Cassini Spacecraft Finds Ocean May Exist Beneath Titan's Crust

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March 20, 2008

Dwayne Brown
Headquarters, Washington
202-358-1726 
dwayne.c.brown@xxxxxxxx

DC Agle/Carolina Martinez 
Jet Propulsion Laboratory, Pasadena, Calif.
818-393-9011/354-9382
agle@xxxxxxxxxxxx, carolina.martinez@xxxxxxxxxxxx

RELEASE: 08-085

CASSINI SPACECRAFT FINDS OCEAN MAY EXIST BENEATH TITAN'S CRUST

PASADENA, Calif. - NASA's Cassini spacecraft has discovered evidence 
that points to the existence of an underground ocean of water and 
ammonia on Saturn's moon Titan. The findings made using radar 
measurements of Titan's rotation will appear in the March 21 issue of 
the journal Science. 

"With its organic dunes, lakes, channels and mountains, Titan has one 
of the most varied, active and Earth-like surfaces in the solar 
system," said Ralph Lorenz, lead author of the paper and Cassini 
radar scientist at the Johns Hopkins Applied Physics Laboratory in 
Laurel, Md., "Now we see changes in the way Titan rotates, giving us 
a window into Titan's interior beneath the surface."

Members of the mission's science team used Cassini's Synthetic 
Aperture Radar to collect imaging data during 19 separate passes over 
Titan between October 2005 and May 2007. The radar can see through 
Titan's dense, methane-rich atmospheric haze, detailing 
never-before-seen surface features and establishing their locations 
on the moon's surface. 

Using data from the radar's early observations, the scientists and 
radar engineers established the locations of 50 unique landmarks on 
Titan's surface. They then searched for these same lakes, canyons and 
mountains in the reams of data returned by Cassini in its later 
flybys of Titan. They found prominent surface features had shifted 
from their expected positions by up to 19 miles. A systematic 
displacement of surface features would be difficult to explain unless 
the moon's icy crust was decoupled from its core by an internal 
ocean, making it easier for the crust to move. 

"We believe that about 62 miles beneath the ice and organic-rich 
surface is an internal ocean of liquid water mixed with ammonia," 
said Bryan Stiles of NASA's Jet Propulsion Laboratory (JPL) in, 
Pasadena, Calif. Stiles also is a contributing author to the paper.

The study of Titan is a major goal of the Cassini-Huygens mission 
because it may preserve, in deep-freeze, many of the chemical 
compounds that preceded life on Earth. Titan is the only moon in the 
solar system that possesses a dense atmosphere. The moon's atmosphere 
is 1.5 times denser than Earth's. Titan is the largest of Saturn's 
moons, bigger than the planet Mercury.

"The combination of an organic-rich environment and liquid water is 
very appealing to astrobiologists," Lorenz said. "Further study of 
Titan's rotation will let us understand the watery interior better, 
and because the spin of the crust and the winds in the atmosphere are 
linked, we might see seasonal variation in the spin in the next few 
years." 

Cassini scientists will not have long to wait before another go at 
Titan. On March 25, just prior to its closest approach at an altitude 
of 620 miles, Cassini will employ its Ion and Neutral Mass 
Spectrometer to examine Titan's upper atmosphere. Immediately after 
closest approach, the spacecraft's Visual and Infrared Mapping 
Spectrometer will capture high-resolution images of Titan's southeast 
quadrant. 

The Cassini-Huygens mission is a cooperative project of NASA, the 
European Space Agency and the Italian Space Agency. The mission is 
managed by JPL, a division of the California Institute of Technology 
in Pasadena. The Cassini orbiter also was designed, developed and 
assembled at JPL. 

For information about Cassini visit:

http://www.nasa.gov/cassini/

	
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