its estuary is 160 km (100 mi) long and has a maximum width of 64 km (40 mi). The Yenisey drains more than 2.6 million sq km (1 million sq mi); the average discharge at its mouth is 19.8 million litres (4.35 million gallons) per second. Although navigable for about 2,900 km (1,800 mi), it is usually frozen from November to May. The chief tributaries of the Yenisey are the Kan, the Angara, the Kureyka, the Abakan, and the Upper (Verkhnyaya Tunguska), Stony Tunguska (Podkamennaya Tunguska), and Lower Tunguska (Nizhnyaya Tunguska) rivers.

Find in this article
View printer-friendly page
E-mail




© 2008 Microsoft