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The Daugava ( ), also known as the Western Dvina or the Väina River, is a large river rising in the of that flows through and into the Gulf of Riga of the . The Daugava rises close to the source of the . It is in length, of which are in Latvia and in Russia. It is a westward-flowing river, tracing out a great south-bending curve as it passes through northern Belarus. The city of Ķekava is located 6 miles south of the west bank of the river.

Latvia's capital, , bridges the river's four times. Built on both riverbanks, the city centre is from the river's mouth and is a significant port.


Etymology
According to 's Etymological Dictionary, the Dvina cannot stem from a ; instead, it possibly comes from an Indo-European word which used to mean 'river' or 'stream'. The name Dvina strongly resembles which is itself derived from the Proto-Indo-European *dānu, meaning 'large river'.

The Finno-Ugric names Vēna (Livonian), Väinajõgi (Estonian), and Väinäjoki () all stem from *väin, which roughly translates to 'a large, peacefully rolling river'.


Geography
The total catchment area of the river is , of which are in Belarus.


Tributaries
The following rivers are tributaries to the river Daugava (from source to mouth):


History
Humans have settled at the mouth of the Daugava and along the shores of the Gulf of Riga for millennia, initially participating in a hunter-gatherer economy and utilizing the waters of the Daugava estuary for fishing and gathering. Beginning around the sixth century CE, explorers crossed the Baltic Sea and entered the Daugava River, navigating upriver into the Baltic interior. Compare:
(2005). 9781576078006, ABC-CLIO. .

In medieval times, the Daugava was part of the trade route from the Varangians to the Greeks, an important route for the transport of furs from the north and of Byzantine silver from the south. The Riga area, inhabited by the -speaking , became a key location of settlement and defence of the mouth of the Daugava at least as early as the Middle Ages, as evidenced by the now destroyed fort at Torņakalns on the west bank of the Daugava in present-day Riga.

From the end of the great part of the Daugava formed the northeastern border of Duchy of Courland and Semigallia separating it initially from the Kingdom of Livonia, later and . After the incorporation later in the the river formed a border between governorates of Courland on the western bank and Livonia and Vitebsk on the eastern bank.

From 1936 to 1939 Ķegums Hydroelectric Power Station was built on the Daugava river in Latvia. Pļaviņas Hydroelectric Power Station was put into operation in 1968 and Riga Hydroelectric Power Plant in 1974.


Settlements
The following are some of the cities and towns built along the Daugava:


Russia

Belarus

Latvia

Environment
river began experiencing environmental deterioration in the Soviet era due to collective agriculture (producing considerable adverse water pollution runoff) and hydroelectric power projects. This is the river that the Vula river flows into.


Water quality
Upstream of the Latvian town of , the river's pH has a characteristic value of about 7.8 (slight ). In this area, the concentration of ionic calcium is around 43 milligrams per liter, is about 0.82 milligrams per liter, ionic is 0.038 milligrams per liter, and oxygen saturation is 80%. The high nitrate and phosphate load of the Daugava has contributed to the extensive buildup of phytoplankton biomass in the Baltic Sea; the and rivers also contribute to the high nutrient loading of the Baltic.

In Belarus, water pollution of the Daugava is considered moderately severe, with the chief sources being treated wastewater, fish-farming, and agricultural chemical runoff (such as herbicides, pesticides, nitrates, and phosphates).

(2025). 9789264583962 .


Notes

Further reading
  • (2025). 9781576078006, . .
  • Francis W. Carter and David Turnock. 2002. Environmental problems of East Central Europe. 442 pages Google eBook


External links

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