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The Vistula (; ) is the longest river in and the ninth-longest in Europe, at in length. Its , extending into three other countries apart from Poland, covers , of which is in Poland. Statistical Yearbook of the Republic of Poland 2017, Statistics Poland, p. 85-86

The Vistula rises at Barania Góra in the south of Poland, above sea level in the (western part of Carpathian Mountains), where it begins with the White Little Vistula ( Biała Wisełka) and the Black Little Vistula ( Czarna Wisełka). Barania Góra - Tam, gdzie biją źródła Wisły at PolskaNiezwykla.pl It flows through Poland's largest cities, including Kraków, , , Płock, Włocławek, Toruń, , Świecie, Grudziądz, and Gdańsk. It empties into the ( Zalew Wiślany) or directly into the Gdańsk Bay of the with a of six main branches (, , Śmiała Wisła, Martwa Wisła, and ).

The river has many associations with Polish culture, history and national identity. It is Poland's most important waterway and natural symbol, flowing through its two main cities (Kraków and ), and the phrase "Land on the Vistula" () can be synonymous with Poland.

(2016). 9788324030743, Otwarte. .
(2006). 9788322725030, Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej. .
Historically, the river was also important for the and German () peoples.

The Vistula has given its name to the last glacial period that occurred in northern Europe, approximately between 100,000 and 10,000 BC, the Weichselian glaciation.


Etymology
The name Vistula first appears in the written record of (3.33) in AD40. Pliny in AD77 in his Natural History names the river Vistla (4.81, 4.97, 4.100). The root of the name Vistula is often thought to come from Proto-Indo-European : 'to ooze, flow slowly' (cf. अवेषन् "they flowed", veisa "slime"), and similar elements appear in many European river-names (e.g. Svislach (Berezina), Svislach (Neman), , Viešinta).D.Q. Adams, Encyclopedia of Indo-European Culture (London: Fitzroy–Dearborn, 1997), 207.

In writing about the river and its peoples, uses Greek spelling: Ouistoula. Other ancient sources spell the name Istula. Ammianus Marcellinus referred to the Bisula (Book22) in the 380s. In the sixth century ( 5 & 17) used Viscla.

The Anglo-Saxon poem refers to the Wistla. The 12th-century Polish chronicler Wincenty Kadłubek Latinised the river's name as Vandalus, a form presumably influenced by Lithuanian vanduõ 'water'. Jan Długosz (1415–1480) in his Annales seu cronicae incliti regni Poloniae contextually points to the river, stating "of the eastern nations, of the Polish east, from the brightness of the water the White Water...so named" (Alba aqua),Długosz, Jan. Annales seu cronicae incliti regni Poloniae a nationibus orientalibus Polonis vicinis, ob aquae candorem Alba aqua ... nominatur perhaps referring to the White Little Vistula (Biała Wisełka).

In the course of history the river has borne similar names in different languages: ; ; ; ; and .


Sources
Vistula rises in the southern Silesian Voivodeship close to the tripoint involving the and from two sources: Czarna ("Black") Wisełka at altitude and Biała ("White") Wisełka at altitude .Żaneta Kosińska: Rzeka Wisła. Both are on the western slope of Barania Góra in the in Poland.
(2025). 9788323996071, Główny Urząd Geodezji i Kartografii.


Geography
Vistula can be divided into three parts: upper, from its sources to ; central, from Sandomierz to the confluences with the river and the river; and bottom, from the confluence with Narew to the sea.

The Vistula river basin covers (in Poland ); its average altitude is above sea level. In addition, the majority of its river basin (55%) is 100 to 200 m above sea level; over of the river basin ranges from in altitude. The highest point of the river basin is at (Gerlach Peak in the ). One of the features of the river basin of the Vistula is its asymmetry—in great measure resulting from the tilting direction of the Central European Lowland toward the northwest, the direction of the flow of glacial waters, and considerable predisposition of its older base. The asymmetry of the river basin (right-hand to left-hand side) is 73–27%.

The most recent glaciation of the , which ended around 10,000 BC, is called the Vistulian glaciation or Weichselian glaciation in regard to north-central Europe.


Major cities
Wisła (Silesian Voivodeship)river source: Biała Wisełka and Czarna Wisełka
Ustroń
SkoczówBrennica
Strumień
Goczałkowice-Zdrój
Czechowice-DziedziceBiała
Vistula, Soła
OświęcimSoła
Zator
Kraków (Cracow)Sanka, Rudawa, Prądnik, Dłubnia, Wilga (most are canalized streams)
Niepołomice
Nida
PołaniecCzarna
Baranów SandomierskiBabolówka
Koprzywianka, Trześniówka
Sanna
Józefów nad Wisłą
Solec nad Wisłą
Bystra
PuławyKurówka
Dęblin
WilgaWilga
Góra KalwariaCzarna
, JózefówŚwider
Konstancin-JeziornaJeziorka
Żerań canal (incl. several smaller streams)
Łomianki
Modlin
Czerwińsk nad Wisłą
Wyszogród
PłockSłupianka, Rosica, Brzeźnica, ,
Dobrzyń nad Wisłą
WłocławekZgłowiączka
Mień
ToruńDrwęca, Bacha
(canalized)
Chełmno
Świecie
Grudziądz
Wierzyca
, Gdańsk (Sobieszewo Island)Szkarpawa, Martwa Wisła


Delta
The river forms a wide delta called Żuławy Wiślane, or the "Vistula Fens" in English. The delta currently starts around Biała Góra near , about from the mouth, where the river splits off. The also starts separately as a river named (on this map ) Alte Nogat (Old Nogat) south of , but further north it picks up water from a crosslink with the Vistula, and becomes a of the Vistula, flowing away northeast into the (Polish: Zalew Wiślany) with a small delta. The Nogat formed part of the border between East Prussia and interwar Poland. The other channel of the Vistula below this point is sometimes called the .

Various causes (rain, snow melt, ) have caused many severe floods of the Vistula over the centuries. Land in the area was sometimes depopulated by severe flooding, and later had to be resettled.

See (Figure 7, on page 812 at History of floods on the River Vistula) for a reconstruction map of the delta area as it was around the year 1300: note much more water in the area, and the west end of the Vistula Lagoon (Frisches Haff) was bigger and nearly continuous with the .


Channel changes
As with some rivers, the lower Vistula has been subject to channel changing.

Near the sea, the Vistula was diverted sideways by coastal sand as a result of and split into an east-flowing branch (the Elbing (Elbląg) Vistula, Elbinger Weichsel, Szkarpawa, flows into the Vistula Lagoon, now for flood control closed to the east with a lock) and a west-flowing branch (the Danzig (Gdańsk) Vistula, Przegalinie branch, reached the sea in Danzig). Until the 14th century, the Elbing Vistula was the bigger.

  • 1242: The Stara Wisła (Old Vistula) cut an outlet to the sea through the barrier near Mikoszewo where the Vistula Cut is now; this gap later closed or was closed.
  • 1371: The Danzig Vistula became bigger than the Elbing Vistula.
  • 1540 and 1543: Huge floods depopulated the delta area, and afterwards the land was resettled by Germans, and economic development followed.
  • 1553: By a plan made by Danzig and , a channel was dug between the Vistula and the Nogat at Weissenberg (now Biała Góra). As a result, most of the Vistula water flowed down the Nogat, which hindered navigation at Danzig by lowering the water level; this caused a long dispute about the river water between Danzig on one side and Elbing and on the other side.
  • 1611: Great flood near Marienburg.
  • 1613: As a result, a royal decree was issued to build a dam at Biała Góra, diverting only a third of the Vistula's water into the Nogat.
  • 1618–1648 Thirty Years' War and 1655–1661 Second Northern War: In wars involving Sweden the river works at Biała Góra were destroyed or damaged.
  • 1724: Until this year the Vistula in Danzig flowed to sea straight through the east end of the . This year it started to turn west to flow south of the Westerplatte.
  • 1747: In a big flood the Vistula broke into the Nogat.
  • 1772: First Partition of Poland: Prussia got control of the Vistula delta area.
  • 1793: Second Partition of Poland: Prussia got control of more of the Vistula drainage area.
  • 1830 and later: Cleaning the riverbed; eliminating meanders; re-routing some tributaries, e.g. the Rudawa.
  • 1840: A flood caused by an ice-jam formed a shortcut from the Danzig Vistula to the sea (shown as Durchbruch v. J 1840 (Breakthrough of year 1840), on this map), a few miles east of and bypassing Danzig, now called the Śmiała Wisła or Wisła Śmiała ("Bold Vistula"). The Vistula channel west of this lost much of its flow and was known thereafter as the Dead Vistula (German: Tote Weichsel; Polish: Martwa Wisła).
  • 1848 or after: In flood control works the link from the Vistula to the Nogat was moved 4 km (2.5 miles) downstream. In the end, the Nogat got a fifth of the flow of the Vistula.
  • 1888: A large flood in the Vistula delta.
  • 1889 to 1895: As a result, to try to stop recurrent flooding on the lower Vistula, the Prussian government constructed an artificial channel about east of Danzig (now named Gdańsk), known as the Vistula Cut (German: Weichseldurchstich; Polish: Przekop Wisły) (ref map ) from the old fork of the Danzig and Elbing Vistulas straight north to the Baltic Sea, diverting much of the Vistula's flow. One main purpose was to let the river easily flush floating ice into the sea to avoid ice-jam floods downstream. This is now the main mouth of the Vistula, bypassing Gdańsk; Google Earth shows only a narrow new connection with water-control works with the old westward channel. The name Dead Vistula was extended to mean all of the old channel of the Vistula below this diversion.
  • 1914–1917: The Elbing Vistula (Szkarpawa) and the Dead Vistula were cut off from the new main river course with the help of locks.
  • 1944–1945: Retreating WWII German forces destroyed many flood-prevention works in the area. After the war, Poland needed over ten years to repair the damage.

GdańskMotława, , In the city the river divides into several separate branches that reach the Baltic Sea at different points, the main branch reaches the sea at
ElblągElblągshortly before reaching


Tributaries
List of right and left tributaries with a nearby city, from source to mouth:
Right tributaries
  • Brennica—Skoczów
  • Iłownica
  • Biała—Czechowice-Dziedzice
  • Soła
  • —Zator
  • Wilga—Kraków
  • Drwinka
  • Raba
  • Gróbka
  • Uszwica
  • Kisielina
  • Breń
  • Brnik
  • Wisłoka
  • Babulówka—Baranów Sandomierski
  • Trześniówka—
  • Łęg—
  • Sanna—
  • Wyżnica—Józefów
  • Chodelka
  • Bystra—
  • Kurówka—Puławy
  • —Dęblin
  • Okrzejka
  • Promnik
  • Wilga—Wilga
  • Świder—, Józefów
  • Kanał Żerański—
  • —Nowy Dwór Mazowiecki
  • Mołtawa
  • Słupianka—Płock
  • Rosica—Płock
  • Brzeźnica—Płock
  • —Płock
  • Mień—
  • Drwęca—Toruń
  • Bacha—Toruń
  • Struga
  • Osa—Grudziądz
  • Liwa
Left tributaries


Climate change and the flooding of the Vistula delta
According to flood studies carried out by Zbigniew Pruszak, who is the co-author of the scientific paper Implications of SLR and further studies carried out by scientists attending Poland's Final International ASTRA Conference, and predictions stated by climate scientists at the climate change pre-summit in , it is highly likely most of the Vistula Delta region (which is below sea level) will be flooded due to the sea level rise caused by climate change by 2100.


Geological history
The history of the River Vistula and its valley spans over 2 million years. The river is connected to the geological period called the , in which distinct cooling of the climate took place. In the last million years, an ice sheet entered the area of Poland eight times, bringing along with it changes of reaches of the river. In warmer periods, when the ice sheet retreated, the Vistula deepened and widened its valley. The river took its present shape within the last 14,000 years, after the complete recession of the Scandinavian ice sheet from the area. At present, along with the Vistula valley, erosion of the banks and collecting of new deposits are still occurring.Państwowy Instytut Geologiczny ( State Geological Institute), Warsaw, "Geologiczna Historia Wisły"

As the principal river of Poland, the Vistula is also in the centre of Europe. Three principal geographical and geological land masses of the continent meet in its river basin: the Eastern European Plain, Western Europe, and the Alpine zone to which the Alps and the belong. The Vistula begins in the Carpathian mountains. The run and character of the river were shaped by ice sheets flowing down from the Scandinavian peninsula. The last ice sheet entered the area of Poland about 20,000 years ago. During periods of warmer weather, the ancient Vistula, "Pra-Wisła", searched for the shortest way to the sea—thousands of years ago it flowed into the somewhere at the latitude of contemporary Scotland. The climate of the Vistula valley, its plants, animals, and its very character changed considerably during the process of glacial retreat.R. Mierzejewski, Państwowa Wyższa Szkoła Filmowa, Telewizyjna I Teatralna im. Leona Schiller w Łodzi, Narodziny rzeki

Wodospad Wiselka Biala.jpg|Biała Wisełka Wisla 010.jpg|Vistula in southern Poland with the Dolina-dolnej-wisly-2.jpg|Vistula in northern Poland File:Przekop Wisly aerial 2.jpg|Przekop Wisły Bogdan Cierpisz, Wiślany Brzeg, 1989, olej na płótnie, 60x75cm.jpg| Vistula Shore, painted by Bogdan Cierpisz in 1898, oil on canvas


Navigation
Vistula is navigable from the Baltic Sea to (where the joins the river). It can accommodate modest river vessels of class II. Farther upstream the river depth lessens. Although a project was undertaken to increase the traffic-carrying capacity of the river upstream of Warsaw by building a number of locks in and around Kraków, this project was not extended further, so that navigability of the Vistula remains limited. The potential of the river would increase considerably if a restoration of the east–west connection via the waterways were considered. The shifting economic importance of parts of Europe may make this option more likely.

Vistula is the northern part of the proposed E40 waterway, continuing eastward into the , linking the to the .


Historical relevance
Large parts of the Vistula Basin were occupied by the Iron Age and Przeworsk cultures in the first millennium BC. Genetic analysis indicates that there has been an unbroken genetic continuity of the inhabitants over the last 3,500 years. The Vistula Basin along with the lands of the , , , and came to be called by Roman authors of the first century AD. This does not imply that the inhabitants were "" in the modern sense of the term; , when describing the , and , wrote that he was not sure if he should call them Germans, since they had settlements and they fought on foot, or rather since they have some similar customs to them. , in the second century AD, would describe the Vistula as the border between and .

Vistula River used to be connected to the , and thence to the via the Augustów Canal, a technological marvel with numerous contributing to its aesthetic appeal. It was the first waterway in to provide a direct link between the two major rivers, the Vistula and the . It provided a link with the to the south through the , , Berezina Canal, and . The Baltic Sea– Vistula– Dnieper– Black Sea route with its rivers was one of the most ancient trade routes, the , on which amber and other items were traded from to Greece, Asia, , and elsewhere.

The Vistula estuary was settled by in the seventh and eighth century.

(1999). 9788390618487, Zamek Książąt Pomorskich.
p.29
Based on archeological and linguistic findings, it has been postulated that these settlers moved northward along the Vistula River. This however contradicts another hypothesis supported by some researchers saying the moved westward from the Vistula delta.

A number of formed small dominions beginning in the eighth century, some of which coalesced later into larger ones. Among the tribes listed in the Bavarian Geographer's ninth-century document was the ( Wiślanie) in southern Poland. Kraków and Wiślica were their main centres.

Many are connected with the Vistula river and the beginnings of Polish statehood. One of the most enduring is that about co nie chciała Niemca ( who rejected the German). According to the most popular variant, popularized by the 15th-century historian Jan Długosz, p.84 Wanda, daughter of , became queen of the Poles upon her father's death. She refused to marry a German prince Rytigier (Rüdiger), who took offence and invaded Poland, but was repelled. Wanda however committed , drowning in the Vistula River, to ensure he would not invade her country again.


Main trading artery
For hundreds of years the river was one of the main trading arteries of Poland, and the castles that line its banks were highly prized possessions. , , , and building stone were among goods shipped via that route between the 10th and 13th centuries.

In the 14th century the lower Vistula was controlled by the Order, invited in 1226 by Konrad I of Masovia to help him fight the pagan Prussians on the border of his lands. In 1308 the Teutonic Knights captured the Gdańsk castle and murdered the population. Since then the event is known as the Gdańsk slaughter. The Order had inherited from Sambor II, thus gaining a foothold on the left bank of the Vistula.

(1995). 9780521362894, Cambridge University Press. .
Many granaries and storehouses, built in the 14th century, line the banks of the Vistula. In the 15th century the city of Gdańsk gained great importance in the Baltic area as a centre of merchants and trade and as a port city. At this time the surrounding lands were inhabited by Pomeranians, but Gdańsk soon became a starting point for German settlement of the largely fallow Vistulan country.
(1978). 9780710086471, Routledge.
p.35

Before its peak in 1618, trade increased by a factor of 20 from 1491. This factor is evident when looking at the tonnage of grain traded on the river in the key years of: 1491: 14,000; 1537: 23,000; 1563: 150,000; 1618: 310,000. a: p. 6, b: p. 7, c: p. 5, d: p. 5

In the 16th century most of the grain exported was leaving Poland through Gdańsk, which because of its location at the end of the Vistula and its tributary waterway and of its Baltic seaport trade role became the wealthiest, most highly developed, and by far the largest centre of crafts and manufacturing, and the most autonomous of the Polish cities. Other towns were negatively affected by Gdańsk's near-monopoly in foreign trade. During the reign of Stephen Báthory Poland ruled two main ports: Gdańsk controlling the Vistula river trade and controlling the trade. Both cities were among the largest in the country. Around 70% the exports from Gdańsk were of grain.

Grain was also the largest export commodity of the Polish–Lithuanian Commonwealth. The volume of traded grain can be considered a good and well-measured proxy for the economic growth of the Commonwealth.

The owner of a usually signed a with the merchants of Gdańsk, who controlled 80% of this inland trade, to ship the grain to Gdańsk. Many rivers in the Commonwealth were used for shipping, including the Vistula, which had a relatively well-developed infrastructure, with and . Most river shipping travelled north, with southward transport being less profitable, and barges and rafts often being sold off in Gdańsk for lumber.

In order to arrest recurrent flooding on the lower Vistula, the Prussian government in 1889–95 constructed an artificial channel about east of Gdańsk (German name: Danzig)—known as the (German: Weichseldurchstich; Polish: Przekop Wisły)—that acted as a huge sluice, diverting much of the Vistula flow directly into the . As a result, the historic Vistula channel through Gdańsk lost much of its flow and was known thereafter as the Dead Vistula (German: Tote Weichsel; Polish: Martwa Wisła). German states acquired complete control of the region in 1795–1812 (see: Partitions of Poland), as well as during the World Wars, in 1914–1918 and 1939–1945.

From 1867 to 1917, after the collapse of the (1863–1865), the Russian tsarist administration called the the ."The name of the kingdom was changed to Privislinsky Krai, which was reduced to a tsarist province; it lost all autonomy and separate administrative institutions".

(2025). 9781576078006, ABC-CLIO. .

Almost 75% of the territory of interbellum Poland was drained northward into the Baltic Sea by the Vistula (total area of of the Vistula within boundaries of the Second Polish Republic was , the (), the () and the ().

In 1920 the decisive of the Polish–Soviet War Battle of Warsaw (sometimes referred to as the Miracle at the Vistula), was fought as forces commanded by Mikhail Tukhachevsky approached the Polish capital of Warsaw and nearby by the river's mouth.

File:Tyniec Abbey.jpg|The 11th century Benedictine Abbey in overlooks Vistula. File:Czersk 25.jpg|Vistula River near the Duke of Masovia Castle in Czersk File:Hogenberg View of Warsaw.jpg|Vistula River in Warsaw near the end of the 16th century. The right side shows the Sigismund Augustus bridge built 1568–1573 by Erazm Cziotko (c.  long). File:Torun Merian 1641.jpg|Vistula river ( Vistvla fluvivs) in Toruń in 1641 File:Aleksander Gierymski, Święto Trąbek I.jpg|Jewish () at the banks of the Vistula, Aleksander Gierymski, 1884 File:Kierbedź Bridge (1900).jpg|Kierbedź Bridge over the Vistula in Warsaw (c. 1900). This framework was constructed by Stanisław Kierbedź in 1850–1864. It was destroyed by the Germans in 1944. File:Wisla Poland 1939 Henryk Poddebski.jpg|Vistula River in spa town Wisła (1939) just before the World War II


World War II
The Polish September campaign included battles over control of the mouth of the Vistula, and of the city of Gdańsk, close to the river delta. During the Invasion of Poland (1939), after the initial battles in , the remains of the Polish Army of Pomerania withdrew to the southern bank of the Vistula.
(1978). 9780739104842, Lexington Books. .
After defending Toruń for several days, the army withdrew further south under pressure of the overall strained strategic situation, and took part in the main battle of Bzura.

The complex of concentration camps was at the confluence of the Vistula and the Soła rivers.the US Holocaust Memorial Museum, Holocaust Encyclopedia, Auschwitz Environs, Summer 1944, online map Ashes of murdered Auschwitz victims were dumped into the river. Auschwitz-Birkenau: History & Overview Jewish Virtual Library

During World War II prisoners of war from the Nazi camp were assigned to cut ice blocks from the River Vistula. The ice would then be transported by truck to the local beer houses.

The 1944 was planned with the expectation that the Soviet forces, who had arrived in the course of their offensive and were waiting on the other side of the Vistula River in full force, would help in the battle for Warsaw. However, the Soviets let down the Poles, stopping their advance at the Vistula and branding the insurgents as criminals in radio broadcasts."The Uprising remained the ultimate symbol of Communist betrayal and bad faith for Poles." "The Warsaw Rising was termed a 'criminal organization

In early 1945, in the Vistula–Oder Offensive, the crossed the Vistula and drove the German back past the river in Germany.

After the war in late 1946, the former Austrian member Amon Göth was sentenced to death and hanged on 13 September at the Montelupich Prison in Kraków, not far from the site of the Płaszów camp, the camp of which he was commandant throughout . His remains were cremated and the ashes thrown in the Vistula River.

(2025). 9780813333755, Westview Press.


See also


External links

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