
Seawater typically has a salinity between 3.1% and 3.8% but rain, glacier melt, upwelling, and evaporation can vary the salt content throughout the world. The Red Sea is the most salty open body of water but Lakes can be salty. Evaporation is greater than freshwater influx in the Great Salt Lake in Utah.
A closed cycle stops the oceans from getting too salty. Rivers bring salt into the oceans by dissolving minerals. Underwater volcanoes and deep sea hydrothermal vents spout out Sodium Chloride NaCL.

But salt is absorbed by many marine organisms and it is leached out of the water into the seafloor. Together these processes regulate salinity.
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