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  2. Ocean floor

    Thermohaline circulation is the process by which deep ocean currents are formed. It is driven by differences in water density, which are caused by variations in temperature and salinity. Cold, salty water is denser than warm, less salty water, so it sinks to the bottom of the ocean and flows along the ocean floor.
    www.americanoceans.org/facts/ocean-currents/
    www.americanoceans.org/facts/ocean-currents/
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