The ocean is salty primarily due to the presence of dissolved salts and minerals. These salts come from various sources, including weathering and erosion of rocks on land, volcanic activity, and hydrothermal vents on the ocean floor.
Rainfall and rivers carry small amounts of dissolved salts from the land into the ocean. Over millions of years, this continuous process has resulted in the accumulation of salts in the ocean. Additionally, underwater volcanic eruptions release minerals and gases, including salts, into the ocean water.
The most abundant salt in seawater is sodium chloride, which is commonly known as table salt. Other salts present in smaller quantities include magnesium, calcium, and potassium salts. These salts remain dissolved in the ocean water, making it salty.
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