Peresyp
A peresyp, is a Russian hydrological term name for a mouth bar, an element of a deltaic system. A peresyp or mouth bar is a deposit of the sediment transported by the river—i.e., a shoal or sandbar—at the river mouth, typically in mid-channel. This narrow sandbar rises above the water level like a spit and separates a liman from the open water.
Unlike a tombolo, a mouth bar/peresyp seldom forms a contiguous strip and instead usually has one or more channels that connect the lagoon/liman to the sea.
Like a spit, a peresyp is formed by actions of surf zone currents from sand, gravel/pebbles, and crushed shells as a result of longitudinal or transverse transport of sediment. A peresyp may form when two spits on the two sides of a liman grow and meet. These channels can then close and re-open cyclically with changes in current and saturation. And water can seep through or spill over a closed peresyp. The seawater within the enclosed and shallow liman will then evaporate, raising the lagoon's salinity. A number of salt lakes in Crimea were formed this way.
A liman or peresyp is classified as "maritime" if formed by sea currents or "fluvial" if by deltaic action.
A number of locations on the Black Sea coasts of Russia and Ukraine are called peresyp. The of Odesa is built on the wide mouth bar that separates the Khadzhibey and Kuialnyk estuaries from the Black Sea. Other sites include the spit on the Tylihul Estuary in Ukraine.
The Black Sea peresyp ecosystem is unique.
Russian пересыпь is derived from the verb пересыпать, "sprinkle over".