Liman (landform)
Liman is defined in Bulgarian, Ukrainian (лиман), Russian (лиман) and Romanian (liman) as an enlarged estuary formed as a lagoon at the widening mouth of one or several rivers, where flow is blocked by a bar of sediments, as in the Dniester Liman or the Razelm liman. A liman can be maritime (the bar being created by the current of a sea) or fluvial (the bar being created by the flow of a bigger river at the confluence).[1] The term is usually used in place of the more universal delta, with its implication of landform, to describe wet estuaries in the Black Sea and the Sea of Azov; a synonymous term guba (губа) is used in Russian sources for estuaries of the Russian shores in the north.[2]
Water in a liman is brackish with a variable salinity: during periods of low fresh-water intake, it may become significantly more saline as a result of evaporation and inflow of sea water.
Such features are found in places with low tidal range, for example along the western and northern coast of the Black Sea, in the Baltic Sea (Vistula Lagoon, the Curonian Lagoon), as well as along the lowest part of the Danube. Examples of limans include Lake Varna in Bulgaria, Lake Razelm in Romania, the Dniester Liman in Ukraine and the Anadyrskiy Liman and Amur Liman in Siberia.
Etymology
English borrows the word from Russian лима́н (Russian pronunciation: [lʲɪˈman]), taken from the Turkish liman spread by Turks when they occupied the western and northern shore of the Black Sea. Liman originated in the Medieval Greek λιμένας (meaning bay or port).
See also
References
- ^ (in Romanian) Mihai Ielenicz (ed., 1999): Dicționar de geografie fizică, Corint publ., Bucharest, 1999 ; Grigore Antipa (1941) : Marea Neagră, Romanian academy press, Bucharest, 1941, pp. 55-64, and Petre Gâștescu, Vasile Sencu (1968) : Împărăția limanelor, Meridiane publ., Bucharest.
- ^ "лимáн" Vasmer's Etymological Dictionary in Russian
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