A brinicle is an underwater phenomenon that occurs in polar regions, often referred to as an "ice finger of death." It forms when cold, salty water is released from sea ice. As this saline water sinks, it interacts with the surrounding seawater, which is less saline and warmer. The process begins when sea ice forms, concentrating salt in the remaining water. When this denser water is released, it sinks and can create a column of brine that descends into the ocean.
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