In 2006, the Cassini spacecraft recorded geyser curtains shooting forth from “tiger stripe” fissures near the south pole of Saturn’s moon Enceladus — sometimes as much as 200 kilograms of water per second. A new study suggests how expanding ice during millennia-long cooling cycles could sometimes crack the moon’s icy shell and let its inner ocean out, providing a possible explanation for the geysers.
Enceladus has a diameter of about 504 kilometers (313 miles) — roughly the length of the United Kingdom at its longest point. The moon is covered in ice 20-30 kilometers (12.4-18.6 miles) thick, and the surface temperature is about -201 Celsius (-330 Fahrenheit), but a decade of data from NASA’s Cassini–Huygens mission supplied evidence for a deep liquid ocean inside the icy shell, escaping into space through continuous “cryo-volcanism”. How such a small, cold world can sustain so much geological activity has been an enduring scientific puzzle.
“It captivated both the scientists’ and the general public’s attention,” said Max Rudolph, an assistant professor in geophysics at the University of California, Davis, and lead author of the new study, published in Geophysical Research Letters.