Note: Distances are in kilometers, rounded to the nearest kilometer. Waterway distances are shown, not towpath distances. Country capitals are shown in bold.
TheDanube (/ˈdæn.juːb/DAN-yoob; see alsoother names) is thesecond-longest river in Europe, after theVolga in Russia. It flows through Central and Southeastern Europe, from theBlack Forest south into theBlack Sea. A large and historically important river, it was once a frontier of theRoman 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 2,850 km (1,770 mi), passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine. Among the manycities on the river are four national capitals:Vienna,Bratislava,Budapest, andBelgrade. Its drainage basin amounts to 817,000 km2 (315,000 sq mi) and extends into nine more countries.
The Danube's longest headstream, theBreg, rises inFurtwangen im Schwarzwald, while the river carries its name from its source confluence in thepalace park inDonaueschingen onwards. Since ancient times, the Danube has been a traditional trade route in Europe. Today, 2,415 km (1,501 mi) of its total length are navigable. The Danube is linked to theNorth Sea via theRhine–Main–Danube Canal, connecting the Danube atKelheim with theMain atBamberg. The river is also an important source ofhydropower and drinking water.
Today the river carries its name from its source confluence inDonaueschingen, Germany, to its discharge into theBlack Sea via theDanube Delta in Romania and Ukraine.
The river was known to theancient Greeks as theIstros (Ἴστρος)[9] from a root possibly also encountered in the ancient name of theDniester (Danaster in Latin,Tiras in Greek) and akin toIranicturos 'swift' andSanskritiṣiras (इषिरस्) 'swift', from thePIE*isro-,*sreu 'to flow'.[10]
In the Middle Ages, the GreekTiras was borrowed into Italian asTyrlo and into Turkic languages asTyrla; the latter was further borrowed into Romanian as a regionalism (Turlă).[10]
The Thraco-Phrygian name wasMatoas,[11] "the bringer of luck".[12]
Danube is anOld European river name derived from theCeltic 'Danu' or 'Don'[16] (both Celtic gods), which itself derived from theProto-Indo-European*deh₂nu. Other European river names from the same root include the Dunaj, Dzvina/Daugava,Don,Donets,Dnieper,Dniestr,Dysna andTana/Deatnu. InRigvedic Sanskrit,danu (दनु) means "fluid, dewdrop" anddanuja (दनु-ज) means "born fromdanu" or "born from dew-drops". InAvestan, the same word means "river". TheFinnish word for Danube isTonava, which is most likely derived from the name of the river inGerman,Donau. ItsSámi nameDeatnu means "Great River". It is possible thatdānu inScythian as in Avestan was a generic word for "river":Dnieper andDniestr, fromDanapris andDanastius, are presumed to continue Scythian*dānu apara "far river" and*dānu nazdya- "near river", respectively.[17]
In Latin, the Danube was variously known asDanubius,Danuvius,Ister[18] orHister. The Latin name is masculine, as are all itsSlavic names, exceptSlovene (the name of theRhine is also masculine in Latin, most of the Slavic languages, as well as in German). The GermanDonau (Early Modern GermanDonaw,Tonaw,[19]Middle High GermanTuonowe)[20] 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 (IPA:[ˈdunəre̯a]).[10] This form was not inherited from Latin, although Romanian is a Romance language.[14] To explain the loss of the Latin name, scholars who suppose that Romanian developed near the large river propose[14] that the Romanian name descends from a hypotheticalThracian*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 theIalomița River,Naparis, and in the unidentifiedMiliare river mentioned byJordanes in hisGetica.[10] Gábor Vékony says that this hypothesis is not plausible, because the Greeks borrowed theIstros form from the native Thracians.[14] He proposes that the Romanian name is a loanword from a Turkic language (Cuman orPecheneg).[14]
Once a long-standing frontier of theRoman Empire, the river passes through or touches the borders of 10 countries. Itsdrainage basin extends into nine more (ten ifKosovo is included).[21]
In addition to the bordering countries (see above), thedrainage basin includes parts of nine more countries:Bosnia and Herzegovina (4.6% of the basin area), theCzech Republic (2.9%),Slovenia (2.0%),Montenegro (0.9%),Switzerland (0.2%),Italy (<0.15%),Poland (<0.1%),North Macedonia (<0.1%) andAlbania (<0.1%).[21] The total drainage basin is 801,463 km2 (309,447 sq mi) in area,[22][23] and is home to 83 million people.[24] The highest point of the drainage basin is the summit ofPiz Bernina at theItaly–Switzerland border, at 4,049 m (13,284 ft).[25] The Danube River Basin is divided into three main parts, separated by "gates" where the river is forced to cut through mountainous sections:[24]
Simulated water and suspended sediment results from climate-driven decadal study (withSTD through specific decade):[30]
P – Simulated averageprecipitation in the Danube basin;T – Simulated averagetemperature in the Danube basin;Q – Simulated averagedischarge in the Danube River at delta;S – Simulatedsediment load in the Danube River atdelta;
Historical average flow to the present day; Measured and reconstructed average water flows from 1742.The reconstructed and observed streamflow (Q – m3/s) atCeatal Izmail for the 1742 to 2022:[31][32][33][34][28]
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
5,780
204,000
1751
6,760
239,000
1761
6,470
228,000
1771
9,700
340,000
1781
5,830
206,000
1791
5,540
196,000
1743
5,355
189,100
1752
7,090
250,000
1762
6,510
230,000
1772
6,050
214,000
1782
6,470
228,000
1792
6,930
245,000
1744
5,370
190,000
1753
4,980
176,000
1763
5,950
210,000
1773
4,600
160,000
1783
7,930
280,000
1793
7,800
280,000
1745
4,940
174,000
1754
6,330
224,000
1764
6,280
222,000
1774
6,150
217,000
1784
8,400
300,000
1794
5,230
185,000
1746
7,140
252,000
1755
6,840
242,000
1765
6,130
216,000
1775
6,060
214,000
1785
7,610
269,000
1795
6,530
231,000
1747
5,850
207,000
1756
6,370
225,000
1766
8,530
301,000
1776
6,320
223,000
1786
6,570
232,000
1796
6,460
228,000
1748
6,840
242,000
1757
6,830
241,000
1767
6,850
242,000
1777
5,530
195,000
1787
6,980
246,000
1797
6,700
240,000
1749
6,690
236,000
1758
8,410
297,000
1768
8,400
300,000
1778
7,470
264,000
1788
5,860
207,000
1798
6,560
232,000
1750
5,180
183,000
1759
5,520
195,000
1769
5,720
202,000
1779
6,600
230,000
1789
7,190
254,000
1799
9,590
339,000
1760
6,840
242,000
1770
10,700
380,000
1780
6,990
247,000
1790
6,940
245,000
1800
6,150
217,000
5,905 (208,500)
6,597 (233,000)
7,154 (252,600)
6,547 (231,200)
6,978 (246,400)
6,749 (238,300)
1801
7,310
258,000
1811
8,220
290,000
1821
6,390
226,000
1831
6,670
236,000
1841
6,210
219,000
1851
7,350
260,000
1802
6,590
233,000
1812
5,230
185,000
1822
5,700
200,000
1832
4,820
170,000
1842
5,340
189,000
1852
6,550
231,000
1803
6,870
243,000
1813
6,680
236,000
1823
6,520
230,000
1833
5,350
189,000
1843
6,710
237,000
1853
7,800
280,000
1804
6,220
220,000
1814
7,290
257,000
1824
6,420
227,000
1834
6,470
228,000
1844
6,960
246,000
1854
5,060
179,000
1805
7,010
248,000
1815
6,640
234,000
1825
8,040
284,000
1835
7,040
249,000
1845
7,440
263,000
1855
7,020
248,000
1806
6,830
241,000
1816
8,090
286,000
1826
5,800
200,000
1836
9,740
344,000
1846
6,750
238,000
1856
5,390
190,000
1807
7,000
250,000
1817
8,650
305,000
1827
6,650
235,000
1837
6,770
239,000
1847
7,070
250,000
1857
4,880
172,000
1808
5,600
200,000
1818
6,920
244,000
1828
8,140
287,000
1838
10,440
369,000
1848
5,620
198,000
1858
5,580
197,000
1809
7,150
252,000
1819
6,470
228,000
1829
8,280
292,000
1839
9,960
352,000
1849
5,360
189,000
1859
5,630
199,000
1810
8,430
298,000
1820
6,560
232,000
1830
7,790
275,000
1840
5,560
196,000
1850
7,360
260,000
1860
7,220
255,000
6,901 (243,700)
7,075 (249,900)
6,973 (246,200)
7,282 (257,200)
6,482 (228,900)
6,248 (220,600)
1861
5,980
211,000
1871
8,860
313,000
1881
8,320
294,000
1891
5,440
192,000
1901
5,570
197,000
1911
5,120
181,000
1862
5,040
178,000
1872
5,970
211,000
1882
5,130
181,000
1892
5,620
198,000
1902
5,650
200,000
1912
6,940
245,000
1863
3,340
118,000
1873
5,150
182,000
1883
7,590
268,000
1893
5,710
202,000
1903
5,490
194,000
1913
6,410
226,000
1864
6,150
217,000
1874
4,680
165,000
1884
5,250
185,000
1894
4,770
168,000
1904
4,940
174,000
1914
6,560
232,000
1865
5,690
201,000
1875
5,360
189,000
1885
5,430
192,000
1895
6,240
220,000
1905
6,100
220,000
1915
9,540
337,000
1866
3,780
133,000
1876
7,520
266,000
1886
5,660
200,000
1896
6,470
228,000
1906
6,190
219,000
1916
7,550
267,000
1867
6,350
224,000
1877
6,660
235,000
1887
5,340
189,000
1897
7,700
270,000
1907
6,770
239,000
1917
6,410
226,000
1868
5,660
200,000
1878
7,040
249,000
1888
6,800
240,000
1898
4,550
161,000
1908
4,400
160,000
1918
4,300
150,000
1869
5,370
190,000
1879
8,300
290,000
1889
6,530
231,000
1899
4,500
160,000
1909
5,590
197,000
1919
7,410
262,000
1870
7,470
264,000
1880
5,660
200,000
1890
4,650
164,000
1900
6,900
240,000
1910
7,450
263,000
1920
6,720
237,000
5,483 (193,600)
6,520 (230,000)
6,070 (214,000)
5,790 (204,000)
5,815 (205,400)
6,770 (239,000)
Observed
1921
3,906
137,900
1931
6,706
236,800
1941
9,916
350,200
1951
6,368
224,900
1961
5,860
207,000
1971
5,272
186,200
1922
6,530
231,000
1932
6,181
218,300
1942
7,266
256,600
1952
5,850
207,000
1962
6,628
234,100
1972
6,160
218,000
1923
6,430
227,000
1933
6,344
224,000
1943
4,308
152,100
1953
6,117
216,000
1963
6,047
213,500
1973
5,766
203,600
1924
6,700
240,000
1934
5,644
199,300
1944
7,190
254,000
1954
6,168
217,800
1964
5,259
185,700
1974
7,258
256,300
1925
5,255
185,600
1935
5,718
201,900
1945
5,870
207,000
1955
8,834
312,000
1965
8,400
300,000
1975
7,190
254,000
1926
8,144
287,600
1936
6,392
225,700
1946
4,684
165,400
1956
7,100
250,000
1966
7,954
280,900
1976
6,567
231,900
1927
5,990
212,000
1937
8,325
294,000
1947
5,418
191,300
1957
6,254
220,900
1967
7,500
260,000
1977
7,073
249,800
1928
5,005
176,700
1938
6,867
242,500
1948
6,357
224,500
1958
6,340
224,000
1968
5,660
200,000
1978
7,120
251,000
1929
5,330
188,000
1939
6,310
223,000
1949
4,301
151,900
1959
5,375
189,800
1969
7,710
272,000
1979
7,747
273,600
1930
5,197
183,500
1940
9,533
336,700
1950
5,130
181,000
1960
6,514
230,000
1970
9,602
339,100
1980
8,767
309,600
5,888 (207,900)
6,802 (240,200)
6,044 (213,400)
6,492 (229,300)
7,062 (249,400)
6,892 (243,400)
1981
8,172
288,600
1991
6,274
221,600
2001
6,304.3
222,630
2011
5,303
187,300
2021
6,018
212,500
1982
6,700
240,000
1992
5,710.8
201,670
2002
6,837.1
241,450
2012
5,053
178,400
2022
5,753
203,200
1983
5,543
195,700
1993
4,873
172,100
2003
5,021
177,300
2013
7,164
253,000
2023
6,623.8
233,920
1984
6,325
223,400
1994
6,031.8
213,010
2004
6,524
230,400
2014
7,446
263,000
2024
1985
6,449
227,700
1995
6,223.7
219,790
2005
8,711
307,600
2015
6,138
216,800
2025
1986
6,257
221,000
1996
7,035.8
248,470
2006
8,428
297,600
2016
6,465
228,300
2026
1987
6,619
233,700
1997
6,684.2
236,050
2007
5,626
198,700
2017
5,202
183,700
2027
1988
6,383
225,400
1998
6,804.6
240,300
2008
5,909
208,700
2018
6,487.8
229,110
2028
1989
5,448
192,400
1999
7,951.5
280,800
2009
6,492
229,300
2019
5,579
197,000
2029
1990
4,194
148,100
2000
6,580.6
232,390
2010
9,598
339,000
2020
4,893.5
172,810
2030
6,209 (219,300)
6,417 (226,600)
6,945 (245,300)
5,973 (210,900)
6,131.6 (216,540)
Multiannual average discharge 1742 to 2022: ~6,500 m3/s (230,000 cu ft/s)
The land drained by the Danube extends into many other countries. Many Danubian tributaries are important rivers in their own right, navigable by barges and other shallow-draught boats. From its source to its outlet into the Black Sea, its main tributaries are (as they enter):
The Danube flows through many cities, including four national capitals (shown below in bold), more than any other river in the world. Ordered from the source to the mouth they are:
Vienna – capital ofAustria and the most populous city on the Danube, where the Danube floodplain is called theLobau, though theInnere Stadt is situated away from the main flow of the Danube (it is bounded by theDonaukanal – 'Danube canal').
Aerial view ofMargaret Island,Budapest, Hungary. There are 15 bridges over the Danube in Budapest.Great War Island in Belgrade, Serbia. It is located at the confluence of theSava and Danube.TheAda Kaleh island in the Danube was forgotten during the peace talks at theCongress of Berlin in 1878, which allowed it to remain ade jure Turkish territory and the Ottoman SultanAbdul Hamid II's private possession until theTreaty of Lausanne in 1923 (de facto untilRomania unilaterally declared its sovereignty on the island in 1919 and further strengthened it with theTreaty of Trianon in 1920).[35][36] The island was submerged during the construction of theIron Gates hydroelectric plant in 1970.
Upper Section: From spring toDevín Gate, at the border of Austria and Slovakia. Danube remains a characteristic mountain river untilPassau, with average bottom gradient 0.12% (1200 ppm), from Passau to Devín Gate the gradient lessens to 0.06% (600 ppm).
Middle Section: From Devín Gate toIron Gate, at the border of Serbia and Romania. The riverbed widens and the average bottom gradient becomes only 0.006% (60 ppm).
Lower Section: From Iron Gate toSulina, with average gradient as little as 0.003% (30 ppm).
The Danube is navigable by ocean ships from the Black Sea toBrăila in Romania (the maritime river sector), and further on by river ships toKelheim,Bavaria, Germany; smaller craft can navigate further upstream toUlm,Württemberg, Germany. About 60 of its tributaries are also navigable.
Since the completion of the GermanRhine–Main–Danube Canal in 1992, the river has been part of a trans-European waterway fromRotterdam on theNorth Sea toSulina on the Black Sea, a distance of 3,500 km (2,200 mi). In 1994 the Danube was declared one of tenPan-European transport corridors, routes in Central and Eastern Europe that required major investment over the following ten to fifteen years.[citation needed] 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 theNATO bombing of three bridges in Serbia during theKosovo War. Clearance of the resulting debris was completed in 2002, and a temporarypontoon bridge that hampered navigation was removed in 2005.[citation needed]
At theIron Gate, the Danube flows through agorge that forms part of the boundary between Serbia and Romania; it contains theIron Gate I Hydroelectric Power Station dam, followed at about 60 km (37 mi) downstream (outside the gorge) by theIron Gate II Hydroelectric Power Station. On 13 April 2006, a record peak discharge at Iron Gate Dam reached 15,400 m3/s (540,000 cu ft/s).
There are three artificial waterways built on the Danube: theDanube-Tisa-Danube Canal (DTD) in theBanat andBačka regions (Vojvodina, northern province of Serbia); the 64 km (40 mi)Danube-Black Sea Canal, betweenCernavodă andConstanța (Romania) finished in 1984, shortens the distance to the Black Sea by 400 km (250 mi); theRhine–Main–Danube Canal is about 171 km (106 mi), finished in 1992, linking the North Sea to the Black Sea.[37] A Danube-Aegean canal has been proposed.[38]
Cruising on the Danube is a popular sightseeing activity, especially betweenPassau, Germany, toBudapest, Hungary.[39]
In 2010–12, shipping companies, especially from Ukraine, claimed that their vessels suffered from "regularpirate attacks" on the Serbian and the Romanian stretches of the Danube.[40][41][42] However, the transgressions may not be considered acts of piracy, as defined according to theUnited Nations Convention on the Law of the Sea, but rather instances of "river robbery".[43]
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-timecontraband theft along the river.[44]
The Danube Delta (Romanian:Delta Dunăriipronounced[ˈdeltaˈdunərij];Ukrainian:Дельта Дунаю,romanized: Del'ta Dunayu) is the largestriver delta in theEuropean Union. The greater part of the Danube Delta lies in Romania (Tulcea county), while its northern part, on the left bank of the Chilia arm, is situated in Ukraine (Odesa Oblast). The approximate surface is 4,152 km2 (1,603 sq mi), of which 3,446 km2 (1,331 sq mi) are in Romania. If one includes the lagoons ofRazim-Sinoe (1,015 km2 (392 sq mi) of which 865 km2 (334 sq mi) water surface), which are located south of the delta proper, but are related to it geologically and ecologically (their combined territory is part of the World Heritage Site), the total area of the Danube Delta reaches 5,165 km2 (1,994 sq mi).
The Danube Delta is also the best-preserved river delta in Europe, aUNESCO World Heritage Site (since 1991) and aRamsar Site. Its lakes and marshes support 45 freshwater fish species. Its wetlands support vast flocks of migratory birds of over 300 species, including the endangeredpygmy cormorant (Phalacrocorax pygmaeus). These are threatened by rival canalization and drainage schemes such as theBystroye Canal.[45]
The International Commission for the Protection of the Danube River (ICPDR) is an organization that consists of 14 member states (Germany, Austria, the Czech Republic, Slovakia, Slovenia, Hungary, Croatia, Bosnia and Herzegovina, Serbia, Bulgaria, Romania, Moldova, Montenegro, and Ukraine) and theEuropean Union. The commission, established in 1998, deals with the whole Danube river basin, which includes tributaries and groundwater resources. Its goal is to implement the Danube River Protection Convention by promoting and coordinating sustainable and equitable water management, including conservation, improvement, and rational use of waters and the implementation of the EUWater Framework Directive and theDanube Strategy.
The Danube Commission is concerned with the maintenance and improvement of the river's navigation conditions. It was established in 1948 by seven countries bordering the river. Members include representatives from Austria, Bulgaria, Croatia, Germany, Hungary, Moldova, Slovakia, Romania, Russia, Ukraine, and Serbia; it meets regularly twice a year. It also convenes groups of experts to consider items provided for in the commission's working plans.
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.
Although theheadwaters of the Danube are relatively small today, geologically, the Danube is much older than theRhine, with which its catchment area competes in today's southern Germany. This has a few interesting geological complications. Since the Rhine flows north towards the North Sea, acontinental divide beginning atPiz Lunghin divides large parts of southern Germany, which is sometimes referred to as theEuropean Watershed.
Before the lastice age in thePleistocene, 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-calledUrdonau (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 theSwabian Alb. The erosion of theUpper Rhine valley led tostream capture; waters from the Alps changed their direction and began feeding the Rhine. Today's upper Danube is thus anunderfit stream.
Since the Swabian Alb is largely shaped of porouslimestone, 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 Sink). Most of this water resurfaces only 12 km (7.5 mi) south at theAachtopf, Germany's wellspring with the highest flow, an average of 8,500 L/s (300 cu ft/s), north ofLake 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 calledstream capturing.
The hydrological parameters of Danube are regularly monitored in Croatia atBatina,Dalj,Vukovar andIlok.[46]
Combat between Russian and Turkish forces on the Danube in 1854, during theCrimean War (1853–1856)
The Danube basin was the site of some of the earliest human cultures. TheDanubian Neolithic cultures include theLinear Pottery cultures of the mid-Danube basin. Many sites of the sixth-to-third millennium BCEVinča culture (Vinča, Serbia), are sited along the Danube. The third millennium BCEVučedol culture (from the Vučedol site nearVukovar,Croatia) is famous for its ceramics.
Alexander the Great defeated the Triballian kingSyrmus 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 EmperorValentinian I (364–375) theDanubian 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 intoDacia was achieved by theImperium Romanum, first in two battles in 102 and then in 106 after the construction of a bridge in 101 near the garrison town ofDrobeta at the Iron Gate. This victory over Dacia underDecebalus enabled the Province ofDacia to be created, but in 271 it was abandoned by emperorAurelian.
Avars used the river as their southeastern border in the 6th century.
A look upstream from theDonauinsel in Vienna,Austria during an unusually cold winter (February 2006). A frozen Danube usually occurs just once or twice in a lifetime.
Bratislava does not usually suffer major floods, but the Danube sometimes overflows its right bank.
Part of the rivers Danubius or Istros was also known as (together with the Black Sea) theOkeanos in ancient times, being called theOkeanos Potamos (Okeanos River). The lower Danube was also called theKeras Okeanoio (Gulf or Horn of Okeanos) in theArgonautica byApollonius Rhodos (Argon. IV. 282).
At the end of theOkeanos 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.[47]
InAustria andHungary, 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.[51]
Fishing from a Zille on the Danube in Lower Austria, 1982
In the 19th century, the Danube was an important waterway but was, asThe Times of London put it, "annually swept by ice that will lift a large ship out of the water or cut her in two as if she were a carrot."[52]
The waterway is designed for large-scale inland vessels (110 × 11.45 m) 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 theFreudenau locks in Vienna, canalization of the Danube was limited to theGabčíkovo dam and locks near Bratislava and the two doubleIron Gate 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 860 kilometres (530 mi).
The Danube connects with the Rhine–Main–Danube Canal atKelheim, with theDonaukanal in Vienna, and with the Danube–Black Sea Canal atCernavodă.
Apart from a couple of secondary navigable branches, the only major navigable rivers linked to the Danube are theDrava,Sava andTisa. In Serbia, a canal network also connects to the river; the network, known as theDanube–Tisa–Danube Canals, links sections downstream.
In the Austrian and German sections of the Danube, a type of flat-bottomed boat called aZille 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 importance of fishing on the Danube, which was critical in theMiddle Ages, has declined dramatically. Some fishermen are still active at certain points on the river, and theDanube Delta still has an important industry. However, some of the river's resources have been managed in an environmentally unsustainable manner in the past, leading to damage by pollution, alterations to the channel, and major infrastructure development, including large hydropower dams.[53]
Thesturgeon 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.[54] 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).[55] The initial design of these dams has not included any fish passage facility.[56] The possibility of building a human-madefish pass enabling migration for fish species including the sturgeon, is currently under review by projects such as We Pass.[57]
The Upper Danubeecoregion alone has about 60 fish species and the Lower Danube–Dniester ecoregion has about twice as many.[58] Among these are an exceptionally high diversity of sturgeon, a total of six species (beluga,Russian sturgeon,bastard sturgeon,sterlet,starry sturgeon andEuropean sea sturgeon), but these are all threatened and have largely–or entirely in the case of the European sea sturgeon–disappeared from the river.[58] Thehuchen, one of the largest species of salmon, isendemic to the Danube basin, but has beenintroduced elsewhere by humans.[59]
Also, leisure and travel cruises on the river are of significance. Besides the often frequented route between Vienna and Budapest, some ships even go fromPassau in Germany to theDanube 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.[60]
The Danube Banks inBudapest 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 running along theSchlögener SchlingeThe Danube Bike Trail leading through the city ofLinz
TheDanube Bike Trail (also called Danube Cycle Path or theDonauradweg) is a bicycle trail along the river. Especially the parts through Germany and Austria are very popular, which makes it one of the 10 most popular bike trails in Germany.[61]
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:
TheSultans Trail is a hiking trail that runs along the river betweenVienna andSmederevo in Serbia. From there the Sultans Trail leaves the Danube, terminating inIstanbul. Sections along the river are as follows.
Resting area along theDonausteig hiking trail nearBad Kreuzen
In 2010, theDonausteig, a hiking trail from Passau toGrein, was opened. It is 450 km (280 mi) long and it is divided into 23 stages. The route passes through five Bavarian and 40 Austrian communities. A landscape and viewpoints, which are along the river, are the highlights of theDonausteig.[62]
The Route of Emperors and Kings is an international touristic route leading fromRegensburg to Budapest, calling in Passau, Linz and Vienna.[63] The international consortiumARGE Die Donau-Straße der Kaiser und Könige, comprising ten tourism organisations, shipping companies, and cities, strives for the conservation and touristic development of the Danube region.[60]
In medieval Regensburg, with its maintained old town,stone bridge andcathedral, the Route of Emperors and Kings begins. It continues toEngelhartszell, with the onlyTrappist monastery in Austria. Further highlight-stops along the Danube, include the "Schlögener Schlinge", the city of Linz, which wasEuropean Capital of Culture in 2009 with its contemporary art richness, theMelk Abbey, the university city ofKrems 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 theAustro-Hungarian Empire.Sinceancient Roman times, 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 theHoly Roman Emperor Frederick I of Barbarossa and thecrusaders as well as fromRichard I of England who had been jailed in theDürnstein Castle, which is situated above the Danube. The most imperial journeys throughout time were those of theHabsburg family. Once crowned inFrankfurt, the emperors ruled from Vienna and also held in Regensburg thePerpetual 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 theUNESCO World Heritage cities of Regensburg,Wachau and Vienna.[64]
The Danube figures prominently in theBulgarian National Anthem, as a symbolic representation of the country's natural beauty. In Lithuanian folklore songs, the appearance of Danube (Dunojus, Dunojėlis) is more common than the appearance of the longest Lithuanian riverNeman.
The German tradition of landscape painting, the Danube school, was developed in the Danube valley in the 16th century.[citation needed]
One ofClaudio Magris's masterpieces is calledDanube (ISBN1-86046-823-3). The book, published in 1986, is a large cultural-historical essay, in which Magris travels the Danube from the first sources to the delta, tracing the rich European ethnic and cultural heritage, literary and ideological past and present along the way.
Lóczy, Dénes. The Danube: Morphology, Evolution, and Environmental Issues. In Avijit Gupta, ed., Large Rivers: Geomorphology and Management. 2nd Ed. Hoboken, N.J.: Wiley-Blackwell, 2022, pp. 335–367. ISBN 9781119412601
Sommerwerk, Nike, Jurg Bloesch, Christian Baumgartner, Thomas Bittl, Dubravka Cerba, Bela Csanyi, Grigore Davideanu, Martin Dokulil, Georg Frank, Iulia Grecu, Thomas Hein, Vladimir Kovac, Ilulian Nichersu, Tibor Mikuska, Karin Pall, Momir Paunovic, Carmen Postolache, Maja Rakovic, Cristina Sandu, Martin Schneider-Jacoby, Katharina Stefke, Klement Tockner, Ion Toderas, and Laurentia Ungureanu. The Danube River Basin. In Klement Tockner, Christiane Zarfl, and Christopher T. Robinson (eds.), Rivers of Europe, 2nd Ed. Cambridge, MA: Elsevier, 2022, pp. 83–181. ISBN 978-0-08-102612-0
^Dyer, Robert (1974). "Matoas, the Thraco-Phrygian name for the Danube, and the IE root *madų".Glotta.52 (1/2). Vandenhoeck & Ruprecht (GmbH & Co. KG):91–95.JSTOR40266286.
^Šašel Kos, Marjeta (2009). "Reka kot božanstvo — Sava v antiki" [River as a Deity – The Sava in Antiquity]. In Barachini, Jožef (ed.).Ukročena lepotica: Sava in njene zgodbe [The Tamed Beauty: The Sava and Its Stories](PDF) (in Slovenian and English). Sevnica: Javni zavod za kulturo, šport, turizem in mladinske dejavnosti. pp. 42–50.ISBN978-961-92735-0-0. Archived fromthe original(PDF) on 4 March 2016.
^Abel-Rémusat, Jean-Pierre (1829).Nouveaus Mélanges Asiatiques. Vol. 2. Paris: Schubart and Heidelhoff. pp. 96–97.
^Ancient Languages of the Balkans, Part One. Paris: Mouton. 1976. p. 144.
^Tonaw inSebastian Franck (1542).Weltbuch. p. 81.Donaw e.g. inLeonhard Thurneisser zum Thurn (1572).Pison. p. 186. SpellingDonau from the 17th century.
^McCarney-Castle, K.; Voulgaris, G.; Kettner, A.J.; Giosan, L. (2021). "Simulating fluvial fluxes in the Danube watershed: The "Little Ice Age" versus modern day".The Holocene.22:91–105.doi:10.1177/0959683611409778.S2CID129864432.
^"About Us".International Commission for the Protection of the Danube River. Retrieved5 February 2021.
^"Blue River".wwf.panda.org.Archived from the original on 12 April 2021. Retrieved5 February 2021.
^"The Danube". International Association of Water Supply Companies in the Danube River Catchment Area. Archived fromthe original on 19 May 2012. Retrieved28 July 2012.