Vistula#cite ref-chodakiewicz 43-0

The name Vistula first appears in the written record of Pomponius Mela (3.33) in AD{{nbsp}}40. Pliny in AD{{nbsp}}77 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 *weys-: 'to ooze, flow slowly' (cf. Sanskrit {{lang|sa|अवेषन्}} {{Transliteration|sa|avēṣan}} "they flowed", Old Norse {{lang|non|veisa}} "slime"), and similar elements appear in many European river-names (e.g. Svislach (Berezina), Svislach (Neman), Weser, Viešinta).D.Q. Adams, Encyclopedia of Indo-European Culture (London: Fitzroy–Dearborn, 1997), 207.

In writing about the river and its peoples, Ptolemy uses Greek spelling: Ouistoula. Other ancient sources{{which|date=February 2024}} spell the name Istula. Ammianus Marcellinus referred to the Bisula (Book{{nbsp}}22) in the 380s. In the sixth century Jordanes (Getica{{nbsp}}5 & 17) used Viscla.

The Anglo-Saxon poem Widsith refers to the Wistla.{{cite web | author = William Napier | url = http://findarticles.com/p/articles/mi_qn4159/is_20051120/ai_n15851679/ | title = Building a Library: The Fall of Rome | work = findarticles.com | publisher = Independent Newspapers UK Limited | date =20 November 2005 | access-date = 1 April 2009}} {{Dead link|date= October 2010|bot= H3llBot}} The 12th-century Polish chronicler Wincenty Kadłubek Latinised the river's name as Vandalus, a form presumably influenced by Lithuanian {{lang|lt|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" ({{lang|la|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 ({{lang|pl|Biała Wisełka}}).{{citation needed|date=June 2023}}

In the course of history the river has borne similar names in different languages: {{langx|de|Weichsel|links=no}}; {{Langx|nds|Wießel}}; {{langx|nl|Wijsel}} {{IPA|nl|ˈʋɛisəl|}}; {{langx|yi|ווייסל|Veysl}} {{IPA|yi|ˈvajsl̩|}}; and {{langx|ru|Висла|Visla}}.

Vistula rises in the southern Silesian Voivodeship close to the tripoint involving the Czech Republic and Slovakia from two sources: Czarna ("Black") Wisełka at altitude {{convert|1107|m|ft|abbr=on}} and Biała ("White") Wisełka at altitude {{convert|1080|m|ft|abbr=on}}.Żaneta Kosińska: [http://www.home.umk.pl/~geopolar/stacja/wisla.htm Rzeka Wisła]. Both are on the western slope of Barania Góra in the Silesian Beskids in Poland.{{cite book |title=Nazewnictwo geograficzne Polski. T.1: Hydronimy. 2cz. w 2 vol.|date=2006 |publisher=Główny Urząd Geodezji i Kartografii |isbn=978-83-239-9607-1}}

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

The Vistula river basin covers {{convert|194424|km2|0|abbr=off}} (in Poland {{convert|168700|km2|0|abbr=off}}); its average altitude is {{convert|270|m|0|abbr=off}} above sea level. In addition, the majority of its river basin (55%) is 100 to 200 m above sea level; over {{frac|3|4}} of the river basin ranges from {{convert|100|to|300|m|0|abbr=off}} in altitude. The highest point of the river basin is at {{convert|2655|m|0|abbr=off}} (Gerlach Peak in the Tatra mountains). 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 Pleistocene epoch, which ended around 10,000 BC, is called the Vistulian glaciation or Weichselian glaciation in regard to north-central Europe.{{cite journal | title=Record of the Vistula ice lobe advances in the Late Weichselian glacial sequence in north-central Poland | last1=Wysota | first1=W. | last2=Molewski | first2=P.| last3=Sokołowski, R.J. | journal=Quaternary International | year=2009 | doi=10.1016/j.quaint.2008.12.015 | first3=Robert J. | volume=207 | issue=1–2 | pages=26–41 | title-link=Weichselian | bibcode=2009QuInt.207...26W }}

{{multiple image

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| image1 = Rzeka Wisła 0004.jpg

| caption1 = Vistula River in the vicinity of Płock, Poland

| image2 = Bdg Wisla most 4 02-2014.jpg

| caption2 = Vistula River near Bydgoszcz, Poland

| image3 = Krakau Wawel Wisla.jpg

| caption3 = Medieval Wawel Castle in Kraków seen from the Vistula river

| image4 = Old Town in Warsaw view from Vistula 2019b.jpg

| caption4 = Vistula River and the Warsaw Old Town

| image5 = Calle Dlugie Pobrzeze, Gdansk, Polonia, 2013-05-20, DD 04.jpg

| caption5 = Vistula River and Gdańsk

| image6 = Polska KazimierzDolny 016.jpg

| caption6 = Renaissance town of Kazimierz Dolny overlooking serene Vistula

| image7 = Grudziądz_Granaries_2009.JPG

| caption7 = Granaries in Grudziądz seen from the left riverside of the Vistula river, 13th–17th century

| image8 = The Vistula River in Toruń.jpg

| caption8 = Vistula River seen from The Piłsudski Bridge in Toruń, facing upstream

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The river forms a wide delta called Żuławy Wiślane, or the "Vistula Fens" in English. The delta currently starts around Biała Góra near Sztum, about {{convert|50|km|0|abbr=on}} from the mouth, where the river Nogat splits off. The Nogat also starts separately as a river named (on this map ) Alte Nogat (Old Nogat) south of Kwidzyn, but further north it picks up water from a crosslink with the Vistula, and becomes a distributary of the Vistula, flowing away northeast into the Vistula Lagoon (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 Leniwka.

Various causes (rain, snow melt, ice jams) 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 [https://www.tandfonline.com/doi/pdf/10.1623/hysj.51.5.799 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 Drausen See.

As with some aggrading 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 longshore drift 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 Mennonite Germans, and economic development followed.
• 1553: By a plan made by Danzig and Elbing, 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 Marienburg 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 Westerplatte. 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{{cite journal|title=History of floods on the River Vistula|first1=JERZY|last1=CYBERSKI|first2=MAREK|last2=GRZEŚ|first3=MAŁGORZATA|last3=GUTRY-KORYCKA|first4=ELŻBIETA|last4=NACHLIK|first5=ZBIGNIEW W.|last5=KUNDZEWICZ|date=1 October 2006|journal=Hydrological Sciences Journal|volume=51|issue=5|pages=799–817|doi=10.1623/hysj.51.5.799|bibcode=2006HydSJ..51..799C |s2cid=214652302|doi-access=free}} formed a shortcut from the Danzig Vistula to the sea (shown as Durchbruch v. J 1840 (Breakthrough of year 1840), on this map{{Cite web |url=http://schwertfamily.net/maps/map_west_und_ostpreussen_1899.jpg |title=map dated 1899 of parts of Poland |access-date=15 July 2018 |archive-date=26 January 2021 |archive-url=https://web.archive.org/web/20210126122724/https://schwertfamily.net/maps/map_west_und_ostpreussen_1899.jpg |url-status=dead }}), 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 {{convert|12|km|1|abbr=off}} 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; [https://www.google.com/maps/dir///@54.2989392,18.9207939,11111m/data=!3m1!1e3?hl=en 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.

List of right and left tributaries with a nearby city, from source to mouth:

File:Vistula River Flooding, Southeastern Poland.JPG

According to flood studies carried out by Zbigniew Pruszak, who is the co-author of the scientific paper Implications of SLR{{cite journal |author1=Zbigniew Pruszaka |author2=Elżbieta Zawadzka |title = Potential Implications of Sea-Level Rise for Poland |journal=Journal of Coastal Research |volume=242 |pages =410–422|doi=10.2112/07A-0014.1 |year=2008 |s2cid=130427456 }} and further studies carried out by scientists attending Poland's Final International ASTRA Conference,{{cite web |url = http://www.astra-project.org/03_071210_espoo_astraconference_final.html |title = Final International ASTRA conference in Espoo, Finland, 10–11 December 2007 |publisher = www.astra-project.org |access-date = 23 October 2009 |archive-date = 17 November 2021 |archive-url = https://web.archive.org/web/20211117175245/https://www.astra-project.org/03_071210_espoo_astraconference_final.html |url-status = dead }} and predictions stated by climate scientists at the climate change pre-summit in Copenhagen,{{cite news |author =Matt McGrath |url = http://news.bbc.co.uk/2/hi/science/nature/7940532.stm |title = Climate scenarios 'being realised' |publisher =BBC News |date =12 March 2009|access-date = 23 October 2009}} it is highly likely most of the Vistula Delta region (which is below sea level{{cite web |url = http://www.iopan.gda.pl/oceanologia/473prusz.pdf |title = Hydrology and morphology of two river mouth regions (temperate Vistula Delta and subtropical Red River Delta) |publisher = www.iopan.gda.pl |access-date = 23 October 2009}}) will be flooded due to the sea level rise caused by climate change by 2100.

The history of the River Vistula and its valley spans over 2 million years. The river is connected to the geological period called the Quaternary, 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, [http://www.pgi.gov.pl/index.php?option=com_content&task=view&id=595&Itemid=597 "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 Carpathians 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 North Sea 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, [http://www.filmpolski.pl/fp/index.php/4218301 Narodziny rzeki]

Wodospad Wiselka Biala.jpg|Biała Wisełka

Wisla 010.jpg|Vistula in southern Poland with the Silesian Beskids

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

Vistula is navigable from the Baltic Sea to Bydgoszcz (where the Bydgoszcz Canal joins the river). It can accommodate modest river vessels of CEMT 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 Narew–Bug–Mukhovets–Pripyat–Dnieper 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 Bug River, linking the Baltic Sea to the Black Sea.{{cite news |url=https://www.theguardian.com/environment/2020/dec/23/chernobyl-fears-resurface-over-contract-to-dredge-river-in-exclusion-zone-aoe |title=Chernobyl fears resurface as river dredging begins in exclusion zone |last=Weston |first=Phoebe |newspaper=The Guardian |date=23 December 2020 |access-date=27 December 2020}}{{cite journal |url=https://jamestown.org/program/the-e40-waterway-the-polish-dimension/ |title=The E40 Waterway: The Polish Dimension |author=Alexandra St John Murphy |journal=Eurasia Daily Monitor |publisher=The Jamestown Foundation |date=4 May 2020 |volume=17 |issue=61 |access-date=27 December 2020}}

File:Wisla-kolo-Torunia.jpg]]

Large parts of the Vistula Basin were occupied by the Iron Age Lusatian and Przeworsk cultures in the first millennium BC. Genetic analysis indicates that there has been an unbroken genetic continuity{{clarify|date=May 2014}} of the inhabitants over the last 3,500 years.{{cite web |author =Jędrzej Giertych |url = http://www.chipublib.org/search/details/cn/927545 |title = Tysiąc lat historii narodu polskiego |publisher = www.chipublib.org |access-date = 3 April 2009|language=pl}} The Vistula Basin along with the lands of the Rhine, Danube, Elbe, and Oder came to be called Magna Germania by Roman authors of the first century AD. This does not imply that the inhabitants were "Germanic peoples" in the modern sense of the term; Tacitus, when describing the Venethi, Peucini and Fenni, wrote that he was not sure if he should call them Germans, since they had settlements and they fought on foot, or rather Sarmatians since they have some similar customs to them.{{Cite web|url=http://info.uah.edu/student_life/organizations/SAL/texts/latin/classical/tacitus/germania1.html|archive-url=https://web.archive.org/web/20071112190346/http://info.uah.edu/student_life/organizations/SAL/texts/latin/classical/tacitus/germania1.html|archive-date=12 November 2007|title=De Origine et Situ Germanorum Liber by Tacitus Latin Text|date=12 November 2007}} Ptolemy, in the second century AD, would describe the Vistula as the border between Germania and Sarmatia.

File:Piotrowski Śmierć Wandy.jpg, 1859]]

Vistula River used to be connected to the Dnieper River, and thence to the Black Sea via the Augustów Canal, a technological marvel with numerous sluices contributing to its aesthetic appeal. It was the first waterway in Central Europe to provide a direct link between the two major rivers, the Vistula and the Neman. It provided a link with the Black Sea to the south through the Oginski Canal, Dnieper River, Berezina Canal, and Dvina River. The Baltic Sea– Vistula– Dnieper– Black Sea route with its rivers was one of the most ancient trade routes, the Amber Road, on which amber and other items were traded from Northern Europe to Greece, Asia, Egypt, and elsewhere.{{cite web|url=https://whc.unesco.org/en/tentativelists/2101/|title=The Augustów Canal (Kanal Augustowski) - UNESCO World Heritage Centre|first=UNESCO World Heritage|last=Centre|website=whc.unesco.org|access-date=13 August 2018}}{{cite web|url=http://www.suwalszczyzna.pl/eng_ver/eng06.htm|title=Suwalszczyzna - Suwalki Region|website=www.suwalszczyzna.pl|access-date=13 August 2018|archive-date=7 July 2014|archive-url=https://web.archive.org/web/20140707095317/http://www.suwalszczyzna.pl/eng_ver/eng06.htm|url-status=dead}}

File:Wislica grodzisko 20070825 1456.jpg stronghold in Wiślica once stood here.]]

The Vistula estuary was settled by Slavs in the seventh and eighth century.{{cite book | author = Jan M. Piskorski | title = Pommern im Wandel der Zeit | year = 1999 | publisher = Zamek Książąt Pomorskich | isbn = 978-83-906184-8-7 |language=de}} 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 Veleti moved westward from the Vistula delta.

A number of West Slavic Polish tribes 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 Vistulans (Wiślanie) in southern Poland. Kraków and Wiślica were their main centres.

Many Polish legends are connected with the Vistula river and the beginnings of Polish statehood. One of the most enduring is that about Princess Wanda co nie chciała Niemca (who rejected the German).{{cite web |author=Paul Havers |url=http://www.kresy.co.uk/wanda.html |title=The Legend of Wanda |publisher = www.kresy.co.uk |archive-url = https://web.archive.org/web/20120205055922/http://www.kresy.co.uk/wanda.html |archive-date=2012-02-05 |access-date = 31 March 2009}} According to the most popular variant, popularized by the 15th-century historian Jan Długosz,{{cite web |author = Leszek Paweł Słupecki |url = http://sms.zrc-sazu.si/pdf/02/SMS_02_Slupecki.pdf |title = The Krakus' and Wanda's Burial Mounds of Cracow |publisher = sms.zrc-sazu.si |access-date = 31 March 2009}} p.84 Wanda, daughter of King Krak, 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.{{cite web |url = http://www.brooklynmuseum.org/eascfa/dinner_party/heritage_floor/wanda.php |title = Wanda |publisher = www.brooklynmuseum.org |access-date = 31 March 2009}} Wanda however committed suicide, drowning in the Vistula River, to ensure he would not invade her country again.

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. Salt, timber, grain, and building stone were among goods shipped via that route between the 10th and 13th centuries.{{cite encyclopedia |author1=Władysław Parczewski |author2=Jerzy Pruchnicki |url = http://www.britannica.com/EBchecked/topic/630787/Vistula-River |title = Vistula River |encyclopedia = Encyclopædia Britannica |access-date = 3 April 2009}}

In the 14th century the lower Vistula was controlled by the Teutonic Knights 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.{{cite web |url = http://www.en.gdansk.gda.pl/about,2,12.html |title = History of the City Gdańsk |publisher = www.en.gdansk.gda.pl |access-date = 3 April 2009 |archive-date = 17 October 2012 |archive-url = https://web.archive.org/web/20121017123409/http://www.en.gdansk.gda.pl/about,2,12.html |url-status = dead }} Since then the event is known as the Gdańsk slaughter. The Order had inherited Gniew from Sambor II, thus gaining a foothold on the left bank of the Vistula.{{cite book |author1=Rosamond McKitterick |author2=Timothy Reuter |author3=David Abulafia |author4=C. T. Allmand | title = The New Cambridge Medieval History: c. 1198–c. 1300| year = 1995 |volume=5 | publisher = Cambridge University Press | isbn = 978-0-521-36289-4 | url = https://books.google.com/books?id=bclfdU_2lesC&q=The+New+Cambridge+Medieval+History:+C.+1198-C.+1300 }} Many granaries and storehouses, built in the 14th century, line the banks of the Vistula.{{cite web|author = Krzysztof Mikulski|url = http://www.mowiawieki.pl/artykul.html?id_artykul=1634|title = Dzieje dawnego Torunia|publisher = www.mowiawieki.pl|access-date = 3 April 2009|language = pl|archive-url = https://web.archive.org/web/20110718121304/http://www.mowiawieki.pl/artykul.html?id_artykul=1634|archive-date = 18 July 2011|df = dmy-all}} 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.{{cite book |author1=Oskar Halecki |author2=Antony Polonsky | title = A history of Poland | year = 1978 | publisher = Routledge | isbn = 978-0-7100-8647-1 |language=de}} 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.{{cite book | author = Krzysztof Olszewski | title = The Rise and Decline of the Polish-Lithuanian Commonwealth due to Grain Trade| year = 2007 }} 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.{{cite encyclopedia |url = http://www.britannica.com/EBchecked/topic/227552/Gdansk |title = Gdańsk (Poland) |encyclopedia = Encyclopædia Britannica |access-date = 3 April 2009}} Other towns were negatively affected by Gdańsk's near-monopoly in foreign trade. During the reign of Stephen Báthory Poland ruled two main Baltic Sea ports: Gdańsk{{cite encyclopedia |url = http://www.britannica.com/EBchecked/topic/565459/Stephen-Bathory |title = Stephen Bathory (king of Poland) |encyclopedia = Encyclopædia Britannica |access-date = 3 April 2009}} controlling the Vistula river trade and Riga controlling the Western Dvina 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 folwark usually signed a contract 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 river ports and granaries. 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 {{convert|12|km|0|abbr=off}} east of Gdańsk (German name: Danzig)—known as the Vistula Cut (German: Weichseldurchstich; Polish: Przekop Wisły)—that acted as a huge sluice, diverting much of the Vistula flow directly into the Baltic. 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 January Uprising (1863–1865), the Russian tsarist administration called the Kingdom of Poland the Vistula Land."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". {{cite book | author = Richard C. Frucht | title = Eastern Europe: An Introduction to the People, Lands, and Culture | year = 2008 | publisher = ABC-CLIO | isbn = 978-1-57607-800-6 | url = https://books.google.com/books?id=lVBB1a0rC70C&q=Eastern+Europe:+An+Introduction+to+the+People,+Lands,+and+Culture |page=19}}

Almost 75% of the territory of interbellum Poland was drained northward into the Baltic Sea by the Vistula (total area of drainage basin of the Vistula within boundaries of the Second Polish Republic was {{cvt|180,300|km2}}, the Niemen ({{cvt|51600|km2|disp=sqbr}}), the Oder ({{cvt|46700|km2|disp=sqbr}}) and the Daugava ({{cvt|10400|km2|disp=sqbr}}).

In 1920 the decisive battle of the Polish–Soviet War Battle of Warsaw (sometimes referred to as the Miracle at the Vistula), was fought as Red Army forces commanded by Mikhail Tukhachevsky approached the Polish capital of Warsaw and nearby Modlin Fortress by the river's mouth.{{citation needed|date=May 2019}}

File:Tyniec Abbey.jpg|The 11th century Benedictine Abbey in Tyniec 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. {{convert|500|m|ft|abbr=on}} long).{{cite web |author = Jerzy S. Majewski |url = http://miasta.gazeta.pl/warszawa/1,97596,2049149.html |title = Most Zygmunta Augusta |publisher = miasta.gazeta.pl |date =29 April 2004 |access-date = 25 October 2009|language=pl}}

File:Torun Merian 1641.jpg|Vistula river (Vistvla fluvivs) in Toruń in 1641

File:Aleksander Gierymski, Święto Trąbek I.jpg|Jewish Feast of Trumpets ({{langx|pl|Święto trąbek}}) 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 bridge was constructed by Stanisław Kierbedź in 1850–1864. It was destroyed by the Germans in 1944.{{cite web|url=http://www.1944.pl/index.php?a=site_text&id=12147&se_id=12196 |title=SEPTEMBER 13, 1944 |publisher=www.1944.pl |access-date=25 October 2009 |archive-url=https://web.archive.org/web/20060523212618/http://www.1944.pl/index.php?a=site_text&id=12147&se_id=12196 |archive-date=23 May 2006 }}

File:Wisla Poland 1939 Henryk Poddebski.jpg|Vistula River in spa town Wisła (1939) just before the 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 Pomerelia, the remains of the Polish Army of Pomerania withdrew to the southern bank of the Vistula.{{cite book | author = Marek Jan Chodakiewicz | title = Between Nazis and Soviets: Occupation Politics in Poland, 1939–1947 | year = 1978 | publisher = Lexington Books | isbn = 978-0-7391-0484-2 | url = https://books.google.com/books?id=TvUErL-MnV8C }} 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 Auschwitz 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, [http://www.ushmm.org/wlc/media_nm.php?lang=en&ModuleId=10005189&MediaId=306 online map] {{Webarchive|url=https://web.archive.org/web/20090506223447/http://www.ushmm.org/wlc/media_nm.php?lang=en&ModuleId=10005189&MediaId=306 |date=6 May 2009 }} Ashes of murdered Auschwitz victims were dumped into the river.[https://www.jewishvirtuallibrary.org/jsource/judaica/ejud_0002_0002_0_01609.html Auschwitz-Birkenau: History & Overview] Jewish Virtual Library

During World War II prisoners of war from the Nazi Stalag XX-B camp were assigned to cut ice blocks from the River Vistula. The ice would then be transported by truck to the local beer houses.{{Citation needed|date=December 2020}}

The 1944 Warsaw Uprising 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.{{cite web |url=http://www.warsawuprising.com/timeline.htm |title=Warsaw Uprising of 1944 |publisher=www.warsawuprising.com |access-date=14 July 2008 |archive-date=3 August 2018 |archive-url=https://web.archive.org/web/20180803215556/http://www.warsawuprising.com/timeline.htm |url-status=dead }} 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." {{cite web |author=John Radzilowski |url=http://ww2db.com/battle_spec.php?battle_id=150|title=Warsaw Uprising |publisher=ww2db.com |access-date=25 March 2010}}"The Warsaw Rising was termed a 'criminal organization{{'"}} {{cite journal | last = Radzilowski| first=John| title = Remembrance and Recovery: The Museum of the Warsaw Rising and the Memory of World War II in Post-communist Poland| year = 2009 | journal = The Public Historian | pages = 143–158 | volume = 31| issue = 4| doi = 10.1525/tph.2009.31.4.143}}

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

After the war in late 1946, the former Austrian SS 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 The Holocaust. His remains were cremated and the ashes thrown in the Vistula River.{{Cite book |last=Crowe |first=David |year=2004 |title=Oskar Schindler: The Untold Account of His Life, Wartime Activities, and the True Story Behind the List |edition=First |publisher=Westview Press |isbn=978-0813333755}}

• Geography of Poland
• Rivers of Poland
• Vistula Lagoon
• Vistula Spit

{{Reflist|colwidth=30em}}

{{Commons category|Vistula}}

• {{Osmrelation-inline|34392}}
• {{GEOnet2|32FA87D047383774E0440003BA962ED3|Vistula}}
• [https://www.tandfonline.com/doi/pdf/10.1623/hysj.51.5.799 "History of Floods on the River Vistula"], Hydrological Sciences Journal

{{Vistula}}

{{Tributaries of the Vistula}}

{{Polish rivers}}

{{Authority control}}

Category:Cieszyn Silesia

Category:Rivers of Kuyavian-Pomeranian Voivodeship

Category:Rivers of Lesser Poland Voivodeship

Category:Rivers of Lublin Voivodeship

Category:Rivers of Masovian Voivodeship

Category:Rivers of Subcarpathian Voivodeship

Category:Rivers of Poland

Category:Rivers of Pomeranian Voivodeship

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Category:Rivers of Świętokrzyskie Voivodeship

Category:Waterways in Poland