Liman (landform)

Source: Wikipedia, the free encyclopedia.
Landsat
satellite photo of limans along the Black Sea coast
Dnieper River and Southern Bug
river estuaries
river estuary

A liman (

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

Anadyrskiy Liman and Amur Liman in Siberia
.

Etymology

English borrows the word from

natural harbour
is frequently synonymous.

Locations

Europe

See also

  • Natural harbour
  • Ria

References

  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