Saturn's Dynamic Moon Enceladus Shows More Signs of Activity

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Dec. 15, 2008

Steve Cole 
Headquarters, Washington 
202-657-2194 
stephen.e.cole@xxxxxxxx 

Carolina Martinez 
Jet Propulsion Laboratory, Pasadena, Calif. 
818-354-9382 
carolina.martinez@xxxxxxxxxxxx 

RELEASE: 08-325

SATURN'S DYNAMIC MOON ENCELADUS SHOWS MORE SIGNS OF ACTIVITY

SAN FRANCISCO -- The closer scientists look at Saturn's small moon 
Enceladus, the more they find evidence of an active world. The most 
recent flybys of Enceladus made by NASA's Cassini spacecraft have 
provided new signs of ongoing changes on and around the moon. The 
latest high-resolution images of Enceladus show signs that the south 
polar surface changes over time. 

Close views of the southern polar region, where jets of water vapor 
and icy particles spew from vents within the moon's distinctive 
"tiger stripe" fractures, provide surprising evidence of Earth-like 
tectonics. They yield new insight into what may be happening within 
the fractures. The latest data on the plume -- the huge cloud of 
vapor and particles fed by the jets that extend into space -- show it 
varies over time and has a far-reaching effect on Saturn's 
magnetosphere. 

"Of all the geologic provinces in the Saturn system that Cassini has 
explored, none has been more thrilling or carries greater 
implications than the region at the southernmost portion of 
Enceladus," said panel member Carolyn Porco, Cassini imaging team 
leader at the Space Science Institute in Boulder, Colo. 

A panel of Cassini scientists presented these new findings Monday in a 
news briefing at the American Geophysical Union's Fall Meeting in San 
Francisco. 

"Enceladus has Earth-like spreading of the icy crust, but with an 
exotic difference -- the spreading is almost all in one direction, 
like a conveyor belt," said panelist Paul Helfenstein, Cassini 
imaging associate at Cornell University in Ithaca, N.Y. "Asymmetric 
spreading like this is unusual on Earth and not well understood." 

"Enceladus has asymmetric spreading on steroids," Helfenstein added. 
"We are not certain about the geological mechanisms that control the 
spreading, but we see patterns of divergence and mountain-building 
similar to what we see on Earth, which suggests that subsurface heat 
and convection are involved." 

The tiger stripes are analogous to the mid-ocean ridges on Earth's 
seafloor where volcanic material wells up and creates new crust. 
Using Cassini-based digital maps of the moon's south polar region, 
Helfenstein reconstructed a possible history of the tiger stripes by 
working backward in time and progressively snipping away older and 
older sections of the map, each time finding that the remaining 
sections fit together like puzzle pieces. 

Images from recent close flybys also have bolstered an idea the 
Cassini imaging team has that condensation from the jets erupting 
from the surface may create ice plugs that close off old vents and 
force new vents to open. The opening and clogging of vents also 
corresponds with measurements indicating the plume varies from month 
to month and year to year. 

"We see no obvious distinguishing markings on the surface in the 
immediate vicinity of each jet source, which suggests that the vents 
may open and close and thus migrate up and down the fractures over 
time," Porco said. "Over time, the particles that rain down onto the 
surface from the jets may form a continuous blanket of snow along a 
fracture." 

Enceladus' output of ice and vapor dramatically impacts the entire 
Saturnian system by supplying the ring system with fresh material and 
loading ionized gas from water vapor into Saturn's magnetosphere. 

"The ions added to the magnetosphere are spun up from Enceladus' 
orbital speed to the rotational speed of Saturn," said Cassini 
magnetometer science team member Christopher Russell of the 
University of California, Los Angeles. "The more material is added by 
the plume, the harder this is for Saturn to do, and the longer it 
takes to accelerate the new material." 

With water vapor, organic compounds and excess heat emerging from 
Enceladus' south polar terrain, scientists are intrigued by the 
possibility of a liquid-water-rich habitable zone beneath the moon's 
south pole. 

Cassini's flybys on Aug. 11 and Oct. 31 targeted Enceladus' fractured 
southern region. An Oct. 9 flyby took the spacecraft deep into the 
plume of water vapor and ice shooting out of the moon's vents. 
Cassini's next flyby of Enceladus will be in November 2009. The 
Cassini-Huygens mission is a cooperative project of NASA, the 
European Space Agency and the Italian Space Agency. 

For more information about the Cassini-Huygens mission, visit: 



http://www.nasa.gov/cassini 

	
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