Inactive Tutor answered 07/21/26
The ocean’s salt did not come from one single event. It accumulated gradually as water interacted with rocks over geologic time.
Rainwater contains dissolved carbon dioxide and is slightly acidic. As it moves through soils and rocks, it chemically weathers minerals and releases dissolved ions. Rivers then carry ions such as sodium, calcium, magnesium, chloride, and sulfate to the ocean. Volcanic gases, submarine hydrothermal systems, and reactions between seawater and oceanic crust also contribute dissolved material.
Salt becomes concentrated because the water cycle removes mostly pure water by evaporation, while most dissolved ions remain behind. However, the ocean does not simply become saltier forever. Ions are also removed by processes such as mineral precipitation, biological activity, alteration of the seafloor, and burial in sediments. Ocean salinity therefore reflects a long-term balance between sources and sinks.
From a geologic-time perspective, the important issue is not a planet’s age alone but whether it has liquid water, reactive rock, and enough time for water-rock interaction and concentration. An enclosed ocean beneath the ice of Europa could become salty through reactions between water and its rocky interior even without rivers or an atmosphere like Earth’s.