Rainwater erodes rocks on land, carrying minerals and salts into rivers and eventually into the ocean.
Volcanic eruptions release gases and minerals into the atmosphere, which can then dissolve in rainwater and be carried into the ocean.
These vents release hot, mineral-rich fluids into the ocean, contributing to the salt content.
The Earth's crust contains a significant amount of salt, and over time, this salt is slowly released into the ocean through various geological processes.
Once in the ocean, these salts dissolve in the water, resulting in the characteristic saltiness of seawater. The most abundant salt in seawater is sodium chloride (table salt), but other salts such as magnesium, calcium, and potassium are also present in smaller amounts.
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