NASA’s Cassini mission has been studying Saturn and its moons since it arrived at Saturn in 2004, seven years after its launch. Recent data from the probe, published in the March 4th edition of the Journal of Geophysical Research, showed a much greater level of internal heat on the moon Enceladus than expected.
The Cassini spacecraft focused its infrared spectrometer on the south pole of Enceladus, one of the many moons in orbit around Saturn, and registered internal heat-generated power in the region of 15.8 gigawatts. Scientists had only expected output to be in the range of megawatts at the most. Instead what they found was equivalent to the output of about 20 coal-fuel power plants here on earth. Geologically speaking this is over two and a half times the thermal energy of all the hot springs in Yellowstone combined.
“The mechanism capable of producing the much higher observed internal power remains a mystery and challenges the currently proposed models of long-term heat production,” said Carly Howet lead author of the study, and member of the infrared spectrometer science team.
Like many of the moons so far out from Sun, Enceladus has an icy outer layer, but the recent discovery, along with previous evidence of salty sub surface water, increases the chances that a liquid ocean may exist below the ice.