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Uglich Reservoir

From Wikipedia, the free encyclopedia

Uglich Reservoir
A lock at Uglich Reservoir
Uglich Reservoir is located in Tver Oblast
Uglich Reservoir
Uglich Reservoir
Uglich Reservoir is located in Yaroslavl Oblast
Uglich Reservoir
Uglich Reservoir
Uglich Reservoir is located in European Russia
Uglich Reservoir
Uglich Reservoir
Coordinates57°15′N 37°50′E / 57.250°N 37.833°E / 57.250; 37.833
TypeHydroelectric reservoir
Primary inflowsVolga, Medveditsa, Kashinka, Nerl
Basin countriesRussia
Max. length143 km (89 mi)
Max. width5 km (3.1 mi)
Surface area249 km2 (96 sq mi)
Average depth5 m (16 ft)
Max. depth23 m (75 ft)
Water volume1.24 km3 (0.30 cu mi)
SettlementsKaliazin, Kimry

Uglich Reservoir or Uglichskoye Reservoir (Russian: У́гличское водохрани́лище) is an artificial lake in the upper part of the Volga River formed by the Uglich Hydroelectric Station dam.

It was built in 1939 in the town of Uglich. It is located in Tver and Yaroslavl Oblasts in central Russia.

YouTube Encyclopedic

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  • Kalyazin - a city under water in in 4k UltraHD | Калязин - город под водой в 4к
  • Kalyazin, Tver region, Russia
  • Drowned Church in Kalyazin / Затопленная церковь в Калязине

Transcription

Description

The Uglich Reservoir has a surface area of 249 km2 and a water volume of 1.2 km3. Its length is 143 km, its maximum width is 5 km, and average depth is 5 m (with maximum depth equaling 23 m). The Uglich Reservoir was created for the benefit of transportation, energy, and water supply. It also performs seasonal flow regulation. The towns of Uglich, Kalyazin, and Kimry are located along the reservoir.

Consequences

The construction of the dam led to the 15th-century Intercession monastery in Uglich and 16th-century monastery in Kalyazin being submerged by the artificial lake. The Flooded Belfry is an example of a submerged landmark.

References

This article includes content derived from the Great Soviet Encyclopedia, 1969–1978, which is partially in the public domain.

InternationalNational
This page was last edited on 29 February 2024, at 12:32
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