Liman (landform)

Landsat satellite photo of limans along the Black Sea coast
Liman forming the Dnieper River and Southern Bug river estuaries
Dniester Liman forming the Dniester river estuary

A liman (Russian: лиман; Romanian: liman) is an enlarged estuary formed as a lagoon at the wide mouth of one or several rivers, where flow is nearly fully or partially constrained by a mouth bar of sediments (peresyp), 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 slowed or turned flow of a sediment-saturated river).[1] The term describes many 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, wide-mouthed, deep examples will be greatly saline from inflow of sea water and evaporation.

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.

  1. ^ (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.
  2. ^ "лимáн" Vasmer's Etymological Dictionary in Russian