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The Vuoksi (, historically: "Uzerva"; ; ; ) is a river running through the northernmost part of the from in southeastern to in northwestern . The river enters Lake Ladoga in three branches, an older main northern branch at (Käkisalmi), a smaller branch a few kilometers to the north of it, and a new southern branch entering further southeast as (Finnish: Taipaleenjoki), which has become the main stream in terms of water discharge. Since 1857, the old northern distributaries drain only the lower reaches of the Vuoksi basin and are not fed by Lake Saimaa. The northern and southern branches actually belong to two separate river systems, which at times get isolated from each other in dry seasons.

The descent between Lake Saimaa and Lake Ladoga is . The entire run of the river is via the Priozersk branch, or via the Taipale (Burnaya) branch. It has a of . For most of its length, the river broadens out to a series of lakes bound together by shorter riverlike connections. One of these lakes, Uusijärvi close to Priozersk, was renamed ' in the .

The Vuoksi connects Lake Ladoga with central Finland, and was once an important route for trade and communication. A western branch, which disappeared due to ongoing land uplift, was an alternative route for the to reach the Gulf of Finland when the was blocked by enemies. Now the bypasses the Vuoksi and enters the Gulf of Finland in the Bay of Vyborg near the medieval city of .

During both the and the river Vuoksi was a major Finnish against the Soviet advance. The and were located along the northern shore of its southern armlet.

From the Industrial Revolution, power generated from Vuoksi's rapids made the Vuoksi region Finland's industrial center in the late 19th century. Since the Winter War (1940), the Karelian Isthmus has belonged to Russia and only of the river's length remains in Finland. The major at Tainionkoski and Imatra are on the Finnish side in the city of .

The river's surroundings, including the (formerly: Käkisalmi), is a popular resort for 's residents.

The river is famous for its , for instance in Imatra and rapid in the village of Losevo (Kiviniemi). The rapid junction of the Vuoksi and Suvanto/Lake Sukhodolskoye at Losevo is a popular area for , and competitions.

A project is currently being discussed in Russia to destroy the rapids at Losevo and turn the River Burnaya, Lake Sukhodolskoye and lower portions of Vuoksi into a navigable canal, which would connect Lake Ladoga to the Gulf of Finland and allow to bypass River Neva and the city of Saint Petersburg.


Geological history
Around 5,000 BP the waters of the penetrated Salpausselkä, forming the river emptying into Lake Ladoga in its northwestern corner and raising the level of the latter by . Lake Ladoga transgressed, flooding lowland lakes and the Vuoksi, and connected with the at , to the east of present-day . Ladoga's level gradually sank and the River Neva, originating around 3100–2400 BP, drained its waters into the Gulf of Finland; but the Vuoksi still had a significant direct outflow connection to the Bay of Vyborg, possibly as late as in the 16th or 17th century AD. The connection disappeared due to ongoing land uplift.Davydova, Natalia N. et al. (1996). Late- and postglacial history of lakes of the Karelian Isthmus. 322.1-3, 199-204.Saarnisto, Matti & Tuulikki Grönlund (1996). Shoreline displacement of Lake Ladoga - new data from Kilpolansaari. 322.1-3, 205-215.Saarnisto, Matti (1970). The Late Weichselian and Flandrian history of the Saimaa Lake complex. Societas Scientiarium Fennicae. Commentationes Physico-Mathematicae 37.

In 1818, a canal was dug to drain spring flood waters from (now Lake Sukhodolskoye, a long narrow lake in the eastern part of the ) into Lake Ladoga; the canal unexpectedly eroded and turned into (now Burnaya River). The Taipaleenjoki started draining Suvanto and decreased its level by . Originally Lake Suvanto flowed into the Vuoksi through a waterway at Kiviniemi (now Losevo), but as a result of the change, the waterway dried out. In 1857 a channel was dug there, but the stream reversed direction, creating and rendering navigation at Kiviniemi impossible. Since 1857 Suvanto and Taipaleenjoki have constituted the southern branch of the Vuoksi, which has decreased the level of the original northern branch emptying into Ladoga near (now Priozersk) by and has become the main stream.


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