You may have seen headlines proclaiming that the great mystery of Antarctica’s “Blood Falls” has finally been solved. That’s a little silly, because the big mystery—the question of why blood-like bright red liquid oozes out of the otherwise white surface of Taylor Glacier—hasn’t been all that mysterious for some time. Two years ago, a study suggested that the water, a salty brine full of interesting microbial life and colored by a high level of iron, seems to come up from an underground waterway that connects visible lakes on the surface.
“It turns out that as beautiful and visceral as Blood Falls is in these valleys, it’s actually just a blip. It’s a little defect in this much more exciting feature,” microbiologist Jill Mikucki told The Washington Post in 2015.
But we digress. Blood Falls? Still awesome. And the latest research on their origins, while not as out-of-the-blue as some headlines might suggest, is still really cool. Essentially, the study turns the speculation of the 2015 paper into a confirmed fact—and includes some findings that could have major implications for our warming planet, too.
In a study published this week in the Journal of Glaciology, researchers (including Mikucki) report new information on the intriguing natural phenomenon’s plumbing: they believe they’ve traced the water’s exact starting point to an reservoir of brine beneath Taylor Glacier.
“We knew that there was a brine outflow creating the falls, and that 2015 paper pretty much verified that the salty water came from beneath the glacier,” lead study author Jessica Badgeley, a graduate student at the University of Washington, told PopSci. Badgeley conducted the research while she was an undergrad at Colorado College, working with the University of Alaska Fairbanks glaciologist Erin Pettit and her team. “The mystery that remained was the link between that source and the outflow. This is an unusual feature, and there are very few things like it. So it wasn’t obvious how you got the brine from below the glacier up to the surface.”
For starters, the glacier wasn’t supposed to have liquid water running through it at all. Salt lowers water’s freezing point, so brine stays sloshy for longer. “But that’s not enough,” Badgeley explained. “There’s another mechanism.”
She and her colleagues found that the brine actually warms itself up as it freezes. Sounds, wacky, sure, but we are talking about the Blood Falls. Here’s how that works: when water undergoes the phase change from liquid to frozen, it gives off heat—that’s just basic chemistry. In the case of the brine flowing through Taylor Glacier, the heat given off by the brine that does freeze is enough to keep the rest of it flowing.
The signature of that heat helped Badgeley and her team track down the water’s path: they sent radio waves into the glacier and measured the amount of time it took for the waves to bounce back, as well as how they changed during their journey. That told them about the glacier’s innards, and their results showed that an area inside was particularly warm and liquidy.
Source/More: Popular Science