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Saltlakes (also called saline lakes) can form where there is no natural outlet or where the water evaporates rapidly, and the drainage surface of the water table has a higher than normal salt content.
The significant input sources are precipitation onto the lake; runoff carried by streams and channels from the lake's catchment area; groundwater channels and aquifers; and artificial sources from outside the catchment area.
A lake may be infilled with deposited sediment, and gradually, the lake becomes a wetland, such as a swamp or marsh.
Zwitterions are salts that contain an dead sea salts anionic center and a cationic center salt peter in the same molecule, examples are the amino acids, salt water many salt metabolites, peptides, and proteins.
Salts can also form if solutions salt water aquarium of different salts are mixed, their ions recombine, and the new salt is insoluble and precipitates (see: Solubility equilibrium).
Salting the earth is the deliberate massive use of salt to render a soil unsuitable for cultivation, and thus disencourage habitation
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