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Ocean Salinity: A Dynamic Equilibrium of Mineral Inputs and Outputs
The salinity of the ocean results from a continuous process where rivers carry dissolved minerals from land to the ocean, and hydrothermal vents and underwater volcanoes add more, maintaining a dynamic equilibrium over millions of years, resulting in an average of 3.5% salinity, although geographic ...
Ocean Salinity: A Dynamic Equilibrium of Mineral Inputs and Outputs
The salinity of the ocean results from a continuous process where rivers carry dissolved minerals from land to the ocean, and hydrothermal vents and underwater volcanoes add more, maintaining a dynamic equilibrium over millions of years, resulting in an average of 3.5% salinity, although geographic ...
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