In today's world, Ozhogina has gained unprecedented relevance. Whether as a protagonist on the political scene, as a central topic in academic debates or as a cultural phenomenon, Ozhogina has managed to capture the attention of a wide spectrum of society. Its influence extends to different areas, from the economy to people's daily lives. In this article, we will explore the various facets of Ozhogina, analyzing its impact on different aspects of modern life and examining the reasons behind its increasing relevance.
| Ozhogina Yakut: Одьуогун | |
|---|---|
Location in the Sakha Republic, Russia | |
| Location | |
| Country | Russia |
| Physical characteristics | |
| Source | |
| • location | confluence of Sulakkan and Delkyu |
| • elevation | 109 m (358 ft) |
| Mouth | Kolyma |
• coordinates | 66°13′10″N 151°05′24″E / 66.21944°N 151.09000°E |
• elevation | 21 m (69 ft) |
| Length | 523 km (325 mi) |
| Basin size | 24,300 square kilometres (9,400 sq mi) |
The Ozhogina (Russian: Ожогина; Yakut: Одьуогун, Ocuogun) is a tributary of the Kolyma in eastern Siberia. The river is 523 kilometres (325 mi) long. The area of its basin is 24,300 square kilometres (9,400 mi2).[1]
It is formed by the confluence of two rivers: Sulakkan and Delkyu, which sources are located on the northern slopes of the Moma Range.[2] It flows eastwards south of the Alazeya Plateau.[3] The river is winding, there are more than 2,800 lakes in its basin. The river valley is covered with sparse larch taiga. It is covered with ice in October. The ice breaks up in May. The river is fed by snow and rain. The major tributaries are Chyocholyugyun and Khoska.[4]