The Brinicle: The Ocean's Finger of Death

192 cases of this type on file · the jury believed 84% of them · 24810 verdicts cast

Drop through a hole cut in the Antarctic sea ice and hang in the cold blue underneath, and you might see something growing downward from the roof of the world: a translucent tube of ice, thickening by the second, reaching for the seabed like a slow finger. Where it lands, it does not stop. A pale frost spreads across the bottom, and the starfish and sea urchins caught in its path stiffen and die in place. Divers who have watched it happen gave it a fittingly grim name. The brinicle. The finger of death.

For all the folklore in its nickname, the brinicle is real physics, filmed and explained. It was captured on camera for the first time by the BBC series Frozen Planet in 2011, when cameramen Hugh Miller and Doug Anderson used time-lapse to record one forming near Little Razorback Island off Antarctica. What they filmed was not a creature and not a curse. It was salt behaving the way salt must.

How the finger forms

Sea ice is not frozen seawater in the simple sense. As the surface freezes, the ice crystals push out the salt, concentrating it into pockets of extremely cold, extremely salty brine trapped within and beneath the ice. This brine is denser than the seawater around it and colder than the normal freezing point, because its high salinity lets it stay liquid below zero. When it finds a channel and begins to sink, it carries its lethal chill with it.

As that plume of supercold brine descends, it freezes the ordinary seawater it touches, sheathing itself in a growing tube of fresh ice. The brine keeps flowing down the inside; the ice keeps building around the outside. The result is a hollow icicle extending from the underside of the sea ice toward the bottom, sometimes reaching it. When the tip meets the seabed, the brine spills outward across the floor, freezing everything slow enough to be caught, the sea stars and urchins that cannot scuttle clear in time.

Folklore made of chemistry

Sailors of an earlier age, had they somehow seen one, would have reached for a sea-demon to explain it, and the diver's phrase "finger of death" keeps a little of that old dread alive. But the brinicle needs no undine or water elemental to account for it, only temperature, salinity and gravity doing arithmetic in the dark. It is a reminder that the ocean can build something that looks designed to kill without any intent behind it at all.

The phenomenon depends on very particular conditions, still water, a stable brine channel, deep cold, which is why brinicles are rare to catch and rarer to film. They form mainly in polar seas, at the underside of sea ice, well out of ordinary human sight, which is part of why the thing feels mythic even though the mechanism is textbook.

There is a small residue the physics does not soften. Watching the footage, the tube seems to hunt, seeking the floor with something like purpose, and the ring of frozen creatures around its base looks staged, a crime scene with no criminal. The explanation is complete and the unease survives it, which is the honest state of a lot of natural marvels.

Below, readers have filed their own encounters and claims about ice, cold water and the strange things the polar seas do, voting each True, Fake or Not sure. Learn the chemistry, keep the shiver, and add your own verdict.

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Questions people ask

What is a brinicle?

A brinicle is a tube of ice that grows downward from the underside of sea ice, formed as cold, dense, salty brine sinks and freezes the seawater around it. Its deadly reputation comes from freezing slow creatures on the seabed when it lands.

Why is a brinicle called the finger of death?

When a brinicle reaches the seafloor, the freezing brine spreads outward and can encase slow-moving animals like starfish and sea urchins in ice. Divers coined the grim nickname after seeing that trail of frozen creatures.

Is a brinicle real or a myth?

It is entirely real, a documented natural phenomenon explained by salinity, temperature and density. It was filmed for the first time by the BBC's Frozen Planet in 2011 near Little Razorback Island in Antarctica.

Where do brinicles form?

They form mainly in polar seas on the underside of sea ice, where extremely cold, concentrated brine can sink in stable conditions. Because they occur underwater and out of sight, they are rarely observed and harder still to film.

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