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Mercury
Autumn 2008 Table of Contents


This close up of Enceladus shows a fracture crossing the
upper part of the image. Image scale is approximately 30
meters (98 feet) per pixel.
Image courtesy of NASA / JPL / Space Science Institute.
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Cassini
Pinpoints Source of Enceladus Jets
NASA
/ JPL / Space Science Institute
In
a feat of interplanetary sharpshooting, NASA’s Cassini spacecraft
has pinpointed precisely where the icy jets erupt from the surface
of Saturn’s geologically active moon Enceladus.
New
carefully targeted pictures reveal exquisite details in the prominent
south polar "tiger stripe" fractures from which the jets
emanate. The images show the fractures are about 300 meters (980
feet) deep, with V-shaped inner walls. The outer flanks of some
of the fractures show extensive deposits of fine material. Finely
fractured terrain littered with blocks of ice tens of meters in
size and larger surround the fractures.
"This
is the mother lode for us," said Carolyn Porco, Cassini imaging
team leader at the Space Science Institute, Boulder, Colorado. "A
place that may ultimately reveal just exactly what kind of environment
— habitable or not — we have within this tortured little
moon."
One
highly anticipated result of this flyby was finding the location
within the fractures from which the jets blast icy particles, water
vapor, and trace organics into space. Scientists are now studying
the nature and intensity of this process on Enceladus, and its effects
on surrounding terrain. This information may answer the question
of whether reservoirs of liquid water exist beneath the surface.
"There
appears to have been extensive fallout of icy particles to the ground,
along some of the fractures, even in areas that lie between two
jet source locations, though any immediate effects of presently
active jets are subtle," said Porco.
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