Niva (river)
Niva (river) is a topic that has generated great interest in today's society. From its origins until today, it has been the subject of study, debate and analysis in different areas. Its importance lies in its impact on people's daily lives, as well as its relevance in the academic, scientific, social, cultural fields, among others. This article seeks to address in a comprehensive and detailed manner different aspects related to Niva (river), offering a global and updated vision of this topic. Its origins, its evolution over time, its implications in current society and possible future perspectives will be explored.
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| Niva | |
|---|---|
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| Location | |
| Country | Russia |
| Physical characteristics | |
| Source | Lake Imandra |
| Mouth | White Sea |
• coordinates | 67°07′54″N 32°25′22″E / 67.1317°N 32.4229°E |
| Length | 36 km (22 mi) |
| Basin size | 12,830 km2 (4,950 sq mi) |
The Niva (Russian: Нива, Northern Sami: Njavejohka) is a river in the Murmansk Oblast in Russia. It is 36 kilometres (22 mi) long, and has a drainage basin of 12,830 square kilometres (4,950 sq mi).[1] The Niva flows out of the Lake Imandra and into the Kandalaksha Gulf of the White Sea. The town of Kandalaksha is located in the estuary of the Niva.
Its maximum depth is 24 feet (7.3 m).
Between 1936 and 1954 three hydroelectric power stations were built on the Niva. Total capacity is 240 MW and annual power production 1390 GWh.
References
- ^ "Река НИВА in the State Water Register of Russia". textual.ru (in Russian).
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