Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a243858e2d527929

Jump to content

Beyenchime

Beyenchime
Беенчиме / Бэйэнчимэ
Course of the Beyenchime ONC map section
Beyenchime is located in Sakha Republic
Beyenchime
Mouth location in Yakutia, Russia
Beyenchime is located in Russia
Beyenchime
Beyenchime (Russia)
Location
CountryRussian Federation
Federal subjectYakutia
DistrictOlenyoksky District
Physical characteristics
Source 
  locationCentral Siberian Plateau
  coordinates71°10′30″N 118°45′33″E / 71.17500°N 118.75917°E / 71.17500; 118.75917
  elevation123 m (404 ft)
MouthOlenyok
  coordinates
70°32′17″N 121°29′21″E / 70.53806°N 121.48917°E / 70.53806; 121.48917
  elevation
21 m (69 ft)
Length311 km (193 mi)
Basin size
4,080 km2 (1,580 sq mi)
Basin features
ProgressionOlenyokLaptev Sea

The Beyenchime (Russian: Беенчиме Yakut: Бэйэнчимэ, Beyençime) is a river in Yakutia (Sakha Republic), Russia. It is a tributary of the Olenyok with a length of 311 kilometres (193 mi). Its drainage basin area is 4,080 square kilometres (1,580 mi2).[1][2]

The river flows north of the Arctic Circle across a lonely, desolate area of the Olenyoksky District devoid of settlements.[3] The Beyenchime-Udzha interfluve is an area where diamonds are found.[4]

Course

[edit]

The Beyenchime is a left tributary of the Olenyok. Its sources are at the limit of the Northern Siberian Lowland, in the vicinity of the sources of the Bur and the Udya. It flows roughly eastwards to the south of the Bur and to the north of the Kuoika. To the south and southwest of its middle course there is a large area dotted with lakes. In its last stretch the Beyenchime turns into the Central Siberian Plateau and heads in a SSE direction until its mouth in the Olenyok, 434 km (270 mi) from its mouth.[3][5][6]

The river is frozen between early October and late May and may cause floods in the summer. Its main tributaries are the 71 kilometres (44 mi) long Beyemchikeen (Бэйэмчикээн) and the 129 kilometres (80 mi) long Beyenchime Salaata (Бэйэнчимэ-Салаата) from the left.[1] There is an impact crater south of the lower course of the Beyenchime Salaata.[7]

See also

[edit]

References

[edit]
  1. 1 2 "Река Бэйэнчимэ in the State Water Register of Russia". textual.ru (in Russian).
  2. "Река Бэйэнчимэ in the State Water Register of Russia". verum.icu (in Russian).
  3. 1 2 Google Earth
  4. Certain characteristics of diamonds from placers in northeastern Siberian Platform
  5. "Топографска карта R-49 50; M 1:1 000 000 - Topographic USSR Chart (in Russian)". Retrieved 21 April 2022.
  6. "Топографска карта R-51 52; M 1:1 000 000 - Topographic USSR Chart (in Russian)". Retrieved 21 April 2022.
  7. Beenchime Salaatinsky crater in northern Yakutia - origin and late quaternary records in the 8-km circular structure
[edit]