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DNIESTER (Tyras and Danaster or Danas...

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Originally appearing in Volume V08, Page 349 of the 1911 Encyclopedia Britannica.
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DNIESTER (See also:Tyras and Danaster or Danastris of classical authors, Nistrul of the Rumanians, and Turla of the See also:Turks)  , a See also:river of See also:south-eastern See also:Europe belonging to the See also:basin of the See also:Black See also:Sea . It rises on the See also:northern slope of the Carpathian mountains in See also:Austrian See also:Galicia, and belongs for the first 350 M. of its course to Austrian, for the remaining 515 M. to See also:Russian, territory . It drains an See also:area of 29,670 sq. m., of which 16,500 sq. m. belong to See also:Russia . It is excessively meandering, and the current in most parts even during See also:low See also:water is decidedly rapid as compared with Russian See also:rivers generally, the mean See also:rate being calculated at I Tm. per See also:hour . The See also:average width of the channel is from 500 to 750 ft., but in some places it attains as much as 1400 ft.; the See also:depth is various and changeable . The See also:principal interruption in the navigable portion of the river, besides a sprinkling of rocks in the See also:bed and the somewhat extensive shallows, is occasioned by a granitic See also:spur from the Carpathians, which gives rise to the Yampol Rapids . For See also:ordinary river See also:craft the passage of these rapids is rendered possible, but not See also:free from danger, by a natural channel on the See also:left See also:side, and by a larger and deeper artificial channel on the right; for steamboats they See also:form an insuperable barrier . The river falls into the sea by several arms, passing through a shallow liman or See also:lagoon, a few See also:miles S.W. of See also:Odessa . There are two periodical floods,—the earlier and larger caused by the breaking up of the See also:ice, and occurring in the latter See also:part of See also:February or in See also:March; and the later due to the melting of the snows in the Carpathians, and taking See also:place about See also:June . The See also:spring See also:flood raises the level of the water 20 ft., and towards the mouth of the river submerges the gardens and vineyards of the adjacent See also:country . In some years the See also:general See also:state of the water is so low that See also:navigation is possible only for three or four See also:weeks, while in other years it is so high that navigation continues without interruption; but in See also:recent years considerable improvements have been effected at See also:government expense . In consequence the See also:traffic has increased, the See also:Dniester tapping regions of See also:great productiveness, especially in cereals and See also:timber, namely, Galicia, See also:Podolia and See also:Bessarabia .

Steamboat traffic was introduced in the See also:

lower reaches in 184o . The See also:fisheries of the lower course and of the See also:estuary are of considerable importance; and these, together with those of the lakes which are formed by the inundations, furnish a valuable addition to the See also:diet of the See also:people in the shape of See also:carp, See also:pike, See also:tench, See also:salmon, See also:sturgeon and eels . Its tributaries are numerous, but not of individual importance, except perhaps the Sereth in Galicia . (P . A . K.; J . T .

End of Article: DNIESTER (Tyras and Danaster or Danastris of classical authors, Nistrul of the Rumanians, and Turla of the Turks)
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