Ever since NASA’s two Voyager spacecraft snapped the first photos of icy cracks crisscrossing Jupiter’s moon Europa in 1979, astronomers have speculated that tectonic forces could be at work. But the first solid evidence didn’t arrive until September, when a team of planetary geologists announced it might have solved the mystery by treating the moon’s crust like a jigsaw puzzle.
Using data from the ’90s-era Galileo probe, the team — led by Simon Kattenhorn, a structural geologist and planetary scientist at the University of Idaho — digitally deconstructed one region of the moon’s surface into icy pieces, then tried to fit them back together.
Astronomers digitally deconstructed a region of Europa and reassembled the “puzzle pieces” of the icy surface by lining up the cracks. They theorized that a 7,700-square-mile missing piece was forced below the surface by subduction. (Credit: Simon Kattenhor and Louise Prockter/NASA/JPL-Caltech)
Simon Kattenhor and Louise Prockter/NASA/JPL-Caltech
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