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Cassini
Prepares to Fly by Walnut-Shaped Moon
Wednesday, September 5, 2007
Ultraviolet
image of Iapetus on the left and a visible light image of
the moon on the right.
Image
Credit: NASA/JPL/University of Colorado/Space Science
Institute
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Cassini will make its only
close flyby of Saturn's odd, two-toned, walnut-shaped moon
Iapetus on Sept. 10, 2007, at about 1,640 kilometers (1,000
miles) from the surface.
This flyby will be 100 times
closer than Cassini's 2004 encounter, and will be the last time
the spacecraft will aim its instruments at this moon.
"Iapetus
spun fast, froze young, and left behind a body with lasting
curves," said Julie Castillo, Cassini scientist at NASA's
Jet Propulsion Laboratory, Pasadena, Calif.
Iapetus
(pronounced eye-APP-eh-tuss) has a ridge of surprisingly large
mountains -- the so-called "belly-band" -- that lies
directly on top of the equator. The moon also has a distinct
difference in the brightness of its leading and trailing
hemispheres, one as bright as snow and the other dark as tar. The
irregular shape, the mountain ridge and Iapetus’ brightness
contrast are among the key mysteries scientists are trying to
solve.
There are several different ideas on the origin of
the dark material. Is it from inside or outside of Iapetus? Is it
residue from some other moon or moons? Is it due to impacts by
meteoroids or comet debris?
"We are on the search
for the brush that may have painted Iapetus's dark side,"
said Dennis Matson, Cassini project scientist at NASA's Jet
Propulsion Laboratory, Pasadena, Calif.
A
map of the surface of Iapetus.
Image
Credit: NASA/JPL/Space Science Institute
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"This dark stuff
appears in several places in the Saturn system and might be
present not just on Iapetus but many other moons,” said JPL
scientist Amanda Hendrix of Cassini’s ultraviolet imaging
spectrograph team and lead author of a paper in the journal
Icarus that explores the possible sources of the Iapetus dark
material.
There’s a reddish tint to the Iapetus
dark stuff, an important clue in tracing its origin, she said.
Saturn's moon Hyperion, which shows evidence of a violent
disruption in its past, has a reddish tint, too. "It may be
that the event that disrupted Hyperion deposited reddish material
onto Iapetus," she said. "Hyperion may be the artist
that’s painting Iapetus dark."
Yet another
Icarus paper on Iapetus by Dale Cruikshank at NASA's Ames
Research Center, Moffett Field, Calif., and colleagues, reports
that the dark material on Iapetus and Saturn's small moon Phoebe
may be composed of the same complex, prebiotic hydrocarbons that
appear to play a fundamental role in the origin of life. These
chemicals, called polycyclic aromatic hydrocarbons, exist on
objects ranging from backyard barbeques to comets, meteorites and
the stardust that forms planets and flows between stars. They are
important markers in studies of the origin of life in the
universe.
An array of Cassini instruments will home in on
Iapetus during the flyby. The full menu of objectives includes
plans to: characterize the chemical composition of the surface;
look for evidence of a faint atmosphere or erupting gas plumes;
and map the nighttime temperature of the surface. This will be
the first Cassini flyby of an icy moon, other than Titan, that's
close enough and slow enough to perform radar imaging with
Cassini's Synthetic Aperture Radar. A large swath of terrain will
be covered, including the equatorial ridge and regions of craters
and basins. These measurements may provide the height of some of
the features.
"What is really neat is that we are
doing radar of an icy object for which we actually have
pictures," said Steve Ostro, a radar scientist at JPL. Until
now, he said, the radar had been used to reveal the surface of
cloud-covered Titan. Iapetus’ surface is easily visible.
"This will be a lesson on how to interpret radar images on
an icy body. With Titan, because of the cloud cover, we don't
know what we are looking at much of the time, but for Iapetus we
will know very well," he said.
In coming weeks,
scientists will be analyzing data from multiple instruments. Some
results of that analysis will be presented at a planetary science
conference in Orlando, Fla., in mid-October.
The
Cassini-Huygens mission is a cooperative project of NASA, the
European Space Agency and the Italian Space Agency. JPL, a
division of the California Institute of Technology in Pasadena,
manages the Cassini mission for NASA's Science Mission
Directorate, Washington, D.C. JPL designed, developed and
assembled the Cassini orbiter.
Source:
NASA / JPL

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