Answer:
The area where water that is very high in salinity trickles out of the seafloor is called a "brine pool" or "brine seep." Brine pools are localized areas on the seafloor where dense, highly saline water, often saturated with dissolved minerals, accumulates. These pools or seeps can occur in various marine environments, such as deep-sea basins, submarine canyons, or hydrothermal vent fields.
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