League. In 1455, when the Teutonic Order had become thoroughly corrupt, Dantzic shook off its yoke and submitted to the king of Poland, to whom it was formally ceded, along with the whole of West Prussia, at the Peace of Thorn. Although nominally subject to Poland, and represented in the Polish diets and at the election of Polish kings, it enjoyed the rights of a free city, and governed a considerable territory with more than thirty villages. It suffered severely through various wars of the 17th and 18th centuries, and in 1734, having declared in favour of Stanislas Lesczinski, was besieged and taken by the Russians and Saxons. At the first partition of Poland, in 1772, Dantzic was separated from that king dom ; and in 1793 it came into the possession of Prussia. In 1807, during the war between France and Pussia, it was bombarded and captured by Marshal Lefebvre, who was rewarded with the title of duke of Dantzic ; and at the Peace of Tilsit Napoleon declared it a free town, under the protection of France, Prussia, and Saxony, restoring to it its ancient territory. A French governor, however, remained in it, and by compelling it to submit to the Continental system almost ruined its trade. It was given back to Prussia in 1814.
DANUBE (German, Donau ; Hungarian, Luna ; Latin, Danubius, or Damivius, and in the lower part of its course, Ister), the largest river of Europe next to the Volga, traversing the southern part of Germany, Austria, Hun gary, and the northern part of Turkey, and falling into the Black Sea after a course of about 1750 (or, including its windings, 2000) miles. Its basin, which comprises a territory of nearly 300,000 square miles, is bounded by the Black Forest, some of the minor Alpine ranges, the Bohe mian Forest, and the Carpathian mountains on the north, and by the Alps and the range of the Balkan on the south. The Danube is generally considered to be formed by the union, at Donaueschingen, of the Brigach and the Brege, two mountain streams from the Black Forest ; though a third stream, originating in a spring in the palace garden of Donaueschingen, at a height of about 2850 feet above the sea, is by some held to be the true source. It seems probable, according to the investigations of Professor Knop of Carlsruhe, that at Immardingen the infant river loses a good part of its waters in the fissures of the soil, and thus gives rise to the Aach, which flows south and joins the Khine. After passing N.E. through the kingdom of Wiirtemberg and part of Bavaria to Ratisbon, it turns to the S.E., and maintains that direction till it approaches Lintz in Austria. From this town its course is in the main easterly to Hungary, which it enters a little above Presburg. From Presburg it flows S.E. through the lesser Hungarian plain to its confluence with the Raab, whence it runs E. to Waitzen. At Waitzen it turns S., and flows with a slow current and numerous windings through the greater plain of Hungary for nearly 2/ degrees of latitude. After its junction with the Drave it again takes a general S.E. direc tion to Orsova, where it leaves the Austrian territories by the famous pass of the Iron Gate, with once formidable rapids. From Orsova, its course is generally S. by E. to Kalafat, thence mostly E. by S. to Sistova ; it there takes an E, by N. direction to Rassova, then turns N. to Galatz, and finally eastward to the Black Sea. Among its 400 tributaries, of which upwards of 100 are navigable, the principal are on the right, the Iller, Lech, Iser, Inn, Ens, Raab, Drave, Save, Morava, Timok, Isker, Vid, and Jantra ; and on the left, the Altmiihl, Nab, Regen, March, Waag, Gran, Theiss, Temes, Chyl, Aluta, Jalomnitza, Sereth, and Pruth. The Danube communicates with the Rhine by means of the Ludwigs-Canal, which unites the Altmiihl with the Main, with the Elbe by means of the Moldau and other canals, and with the Theiss, its own tri butary, by means of the Franzens-Canal. The upper course of the river is regularly frozen over all winter ; and even the lower reaches are usually closed for a considerable period. According to a British consular report in 1873, the river at Galatz during the thirty-seven years from 1837 to 1873 remained open all winter only eight times, namely, in 1839, 1846, 1852, 1853, 1854, 1860, 1867, and 1873; the date of the complete freezing over varied from Dec. 7 to Feb. 14; and the breaking up of the ice occurred as early as Jan. 18, and as late as March 21. This last event always causes great anxiety to the inhabitants ; for, if the thaw begins in the upper part of the stream, the waters rush down with tremendous fury, and frequently do incalculable damage. When such a catastrophe is appre hended, watchmen are stationed on eminences along the banks of the river, to give notice by alarm guns when the ice is broken.
At Ulm the Danube receives the Iller, and thus, at a height of 1400 feet above the sea, becomes navigable for flat-bottomed boats of 100 tons. From Donauworth to Passau it traverses the Bavarian plain, leaving which it intersects a mountainous region till it reaches Vienna. At Passau it is 800 feet above the level of the sea,, and at Vienna 450. From Vienna to the mouth of the Drave it flows through an expanse of plain country, broken only in a few places, as at Presburg, Buda, and Waitzen. At Isakcha the channel is 1700 feet broad and 50 feet deep. At extreme low water the total current is 70,000 cubic feet per second, at ordinary low water 125,000, at ordi nary high water 324,000, and during extraordinary flood 1,000,000, and thus, on a general average from the obser vations of 10 years, 207,000 feet per second. The total amount of alluvium annually carried down by the river is calculated at 67,760,000 cubic feet ; and, according to M. Desjardins, the advance of the coast thus produced during the Christian era is about 9 or 10 miles. About 15 miles below Isakcha the river breaks up into two branches, of which the northern or Kilia branch forms an irregular network of channels on its way to the sea, and, after re uniting into one, gives rise to a secondary delta with nine or ten arms ; while the southern or Tultcha branch sub divides before long into the central or Sulina branch and the southmost or St George s. The delta thus formed com prises an area of about 1000 square miles, almost totally destitute of cultivation, and broken in all directions by swamps and fresh-water lakes. Of the total burden of the river it was calculated in 1857 that the Kilia branch carried down seventeen twenty-sevenths, the Sulina branch two twenty-sevenths, and the St George s eight twenty- sevenths ; but since that date the Tultcha St George s branch has grown shallower, and the volume of the Kilia has increased to about eighteen twenty-sevenths, or two- thirds of the whole discharge.
done to render the Danube more available as a means of communication. In 1816 Austria and Bavaria made ar rangements for the common utilization of the river ; and since then both Governments have been liberal in their outlays for its improvement. In 1830 steam-boats were introduced between Vienna and Pesth, under the en couragement of Count Szechenyi, a steam-boat company having been started in 1828 by two Englishmen, Andrews and Prichard. In 1834 the boats descended as far as Orsova, and in 1835 they began to reach Galatz. About the same time the draining of the Donaumoos, between Neuburg and Ingolstadt, which had been commenced iu 1791, was successfully prosecuted. In 1844 the Ludwigs- Canal was completed at a cost of 400,860,000 dollars ; and in 1845 and 1853 the removal of the rocks which still, in spite of the labours of Joseph II., obstructed the river below Grein was finally achieved. In 1866 an imperial commission was established for the rectification of the river bed in the neighbourhood of Vienna ; and the proposal to construct a new channel, supported by the engineers Abernethy and Sexauer, was ultimately chosen as the most promising scheme. In terms of the Peace of
Paris, March 1856, the river not only was placed under