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Saturn's deeply cratered moon Hyperion,
as imaged by the Cassini probe in 2005. Credit: NASA/JPL
Jan 22, 2008
Homing in on Hyperion
The Cassini space probe to
Saturn has observed dark organic deposits inside craters on the
small moon Hyperion. Now, new evidence suggests the material may
have come from another moon--Iapetus.
We have featured
Hyperion in past
Thunderbolts Pictures of the Day because of the anomalous
cratering and sponge-like texture of its surface. But another
mystery has arisen. Recent images acquired by the Cassini space
probe reveal dark
organic deposits collected in the bottom of some its
craters. No one knows what the actual materials are except in
terms of their elemental composition, though NASA scientists have
emphasized that they are all necessary components for life.
An irregular
celestial body with approximate dimensions of 328 x 260 x
214 kilometers,
Hyperion is smaller than
Dione,
Tethys or
Iapetus, which have all been the subjects of recent
Pictures of the Day commentary because they appear to
exhibit
electric discharge effects. The many unusual craters,
steep conical walls and tubular excavations on Hyperion all
point to multiple disruptive events that have carved the
moon into its present
cavernous shape. Craters of varying sizes cover its
entire surface, some measuring several kilometers in
diameter. And this poses once more the question we
we have asked in the past. How does an object of such a
small size and of such a porous nature sustain multiple
impacts blasting out craters nearly as large as the object
itself, without being blown apart?
In reflecting on
images taken in Cassini's
close approach, NASA scientists have suggested that
Hyperion may have acquired its dark-stained material from
its sister moon, Iapetus, though the means by which this may
have occurred are far from clear. On September 10, Cassini
will once again
make a close flyby of Iapetus, and the scientists will
be looking again for answers to the question. The probe with
return once more on October 21, 2007.
From the
standpoint of the Electric Universe theory, transportation
of charged dust and gas (more accurately called plasma)
between planetary bodies is not a unique condition. It has
been considered in these pages many times as an explanation
for the collection of sulfur ions from Io in Jupiter's
plasmasphere and for the exchanges of atmosphere between
Titan and Saturn. Since Hyperion and Iapetus are both
orbiting within Saturn's intense
electromagnetic field, and Iapetus shows evidence of
massive excavation by electric arcs, the dusty debris
expelled from its surface could easily find its way along a
charged pathway to its neighbor Hyperion.
So far,
Enceladus, Tethys and Dione have all been found to be
"geologically active," though just a few years ago it would
have been considered absurd to apply that phrase to Saturn's
small moons. In the Electric Universe proposed by Wal
Thornhill and his colleagues, the present activity is
largely electrical, all pointing to past events that would
have been orders of magnitude
more
energetic. The sputtering of dust that we see today pales by
comparison with the violent events of Saturn's past. And it
is this ancient activity within the Saturnian system that
will account for the abundant scars dominating all of
Saturn's moons.
By Stephen Smith
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