Beyenchime
| Beyenchime Беенчиме / Бэйэнчимэ | |
|---|---|
| File:Beyenchime ONC C-5.jpg Course of the Beyenchime ONC map section | |
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| Location | |
| Country | Russian Federation |
| Federal subject | Yakutia |
| District | Olenyoksky District |
| Physical characteristics | |
| Source | |
| • location | Central Siberian Plateau |
| • coordinates | Lua error: callParserFunction: function "#coordinates" was not found. |
| • elevation | 123 m (404 ft) |
| Mouth | Olenyok |
• coordinates | Lua error in Module:Coordinates at line 489: attempt to index field 'wikibase' (a nil value). |
• elevation | 21 m (69 ft) |
| Length | 311 km (193 mi) |
| Basin size | 4,080 km2 (1,580 sq mi) |
| Basin features | |
| Progression | Olenyok→Laptev 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 | edit source]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 | edit source]References
[edit | edit source]- ^ a b Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ a b Google Earth
- ^ Certain characteristics of diamonds from placers in northeastern Siberian Platform
- ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ Beenchime Salaatinsky crater in northern Yakutia - origin and late quaternary records in the 8-km circular structure
External links
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