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Pluto's Giant Glacier Might Be Secretly Sweating Liquid Nitrogen

Pluto's icy surface may hide a liquid past! Scientists found evidence of liquid nitrogen flowing across Sputnik Planitia, possibly rising through cracks from deep beneath the ice.

Lina Chen
Lina Chen
·2 min read·41 views

Originally reported by ScienceDaily · Rewritten for clarity and brevity by Brightcast

Why it matters: This discovery expands humanity's understanding of planetary geology and the potential for diverse environments beyond Earth, inspiring future space exploration and scientific inquiry.

Turns out, Pluto isn't just a frozen relic quietly orbiting the sun. New evidence suggests that liquid nitrogen might be seeping onto its surface, bubbling up from deep within its icy crust. This isn't ancient history we're talking about; we're talking right now or, at the very least, very recently.

Imagine a glacier the size of Texas and Oklahoma combined, made almost entirely of frozen nitrogen. That's Sputnik Planitia, the vast, heart-shaped expanse on the dwarf planet. When NASA's New Horizons spacecraft flew past in 2015 and 2016, it spotted strange dark features on this colossal ice sheet. Scientists initially thought, "Huh, that's weird." Now, after a fresh look, they're thinking, "Wait, is that… wet?"

Pluto's Icy Sweat Marks

These peculiar dark patches, particularly at the northern edge of Sputnik Planitia, look suspiciously like what happens on Earth's glaciers when liquid water seeps through cracks or rises from below. But on Pluto, where temperatures hover around -387°F, liquid water is a pipe dream. Liquid nitrogen, however? That's a different story.

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Dr. Alan Stern, the New Horizons mission's principal investigator, noted that Pluto just keeps on surprising everyone. This latest discovery points to a dwarf planet that's far more geologically active than we ever gave it credit for. It's not just a big, cold rock; it's got stuff happening under the surface. Computer models from the SETI Institute paint a compelling picture: nitrogen ice at the bottom of Sputnik Planitia, several kilometers deep, could melt into liquid. This liquid nitrogen could then rise through narrow channels, kind of like a tiny, super-cold geyser. Buoyancy or pressure from below could push it up, letting it reach the surface and spread out, wetting the surrounding frozen nitrogen and creating those dark, tell-tale marks.

This isn't just a cool factoid for Pluto enthusiasts. The surface of Sputnik Planitia is incredibly young, geologically speaking — likely less than a million years old. That means whatever is causing these features is a relatively recent phenomenon. ## Beyond Pluto's Heart

While this particular type of liquid flow hasn't been definitively found elsewhere on Pluto, we've only mapped about half of the dwarf planet in high resolution. So, who knows what other icy secrets are lurking? This mechanism of melting and upward liquid movement could even explain activity on other distant bodies, like Neptune's moon Triton, which famously sports geysers.

Basically, Pluto is still out there, pulling scientific surprises out of its icy sleeves. And it's making us rethink what we thought we knew about how active — and how weird — the outer solar system can get.

Brightcast Impact Score (BIS)

This article celebrates a significant scientific discovery: the first evidence of liquid nitrogen flowing on Pluto, suggesting it's more geologically active than previously thought. The novelty is high as it's a new finding about a distant dwarf planet. While not directly scalable for human benefit, it expands our understanding of planetary science and inspires curiosity.

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Sources: ScienceDaily

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