, be|Заходняя Дзвіна (), liv|Vēna, et|Väina, german: Düna
|image = Fluss-lv-Düna.png
|image_caption = The drainage basin of the Daugava
|source1_location = Valdai Hills
|mouth_location = Gulf of Riga
, Baltic Sea
|subdivision_type1 = Country
|subdivision_name1 = Belarus
The Daugava ( ltg|Daugova; russian: Западная Двина (Západnaya Dviná), meaning "Western Dvina"; pl|Dźwina), is a large river rising in the Valdai Hills
that flows through Belarus
into the Gulf of Riga
of the Baltic Sea
. It rises close to the source of the Volga
. Its length is 1,020 km (630 mi),
of which 325 km (202 mi) are in Russia. It is a westward-flowing river, tracing out a great curve towards its south which means it passes through northern Belarus.
Latvia's capital, Riga
bridges the estuary four times, lying on both banks, the city centre being from the mouth and being a significant port.
The total catchment area of the river is , of which are within Belarus
The following rivers are tributaries to the river Daugava (from source to mouth):
, Drysa, Dubna
According to Max Vasmer
's ''Etymological Dictionary'', the toponym
Dvina clearly cannot stem from a Uralic language
, and it possibly comes from an Indo-European
word which used to mean ''river'' or ''stream''.
The river began experiencing environmental deterioration in the era of Soviet collective agriculture (producing considerable adverse water pollution runoff) and a wave of hydroelectric power projects.
Cities, towns and settlements
, Zapadnaya Dvina
with Boris stones
strewn in the vicinity, Navapolatsk
, and Druya
Humans have settled at the mouth of the Daugava and around the other shores of the Gulf of Riga for millennia, initially participating in a hunter-gatherer economy and utilizing the waters of the Daugava estuary as fishing and gathering areas for aquatic biota. Beginning around the sixth century AD, Viking
explorers crossed the Baltic Sea and entered the Daugava River, navigating upriver into the Baltic interior.
In medieval times the Daugava was an important area of trading and navigation - part of the trade route from the Varangians to the Greeks
- for transport of furs from the north and of Byzantine
silver from the south. The Riga area, inhabited by the Finnic
, became a key element 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 at present day Riga. Since the Late Middle Ages the western part of the Daugava basin has come under the rule of various peoples and states; for example the Latvian town of Daugavpils
, located on the western Daugava, variously came under papal rule as well as Slavonic, Polish, German and Russian sway until restoration of the Latvian independence
in 1990 at the end of the Cold War.
Upstream of the Latvian town of Jekabpils
has a characteristic value of about 7.8 (slight alkaline
); in this reach the calcium ion has a typical concentration of around 43 milligrams per liter; nitrate has a concentration of about 0.82 milligrams per liter (as nitrogen); phosphate ion is measured at 0.038 milligrams per liter; and oxygen saturation was measured at eighty percent. The high nitrate and phosphate load of the Daugava is instrumental to the buildup of extensive phytoplankton biomass in the Baltic Sea; other European rivers contributing to such high nutrient loading of the Baltic are the Oder and Vistula Rivers.
In Belarus, water pollution of the Daugava is considered moderately severe, with the chief sources being treated wastewater, fish-farming and agricultural chemical runoff (e.g. herbicides, pesticides, nitrate and phosphate).
*Francis W. Carter and David Turnock. 2002. Environmental problems of East Central Europe. 442 pages Google eBook
Daugava River photos
Category:International rivers of Europe
Category:Rivers of Belarus
Category:Rivers of Latvia
Category:Gulf of Riga
Category:Rivers of Smolensk Oblast
Category:Rivers of Tver Oblast
Category:Rivers of Vitebsk Region