How does the ice finger of death occur the saline solution is a hollow tube that grows down from the ice surrounded by a column of falling saline solution formed under evolving sea ice.


What is the icy finger of death?, Can Brinicle kill you?, How cold is a Brinicle? ,How is a Brinicle formed?
How does the ice finger of death occur 2020


As seawater freezes in the polar oceans, saline salt solutions are expelled from sea ice, resulting in a downward flow of dense, cold and salty water with less freezing point than the surrounding water.

Technically called ice stalactite, or brinicle, this rare underwater phenomenon was first documented in 1974.

It occurs only in the polar regions, during the winter. At that time, the temperature above the sea drops to at least -40 oc, much colder than the ocean water, around -2 oc.




Under these conditions, the freezing of the surface does not form solid ice, as in icebergs, but "porous", with internal channels. A very cold and salty water flows through them, directed downwards due to its density and the heat flow at the bottom of the sea (the “less cold” water goes up and the colder one goes down).




As it passes through the internal channels, the super-frozen water carries more salt, changing the density and getting colder. When it comes out of the “pipe”, the jet of brine cools the ocean water around it, which is less dense, less cold and ends up freezing. That is, the pipe is millimeter long and the stalactite grows.


Structure. Structure. When it was made, the brinicle looked like an ice pipe from the base of the sea ice sheet. The pipe contains incredibly cold and saltwater, which is deposited through salt canals as a result of the growth of sea ice over it a twisting column of ice leads down through the sea floor, scattered with coloured starfish and sea life. The unusual occurrence freezes and destroys all about it as it hits the sea floor, when called the 'cold finger of destruction.' dubbed.

When salt-rich sea ice leaks, it falls into the sea. Often, an icy finger, called a brinicle, can be formed. However, the saumon is so cold that it freezes and forms a falling ice tunnel, said escribano. A brinicle is a surreal, tearless vision — so tearful in reality that it once was described by a british newspaper as "the subsequent hiercle of destruction" and warned of "killing all along its way." and though it can be a little hyperbolitic, brinicles can potentially be dangerous for those aquatic animals roaming about in super cold ponds.

But the delicate ice sheats conceal a lethal gun in the surrounding sea creatures: as seen in the film, the sea-floor can be penetrated by the brinick and, as it rises, it can theoretically capture many living creatures such as sea urchins and starfish from the ground and freeze them.




"small ponds of spring, which we refer to as the black pool of death, were once quite present in or under the brinicles," says thurber. "it may be simple, however often aquatic species have skeletons roaming haphazardly through it."

This situation will produce a natural occurrence, really unusual and stunning - brinicle!! Under sea ice, a brinicle develops as a highly cold, salt water surge through a region of sea water, which is a subsea counterpart to a hollow stalactites or icicles, is introduced.


A brinicle is a surreal, tearless vision — so tearful in reality that it once was described by a british newspaper as "the subsequent hiercle of destruction" and warned of "killing all along its way." and, while this might be a little bit hyperbolic, certain marine creatures wander in super-cold swimming pools may also be deadly.

Fresh water freezes at 32of, but marine water freezes at around 28.4of owing to the salt in it. However, the ice absorbs so little salt as the seawater freezes and only the portion of the ocean freezes. It may be melted to be used as potable water.




Filmed as a product of exceptionally cold brine sink to the ground by hugh miller and doug anderson on the occasion of bbc one's frozen planet sequence. A 'brinic' of ice is formed when the thick salt falls underneath less saline and hot water.


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