Lake Komsomolskoye

Lake Komsomolskoye is a lake in the north of the Leningrad Region Priozersky District, in the middle of the Karelian Isthmus of north eastern Russia. Until 1948 it was called Kiimajärvi (Finnish Kiimajärvi).

Lake Komsomolskoye
Coordinates60°47′N 30°04′E
Typemoraine lake
Primary inflowsPionerka River
Primary outflowsVuoksi River
Catchment area399 km2 (200 sq mi)
Basin countriesRussia
Max. length14 km (9 mi)
Max. width2 km (1 mi)
Surface area24.6 km2 (9 sq mi)
Average depth10 m (33 ft)
Max. depth19.6 m (64 ft)
Water volume246 km3 (59 cu mi)
Surface elevation13 m (43 ft)
Islands46
SettlementsSolovyovka
Torfyanoye

Description

Lake Komsomolskoye is 14 km (8.7 mi) long, 2 km (1.2 mi) miles wide, with a surface area of 24.6 km2 (9 sq mi). The main inflow of the Lake Komsomolskoye is from the Pionerka River. In the south, a small stream flows into the Lake Komsomolskoye. At the northern end, Lake Komsomolskoye is drained by the Vesyolaya River which flows into the Vuoksi River near the village of Vasilyevo. The lake is divided into three plains by two narrowings. The North Pole occupies part of the basin with depths of 6 to 10 meters. There is a small group of islands. Central reach is the deepest, with depressions up to 19.6 meters, the southern shallow, with gentle underwater slopes.

The coastal shallows of the lake are covered with a mixture of sand and silt, the bottom in deep sections is covered with a thick layer of light brown mud. With the exception of the bays, the lake is overgrown with little: the width of the green border near the coast is 10-20 meters.[1]

Geography
See also: Geology of the Baltic Sea and Svecofennian orogeny
Ancylus Lake around 7,000 BC.

Geologically Lake Komsomolskoye is part of the Lake Ladoga depression, a graben and syncline structure of Proterozoic age (Precambrian).[2] Deglaciation following the Weichsel glaciation took place in the Lake Ladoga basin between 12,500 and 11,500 radiocarbon years BP. During the existence of Lake Komsomolskoye there have been three sharp drops in the water level, so that the shore consists of small but distinctive terraces formed on the banks.[3][4] The shores of the lake are indented with several bays and inlets, overgrown with sedges and reeds.[1] On the south-eastern shore of the lake is the village of Solovyovka. At the northern extremity of the lake are the houses of the village of Torfyanoye.

Notoriety
Main article: Ozero

Part of the shore is fenced by the dacha cooperative Ozero, among the founders of which was Vladimir Putin. Access to this territory is closed in violation of the Russian law.[5][6]

gollark: It's fine if you don't care about performance, like haskellers.
gollark: It is a dynamic DNS provider. They provide subdomains and let you automatically set the IP on them.
gollark: No, it's kind of good in some ways, just horrible in others.
gollark: Why not "terminated"-terminated strings?
gollark: Also, you can technically set up your own DNS servers, but nobody else will use them.

References
  1. Kirillova, VA; Raspopov, IM (1971). Lakes of the Leningrad Region. Leningrad: Lenizdat.
  2. Amantov, A.; Laitakari, I.; Poroshin, Ye (1996). "Jotnian and Postjotnian: Sandstones and diabases in the surroundings of the Gulf of Finland" (PDF). Geological Survey of Finland, Special Paper. 21: 99–113. Retrieved 27 July 2015.
  3. Ailio, Julius (1915). "Die geographische Entwicklung des Ladogasees in postglazialer Zeit". Bull. Comm. Géol. Finlande. 45: 1–159.
  4. Davydova, Natalia N. et al. (1996). Late- and postglacial history of lakes of the Karelian Isthmus. Hydrobiologia 322.1–3, 199–204.
  5. Oleg Kashin (2010-07-12). "A picnic of protest". Kommersant.
  6. "Кооператив "Озеро"" [The "Lake" Cooperative] (in Russian). kompromat.ru. March 6, 2000. Retrieved February 20, 2016.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.