For the first time, NASA's Cassini spacecraft revealed surface
details of Saturn's moon Hyperion. During a flyby in September 2005, it saw cup-like
craters filled with hydrocarbons. These substances may indicate a more
widespread presence of basic chemicals necessary for life in our solar system.
Water and carbon dioxide ices were found, as well as dark
material that fits the spectral profile of hydrocarbons.
Cassini's
ultraviolet imaging spectrograph and visual and infrared mapping spectrometer
captured compositional variations in Hyperion's surface. These instruments, which
map mineral and chemical features of the moon, returned data confirming the
presence of frozen water found by earlier ground-based observations, but also
discovered solid carbon dioxide (dry ice) mixed in unexpected ways with the
ordinary ice. Images of the brightest regions of Hyperion's surface show frozen
water that is crystalline in form, like that found on Earth.
In this map, blue shows the maximum exposure of frozen
water, red denotes carbon dioxide ice ("dry ice"), magenta indicates
regions of water plus carbon dioxide, yellow is a mix of carbon dioxide and an
unidentified material.
The July 5 issue of Nature reports details of
Hyperion's surface craters and composition observed during this flyby,
including keys to understanding the moon's origin and evolution over 4.5
billion years. This is the first time scientists were able to map the surface
material on Hyperion.
Hyperion, Saturn's eighth largest moon, has a chaotic spin
and orbits Saturn every 21 days.
--NASA and SPACE.com Staff
Credit: NASA/JPL/University of
Arizona/Ames
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