Vilyuy Explained

Vilyuy
Other Name:Вилю́й / Бүлүү
Pushpin Map:Russia Sakha Republic
Pushpin Map Caption:Location of the mouth in Yakutia, Russia
Source1 Location:Vilyuy Plateau
Source1 Coordinates:65.9628°N 103.5131°W
Source1 Elevation:520m (1,710feet)
Mouth:Lena
Mouth Coordinates:64.3772°N 126.415°W
Mouth Elevation:55m (180feet)
Subdivision Type1:Country
Subdivision Name1:Russia
Subdivision Type2:Federal subjects
Subdivision Name2:Krasnoyarsk Krai, Yakutia
Length:2650km (1,650miles)
Discharge1 Avg:1700m3/s
Basin Size:454000km2

The Vilyuy (Russian: Вилю́й|p=vʲɪˈlʲʉj; Yakut: Бүлүү, Bülüü, pronounced as /bylyː/) is a river in Russia, the longest tributary of the Lena. About 2650km (1,650miles) long, it flows mostly within the Sakha Republic. Its basin covers about 454000km2.

History

The river is first mentioned in the 17th century in connection with the Russian conquest of Siberia.In 1634, Russian Cossacks, headed by Voin Shakhov, established a winter settlement at the confluence of the rivers Vilyuy and Tyukyan. This settlement served as the administrative center of the area for several decades, after which it was moved to the Yolyonnyokh area 45km (28miles) down by the Vilyuy, where the ostrog (fortified settlement) of Olensk (now Vilyuysk) was founded in 1773.

In the 1950s, diamond deposits were discovered in the area, about 700km (400miles) from its mouth. This led to the construction of the Mir Mine, together with access roads and an airport, and the Vilyuy Dam complex to generate power needed for the diamond concentrators.[1]

Geography

The Vilyuy has its sources in the Vilyuy Plateau, part of the Central Siberian Plateau, in the Evenkiysky District (Krasnoyarsk Krai) and, flowing east, soon enters Sakha. It turns towards the south and southeast in the Central Yakutian Lowland, then back towards the east, and finally enters the Lena about 350km (220miles) downstream of Yakutsk, near Sangar. The Ust-Vilyuy Range rises above the facing bank of the Lena, opposite the mouth of the Vilyuy.[2]

To the west of the Vilyuy and Chona is the Nizhnyaya Tunguska basin.The Vilyuy basin is sparsely populated. Small settlements along the river include Vilyuysk, Verkhnevilyuysk, Suntar, Ekonda and Nyurba.

Tributaries

The main tributaries of the Vilyuy are the Ulakhan-Vava, Chirkuo, Chona, Chybyda, Ulakhan-Botuobuya, Ochchuguy-Botuobuya, Tangnary, Kempendyay, Tonguo and Bappagay on the right; and the Sen, Lakharchana, Akhtaranda, Ygyatta, Markha, Tyukyan, Kosmos https://verum.wiki/wiki/Космос_(значения) and Tyung on the left.[1]

Geology

Vilyuy is associated with geological formations Yakutsk-Vilyuy Rift (Vilyuy Rift Basin) and Yakutsk-Vilyuy LIP (large igneous province), also known as Vilyuy Traps.[3]

See also

External links

Notes and References

  1. A. Gavrilov, Вилюй in: Great Russian Encyclopedia.
  2. http://wikimapia.org/35048117/ru/%D0%A5%D1%80%D0%B5%D0%B1%D0%B5%D1%82-%D0%A3%D1%81%D1%82%D1%8C-%D0%92%D0%B8%D0%BB%D1%8E%D0%B9%D1%81%D0%BA%D0%B8%D0%B9 Хребет Усть-Вилюйский - Wikimapia
  3. http://www.mantleplumes.org/SiberianDykeExtension.html Time correlation between the formation of dyke swarms and crustal extension stages in the Middle Paleozoic Vilyui rift basin, Siberian platform