Icy Volcanoes Likely Shape Saturn's Smooth Moon

Icy Volcanoes Likely Shape Saturn's Smooth Moon
A perspective view over volcanic terrain seen in a new digital elevation model, with ridges in foreground and large impact basin in background. The elevations are exaggerated for effect. Red is high and blue is low. (Image credit: Paul Schenk/LPI, NASA)

Saturn's icy moon Dione may have much in common with its active sibling Enceladus, new research using Cassini spacecraft data has revealed.

Paul Schenk of the Lunar and Planetary Institute and Jeff Moore of NASA's Ames Research Center modelled Dione's surface using digital elevation models (DEMs). Their results indicate volcanism has been a major force in shaping Dione's surface.

"We don't see giant shield volcanoes belching lavas," says Schenk. "Instead we see smooth plains with low crater densities."

These plains are the hallmark of cryovolcanism, which manifests itself as an outpouring of icy liquids from a moon's interior.

The DEMs used by Schenk and Moore reveal Dione's cryovolcanic plains to be higher than the surrounding terrain, suggesting they may have been emplaced in a high viscosity flow similar to terrestrial glaciers sometime within the last 2 billion to 4 billion years.

"As far as the source of the heat, well that's the big question. It is clear that some of the craters (on Dione) have been severely modified by high heat flow, not unlike parts of Enceladus. Perhaps these satellites (Dione and Enceladus) were very hot to begin with and had continued tidal heating to keep them warm," Schenk told SPACE.com.

This tidal heating of these moons interiors would be caused by Saturn's strong gravitational pull as well as help from Dione and Enceladus' orbital resonance; Enceladus completes two orbits of Saturn for every one achieved by Dione.

The same flexing mechanism can be seen if you bend a paper clip back and forth, it heats up. On Enceladus the internal heat results in water-venting geysers at the south pole. Dione is further from Saturn's gravitational grasp and somewhat analogous to the paper clip's cooler end.

"Maybe some residual heat is driving off water from the surface (of Dione) at a slow rate. This seems at least plausible," Schenk said.

Any hopes pinned on obtaining images of geysers on Dione have so far been dashed. Yet like Enceladus, much of Dione's surface is riven with fractures, the evidence of multiple tectonic upheavals. So could Dione possess its own less vicious take on Enceladus' water spewing clefts known as 'tiger-stripes'?

"Dione doesn't have a direct analog to tiger-stripes, although the northern area has been in darkness since 2004. Mapping is still in progress and Dione will definitely be a priority target for at least one close pass during the extended mission," Schenk said.

Contributing writer

David Powell is a space reporter and Space.com contributor from 2006 to 2008, covering a wide range of astronomy and space exploration topics. Powell's Space.com coveage range from the death dive of NASA's Cassini spacecraft into Saturn to space debris and lunar exploration.