The Danube ( ; see also other names) is the second-longest river in Europe, after the Volga in Russia. It flows through Central and Southeastern Europe, from the Black Forest south into the Black Sea. A large and historically important river, it was once a frontier of the Roman Empire. In the 21st century, it connects ten European countries, running through their territories or marking a border. Originating in Germany, the Danube flows southeast for , passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine. Among the many cities on the river are four national capitals: Vienna, Bratislava, Budapest, and Belgrade. Its drainage basin amounts to and extends into nine more countries.
The Danube's longest headstream, the Breg, rises in Furtwangen im Schwarzwald, while the river carries its name from its source confluence in the palace park in Donaueschingen onwards. Since ancient times, the Danube has been a traditional trade route in Europe. Today, of its total length are navigable. The Danube is linked to the North Sea via the Rhine–Main–Danube Canal, connecting the Danube at Kelheim with the Main at Bamberg. The river is also an important source of hydropower and drinking water.
The Danube river basin is home to such fish species as Northern pike, zander, huchen, Wels catfish, burbot and tench. It is also home to numerous diverse carp and sturgeon, as well as salmon and trout. A few species of euryhaline fish, such as European European seabass, mullet, and European eel, inhabit the Danube Delta and the lower portion of the river.
The river was known to the ancient Greece as the Istros (Ἴστρος) from a root possibly also encountered in the ancient name of the Dniester (Danaster in Latin, Tiras in Greek) and akin to Iranic languages turos 'swift' and Sanskrit iṣiras (इषिरस्) 'swift', from the PIE , 'to flow'.
In the Middle Ages, the Greek Tiras was borrowed into Italian as Tyrlo and into Turkic languages as Tyrla; the latter was further borrowed into Romanian as a regionalism (Turlă).
The Thraco-Phrygian name was Matoas, "the bringer of luck".
The Middle Mongolian name for the Danube was transliterated as Tho-na in 1829 by Jean-Pierre Abel-Rémusat.
The modern languages spoken in the Danube basin all use names derived from the Latin name Danubius]]:
Latin | , Dānuvius | N/A | |
German language | 1 Germany 2 Austria | ||
Bavarian | Doana | N/A | |
Silesian | Dōnaj | N/A | |
Upper Sorbian | Dunaj | N/A | |
Czech language | N/A | ||
Slovak language | 3 Slovakia | ||
Polish language | N/A | ||
Hungarian | 4 Hungary | ||
Slovene language | N/A | ||
Serbo–Croatian | / Дунав | 5 Croatia 6 Serbia | |
Macedonian | N/A | ||
Romanian | , definite form Dunărea | , definite form | 7 Romania 9 Moldova |
Bulgarian | (Dúnav) | 8 Bulgaria | |
Ukrainian | (Dunáy) | 10 Ukraine | |
Greek language | (Doúnavis) | N/A | |
French language | N/A | ||
Italian language | N/A | ||
Portuguese | N/A | ||
Spanish language | N/A | ||
Russian language | (Dunáy) | N/A | |
Turkish language | N/A | ||
Romansh language | Danubi | N/A | |
Albanian | Danub, definite form: Danubi | N/A |
In Latin, the Danube was variously known as Danubius, Danuvius, Ister or Hister. The Latin name is masculine, as are all its Slavic languages names, except Slovene language (the name of the Rhine is also masculine in Latin, most of the Slavic languages, as well as in German). The German Donau (Early Modern German Donaw, Tonaw,Tonaw in Donaw e.g. in Spelling Donau from the 17th century. Middle High German Tuonowe) is feminine, as it has been re-interpreted as containing the suffix -ouwe "wetland".
Romanian differs from other surrounding languages in designating the river with a feminine term, Dunărea (). This form was not inherited from Latin, although Romanian is a Romance language. To explain the loss of the Latin name, scholars who suppose that Romanian developed near the large river propose that the Romanian name descends from a hypothetical Thracian *Donaris. The Proto-Indo-European root of this presumed name is related to the Iranic word "don-"/"dan-", while the supposed suffix -aris is encountered in the ancient name of the Ialomița River, Naparis, and in the unidentified Miliare river mentioned by Jordanes in his Getica. Gábor Vékony says that this hypothesis is not plausible, because the Greeks borrowed the Istros form from the native Thracians. He proposes that the Romanian name is a loanword from a Turkic language (Cuman language or Pecheneg).
Germany | 7.0% | Donau | Donaueschingen – source | |
2 | Austria | 10.0% | Donau | Vienna – capital |
3 | Slovakia | 5.9% | Dunaj | Bratislava – capital |
4 | Hungary | 11.6% | Duna | Budapest – capital |
5 | Croatia | 4.4% | Dunav | |
6 | Serbia | 10.2% | Dunav | Belgrade – capital |
7 | Romania | 29.0% | Dunărea | Danube Delta – Black Sea |
8 | Bulgaria | 5.9% | Dunav | |
9 | Moldova | 1.6% | Dunărea | |
10 | Ukraine | 3.8% | Дунай | Danube Delta – Black Sea |
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Multiannual average, minimum and maximum discharge (water period from 1876 to 2010)
Izmail | 1,889 | 6,489 | 14,673 | |||
Reni, Isaccea | 1,805 | 6,564 | 14,820 | |||
Zimnicea, Svishtov | 1,411 | 6,018 | 14,510 | |||
Orșova | 1,672 | 5,572 | 13,324 | |||
Veliko Gradište | 1,461 | 5,550 | 14,152 | |||
Pančevo | 1,454 | 5,310 | 13,080 | |||
Bogojevo | 959 | 2,889 | 8,153 | |||
Bezdan, Batina | 749 | 2,353 | 7,043 | |||
Mohács | 667 | 2,336 | 7,227 | |||
Nagymaros, Szob | 628 | 2,333 | 7,057 | |||
Bratislava | 633 | 2,059 | 7,324 | |||
Vienna | 506 | 1,917 | 6,062 | |||
Krems an der Donau | 596 | 1,845 | 5,986 | |||
Linz | 468 | 1,451 | 4,783 | |||
Hofkirchen | 211 | 638 | 1,943 | |||
Regensburg | 128 | 444 | 1,330 | |||
Ingolstadt | 83 | 312 | 965 | |||
Ulm | 6 | 38 | 153 |
Simulated water and suspended sediment results from climate-driven decadal study (with STD through specific decade):
P – Simulated average precipitation in the Danube basin; T – Simulated average temperature in the Danube basin; Q – Simulated average discharge in the river Danube at delta; S – Simulated Stream load in the river Danube at Danube Delta;
Common Era]]) !rowspan=2 | Scenario !colspan=2 | P !colspan=2 | T !colspan=2 | Q !colspan=2 | S | |||||
!mm
!in
!°C
!°F
!m3/s
!cu ft/s
!metric tons (millions) !short tons (millions) | ||||||||||
'''LIA''' | ||||||||||
1530–1540 | Cool/dry | |||||||||
1650–1660 | Cool/wet | |||||||||
1709–1719 | Warm/wet | |||||||||
1770–1780 | Warm/dry | |||||||||
Modern era]]''' | ||||||||||
1940–1950 | Cool/dry | |||||||||
1960–1970 | Cool/wet | |||||||||
1975–1985 | Warm/wet | |||||||||
1990–2000 | Warm/dry |
!Year !m3/s !cu ft/s!Year !m3/s !cu ft/s!Year !m3/s !cu ft/s!Year !m3/s !cu ft/s!Year !m3/s !cu ft/s!Year !m3/s !cu ft/s | |||||||||||||||||
Reconstructed | |||||||||||||||||
1742 | 1751 | 1761 | 1771 | 1781 | 1791 | ||||||||||||
1743 | 1752 | 1762 | 1772 | 1782 | 1792 | ||||||||||||
1744 | 1753 | 1763 | 1773 | 1783 | 1793 | ||||||||||||
1745 | 1754 | 1764 | 1774 | 1784 | 1794 | ||||||||||||
1746 | 1755 | 1765 | 1775 | 1785 | 1795 | ||||||||||||
1747 | 1756 | 1766 | 1776 | 1786 | 1796 | ||||||||||||
1748 | 1757 | 1767 | 1777 | 1787 | 1797 | ||||||||||||
1749 | 1758 | 1768 | 1778 | 1788 | 1798 | ||||||||||||
1750 | 1759 | 1769 | 1779 | 1789 | 1799 | ||||||||||||
1760 | 1770 | 1780 | 1790 | 1800 | |||||||||||||
1801 | 1811 | 1821 | 1831 | 1841 | 1851 | ||||||||||||
1802 | 1812 | 1822 | 1832 | 1842 | 1852 | ||||||||||||
1803 | 1813 | 1823 | 1833 | 1843 | 1853 | ||||||||||||
1804 | 1814 | 1824 | 1834 | 1844 | 1854 | ||||||||||||
1805 | 1815 | 1825 | 1835 | 1845 | 1855 | ||||||||||||
1806 | 1816 | 1826 | 1836 | 1846 | 1856 | ||||||||||||
1807 | 1817 | 1827 | 1837 | 1847 | 1857 | ||||||||||||
1808 | 1818 | 1828 | 1838 | 1848 | 1858 | ||||||||||||
1809 | 1819 | 1829 | 1839 | 1849 | 1859 | ||||||||||||
1810 | 1820 | 1830 | 1840 | 1850 | 1860 | ||||||||||||
1861 | 1871 | 1881 | 1891 | 1901 | 1911 | ||||||||||||
1862 | 1872 | 1882 | 1892 | 1902 | 1912 | ||||||||||||
1863 | 1873 | 1883 | 1893 | 1903 | 1913 | ||||||||||||
1864 | 1874 | 1884 | 1894 | 1904 | 1914 | ||||||||||||
1865 | 1875 | 1885 | 1895 | 1905 | 1915 | ||||||||||||
1866 | 1876 | 1886 | 1896 | 1906 | 1916 | ||||||||||||
1867 | 1877 | 1887 | 1897 | 1907 | 1917 | ||||||||||||
1868 | 1878 | 1888 | 1898 | 1908 | 1918 | ||||||||||||
1869 | 1879 | 1889 | 1899 | 1909 | 1919 | ||||||||||||
1870 | 1880 | 1890 | 1900 | 1910 | 1920 | ||||||||||||
Observed | |||||||||||||||||
1921 | 1931 | 1941 | 1951 | 1961 | 1971 | ||||||||||||
1922 | 1932 | 1942 | 1952 | 1962 | 1972 | ||||||||||||
1923 | 1933 | 1943 | 1953 | 1963 | 1973 | ||||||||||||
1924 | 1934 | 1944 | 1954 | 1964 | 1974 | ||||||||||||
1925 | 1935 | 1945 | 1955 | 1965 | 1975 | ||||||||||||
1926 | 1936 | 1946 | 1956 | 1966 | 1976 | ||||||||||||
1927 | 1937 | 1947 | 1957 | 1967 | 1977 | ||||||||||||
1928 | 1938 | 1948 | 1958 | 1968 | 1978 | ||||||||||||
1929 | 1939 | 1949 | 1959 | 1969 | 1979 | ||||||||||||
1930 | 1940 | 1950 | 1960 | 1970 | 1980 | ||||||||||||
1981 | 1991 | 2001 | 2011 | 2021 | |||||||||||||
1982 | 1992 | 2002 | 2012 | 2022 | |||||||||||||
1983 | 1993 | 2003 | 2013 | 2023 | |||||||||||||
1984 | 1994 | 2004 | 2014 | 2024 | |||||||||||||
1985 | 1995 | 2005 | 2015 | 2025 | |||||||||||||
1986 | 1996 | 2006 | 2016 | 2026 | |||||||||||||
1987 | 1997 | 2007 | 2017 | 2027 | |||||||||||||
1988 | 1998 | 2008 | 2018 | 2028 | |||||||||||||
1989 | 1999 | 2009 | 2019 | 2029 | |||||||||||||
1990 | 2000 | 2010 | 2020 | 2030 | |||||||||||||
Multiannual average discharge 1742 to 2022: ~ |
| 18. Tisza (entering near Titel) 19. Sava (entering at Belgrade) 20. Timiș (entering at Pančevo) 21. Great Morava (entering near Smederevo) 22. Mlava (entering near Kostolac) 23. Karaš (entering near Banatska Palanka) 24. Jiu (entering at Bechet) 25. Iskar (entering near Gigen) 26. Olt (entering at Turnu Măgurele) 27. Osam (entering near Nikopol, Bulgaria) 28. Yantra (entering near Svishtov) 29. Argeș (entering at Oltenița) 30. Ialomița 31. Siret (entering near Galați) 32. Prut (entering near Galați) |
Since the completion of the German Rhine–Main–Danube Canal in 1992, the river has been part of a trans-European waterway from Rotterdam on the North Sea to Sulina on the Black Sea, a distance of . In 1994 the Danube was declared one of ten Pan-European transport corridors, routes in Central and Eastern Europe that required major investment over the following ten to fifteen years. The amount of goods transported on the Danube increased to about 100 million tons in 1987. In 1999, transport on the river was made difficult by the NATO bombing of three bridges in Serbia during the Kosovo War. Clearance of the resulting debris was completed in 2002, and a temporary pontoon bridge that hampered navigation was removed in 2005.
At the Iron Gate, the Danube flows through a Canyon that forms part of the boundary between Serbia and Romania; it contains the Iron Gate I Hydroelectric Power Station dam, followed at about downstream (outside the gorge) by the Iron Gate II Hydroelectric Power Station. On 13 April 2006, a record peak discharge at Iron Gate Dam reached .
There are three artificial waterways built on the Danube: the Danube-Tisa-Danube Canal (DTD) in the Banat and Bačka regions (Vojvodina, northern province of Serbia); the Danube-Black Sea Canal, between Cernavodă and Constanța (Romania) finished in 1984, shortens the distance to the Black Sea by ; the Rhine–Main–Danube Canal is about , finished in 1992, linking the North Sea to the Black Sea. A Danube-Aegean canal has been proposed.
River cruise on the Danube is a popular sightseeing activity, especially between Passau, Germany, to Budapest, Hungary.
On the other hand, media reports say the crews on transport ships often steal and sell their own cargo and then blame the plundering on "pirates", and the alleged attacks are not piracy but small-time contraband theft along the river.
The Danube Delta is also the best-preserved river delta in Europe, a UNESCO World Heritage Site (since 1991) and a Ramsar Site. Its lakes and marshes support 45 freshwater fish species. Its wetlands support vast flocks of migratory birds of over 300 species, including the endangered pygmy cormorant ( Phalacrocorax pygmaeus). These are threatened by rival canalization and drainage schemes such as the Bystroye Canal.
The commission dates to the Paris Conferences of 1856 and 1921, which established for the first time an international regime to safeguard free navigation on the Danube. Today the Commission include riparian and non-riparian states.
Before the last ice age in the Pleistocene, the Rhine started at the southwestern tip of the Black Forest, while the waters from the Alps that today feed the Rhine were carried east by the so-called Urdonau (original Danube). Parts of this ancient river's bed, which was much larger than today's Danube, can still be seen in (now waterless) canyons in today's landscape of the Swabian Alb. The erosion of the Upper Rhine valley led to stream capture; waters from the Alps changed their direction and began feeding the Rhine. Today's upper Danube is thus an underfit stream. Since the Swabian Alb is largely shaped of porous limestone, and since the Rhine's level is much lower than the Danube's, today subsurface rivers carry much water from the Danube to the Rhine. On many days in the summer, when the Danube carries little water, it completely sinks into these underground channels at two locations in the Swabian Alb, which are referred to as the Donauversickerung (Danube Sinkhole). Most of this water resurfaces only south at the Aachtopf, Germany's wellspring with the highest flow, an average of , north of Lake Constance—thus feeding the Rhine. The European Water Divide applies only for those waters that pass beyond this point, which only occurs during the days of the year when the Danube carries enough water to survive the sinkholes in the Donauversickerung.
Since such large volumes of underground water erode much of the surrounding limestone, it is predicted that the Danube upper course will one day disappear entirely in favor of the Rhine, an event called Stream capture.
The hydrological parameters of Danube are regularly monitored in Croatia at Batina, Dalj, Vukovar and Ilok.
Darius the Great, king of Persia, crossed the river in the late 6th century BCE to invade European Scythia and to subdue the Scythians.
Alexander the Great defeated the Triballian king Syrmus and the northern barbarian Thracian and Illyrian tribes by advancing from Macedonia as far as the Danube in 336 BCE.
Under the Romans, the Danube formed the border of the Empire with the tribes to the north almost from its source to its mouth. At the same time, it was a route for the transport of troops and the supply of settlements downstream. From 37 CE to the reign of the Emperor Valentinian I (364–375) the Danubian Limes was the northeastern border of the Empire, with occasional interruptions such as the fall of the Danubian Limes in 259. The crossing of the Danube into Roman Dacia was achieved by the Imperium Romanum, first in two battles in 102 and then in 106 after the construction of a bridge in 101 near the garrison town of Drobeta at the Iron Gate. This victory over Dacia under Decebalus enabled the Province of Dacia to be created, but in 271 it was abandoned by emperor Aurelian.
Avar Khaganate used the river as their southeastern border in the 6th century.
At the end of the Okeanos Potamos, is the holy island of Alba (Leuke, Pytho Nisi, Isle of Snakes), sacred to the Pelasgian (and later, Greek) Apollo, greeting the sun rising in the east. Hecateus Abderitas refers to Apollo's island from the region of the Hyperboreans, in the Okeanos. It was on Leuke, in one version of his legend, that the hero Achilles was buried (to this day, one of the mouths of the Danube is called Chilia). Old Romanian folk songs recount a white monastery on a white island with nine priests. Dacia Preistorica , Nicolae Densusianu (1913).
The most important wars of the Ottoman Empire along the Danube include the Battle of Nicopolis (1396), the Siege of Belgrade (1456), the Battle of Mohács (1526), the first Turkish Siege of Vienna (1529), the Siege of Esztergom (1543), the Long War (1591–1606), the Battle of Vienna (1683), the Great Turkish War (1683–1699), the Crimean War (1853–1856) and the Russo-Turkish War (1877–1878).
In the 19th century the beaver was hunted to extinction along the Danube in Bavaria. The Beluga sturgeon population also collapsed, Danube sturgeons had been commercially exploited for meat and caviar since the 5th century BC. River regulation schemes commenced in the 19th century and continued into the 20th century. The Danube river has a total of 18 major dams, including Melk and Freudenau in Vienna.
In Austria and Hungary, most water is drawn from ground and spring sources, and only in rare cases is water from the Danube used. Most states also find it too difficult to clean the water because of extensive pollution; only parts of Romania where the water is cleaner still obtain drinking water from the Danube on a regular basis.
Today, as "Corridor VII" of the European Union, the Danube is an important transport route. Since the opening of the Rhine–Main–Danube Canal, the river connects the Port of Rotterdam and the industrial centers of Western Europe with the Black Sea and, also, through the Danube – Black Sea Canal, with the Port of Constanța.
The waterway is designed for large-scale inland vessels () but it can carry much larger vessels on most of its course. The Danube has been partly canalized in Germany (5 locks) and Austria (10 locks). Proposals to build a number of new locks to improve navigation have not progressed, due in part to environmental concerns.
Downstream from the Freudenau locks in Vienna, canalization of the Danube was limited to the Gabčíkovo dam and locks near Bratislava and the two double Iron Gates locks in the border stretch of the Danube between Serbia and Romania. These locks have larger dimensions. Downstream of the Iron Gate, the river is free flowing all the way to the Black Sea, a distance of more than .
The Danube connects with the Rhine–Main–Danube Canal at Kelheim, with the Donaukanal in Vienna, and with the Danube–Black Sea Canal at Cernavodă.
Apart from a couple of secondary navigable branches, the only major navigable rivers linked to the Danube are the Drava, Sava and Tisza. In Serbia, a canal network also connects to the river; the network, known as the Danube–Tisa–Danube Canals, links sections downstream.
In the Austrian and German sections of the Danube, a type of flat-bottomed boat called a Zille was developed for use along the river. Zillen are still used today for fishing, ferrying, and other transport of goods and people in this area.
The sturgeon stocks associated with the Danube river basin have, over the centuries, formed the basis of a large and significant commercial fishery, renowned throughout the world. The construction of the dams, besides overfishing and river pollution, has a significant role in sturgeon population decline because it creates a barrier for fish migratory species that usually spawn in the upper parts of the river. The spawning areas of migratory fishes species has been dramatically reduced by the construction of hydropower and navigation systems at Iron Gates I (1974) and Iron Gates II (1984). The initial design of these dams has not included any fish passage facility. The possibility of building a human-made fish pass enabling migration for fish species including the sturgeon, is currently under review by projects such as We Pass.
The Upper Danube ecoregion alone has about 60 fish species and the Lower Danube–Dniester ecoregion has about twice as many.Hales, J. (2013). Upper Danube. Freshwater Ecoregions of the World. Retrieved 25 February 2013. Among these are an exceptionally high diversity of sturgeon, a total of six species (beluga, Russian sturgeon, bastard sturgeon, sterlet, starry sturgeon and European sea sturgeon), but these are all threatened and have largely–or entirely in the case of the European sea sturgeon–disappeared from the river. The huchen, one of the largest species of salmon, is Endemism to the Danube basin, but has been introduced elsewhere by humans.
Also, leisure and travel cruises on the river are of significance. Besides the often frequented route between Vienna and Budapest, some ships even go from Passau in Germany to the Danube Delta and back. During the peak season, more than 70 cruise liners are in use on the river, while the traffic-free upper parts can only be discovered with canoes or boats.
The Danube region is not only culturally and historically of importance, but also important for the regional tourism industry due to its fascinating landmarks and sights. With its well established infrastructure regarding cycling, hiking, and travel possibilities, the region along the Danube attracts every year an international clientele. In Austria alone, there are more than 14 million overnight stays and about 6.5 million arrivals per year.
The Danube Banks in Budapest are a part of Unesco World Heritage sites, they can be viewed from a number of sightseeing cruises offered in the city.
The Danube Bend is also a popular tourist destination.
The Danube Bike Trail starts at the origin of the Danube and ends where the river flows into the Black Sea. It is divided into four sections:
In medieval Regensburg, with its maintained old town, stone bridge and cathedral, the Route of Emperors and Kings begins. It continues to Engelhartszell, with the only Engelszell Abbey in Austria. Further highlight-stops along the Danube, include the "Schlögener Schlinge", the city of Linz, which was European Capital of Culture in 2009 with its contemporary art richness, the Melk Abbey, the university city of Krems and the cosmopolitan city of Vienna. Before the Route of Emperors and Kings ends, you pass Bratislava and Budapest, the latter of which was seen as the twin town of Vienna during the times of the Austria-Hungary.
Since Ancient Rome, famous emperors and their retinue traveled on and along the Danube and used the river for travel and transportation. While traveling on the mainland was quite exhausting, most people preferred to travel by ship on the Danube. So the Route of Emperors and Kings was the setting for many important historical events, which characterize the Danube up until today.
The route got its name from the Holy Roman Emperor Frederick I of Barbarossa and the Crusades as well as from Richard I of England who had been jailed in the Dürnstein Castle, which is situated above the Danube. The most imperial journeys throughout time were those of the Habsburg family. Once crowned in Frankfurt, the emperors ruled from Vienna and also held in Regensburg the Perpetual Diet of Regensburg. Many famous castles, palaces, residences, and state-run convents were built by the Habsburger along the river. Nowadays they still remind us of the bold architecture of the "Donaubarock".
Today, people can not only travel by boat on the Danube but also by train, by bike on the Danube Bike Trail or walk on the "Donausteig" and visit the UNESCO World Heritage cities of Regensburg, Wachau and Vienna.
Tourism
Danube Bike Trail
Sultans Trail
Donausteig
The Route of Emperors and Kings
Important national parks
In folklore and literature
The Danube in popular culture
See also
Further reading
Notes
Sources
External links
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