If you, like me, are in the northern hemisphere, any kind of snow may seem a bit like a mirage right now.
But the strange formations known as penitentes are wacky enough they may make you question what you’re seeing even when you’re expecting snow.
Penitentes are spikes of snow that form typically only in high-altitude areas, like Chile’s Atacama Desert. They can get as tall as 20 feet in the right conditions. Their name comes from their resemblance to a group of monks who wear spiky hats.
And they have been around for a while. In fact, Charles Darwin wrote about them, saying:
“These frozen masses, during the process of thawing, had in some parts been converted into pinnacles or columns, which, as they were high and close together, made it difficult for the cargo mules to pass.”
When they aren’t getting in Darwin’s way, penitentes have been stumping the scientists who have tried to understand how they form. But there’s finally a theory that seems pretty plausible. It replaces a guess that wind shaped the spikes.
It’s easy to think a sheet of freshly fallen snow is flat, but it turns out there are small dips and dimples from the start. These actually concentrate sunlight, heating the snow more quickly. And where penitentes form, it’s actually so dry that heat vaporizes snow directly to steam. The process eventually hollows out spaces between the spikes.
According to the latest version of the theory, the distance between spikes in any given area is pretty standardised because it’s determined by wind speed. The more wind there is, the more water vapour is carried away, letting more snow be vaporized in its place and creating deeper troughs between spikes.
You can watch timelapse footage of penitentes forming and melting here:
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