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Red-Faced Worlds
Nov
13, 2009
Some of Saturn's moons are
slightly red in color, as are other
bodies in the Solar System.
"Mars the red planet" is a familiar
phrase. The planet exhibits a faint
yellowish-red color when seen with
the naked eye, and its rusty surface
hue is visible through the lenses of
robotic rovers traveling across its
landscape.
Iapetus, one of Saturn's more
enigmatic moons, is notable for a
reddish-black deposit covering one
hemisphere. Hyperion's heavily
cratered surface is also dusted with
what appears to be the same "soot"
that covers Iapetus. The material
piles into drifts inside some of
Hyperion's deeper craters.
According to a recent press release,
new maps of Mimas, Enceladus, Rhea,
Dione, and Tethys show them all to
have patches of red to some degree.
All the new maps indicate that,
except for Mimas, they are all
redder on their trailing hemispheres
and tend to be more intense in the
center of the disk. Although the
leading face of the moons is also
red, it is not as strong
Scientists from the Lunar and
Planetary Institute in Houston admit
that the pattern on both hemispheres
is "difficult to explain" because
only one hemisphere or the other
would normally be affected.
Bombardment by a train of meteors,
or particles from Saturn's rings,
should accumulate on the leading
hemispheres.
However, it is most likely a plasma,
in the form of high energy ions that
is flowing into the moons from their
supercharged electrical parent that
is contributing to the coloration.
Electrical theorists argue that
Saturn moves within the plasmasphere
of the Sun and
interacts with the Sun’s
electric field. Since planets and
moons in the Solar System are
charged bodies that are not isolated
in space, it is to be expected that
they
transact electrically with each
other.
In the image at the top of the page,
a dark equatorial stripe is faintly
visible across the leading face of
Tethys. The stripe is bright at
ultraviolet wavelengths, but dark in
the infrared. Mimas shares a similar
feature, a dark band stretching more
than halfway around its
circumference.
The moons emit ionic plumes because
of their position in Saturn’s
circuit. The
ring formation around
Rhea is probably the remains of
pulverized rock and ice that
billions of watts of electricity
created when they catastrophically
passed through the moon’s conductive
strata at some time in the past.
More than one quarter of Phoebe's
mass has been removed and has been
distributed throughout the Saturnian
system. The reddish-black soot
covering the other inner moons of
Saturn most likely came from Phoebe.
Similar discharge phenomena can be
seen on Jupiter’s moon Europa,
including the red color of the
material. Close-up images reveal
narrow darker deposits that trace
the path of subsurface electric
discharges. It is those discharges
that altered Europa's surface
composition, transforming the water
ice into other materials. Some of
the altered material created the
coloration.
Europa's red color is due to oxygen
atoms from water ice forming a
sulfur atom. On Mars, the volume of
sulfur in the environment is high,
contributing to its ruddy
complexion, but the oxides of iron
that abound there appear to be the
primary influence.
Recently, observations of the dwarf
planet
Haumea's reflected brightness
revealed the presence of a dark spot
on the dimmer side. The spot also
has a reddish tint that could be due
to a concentration of compounds that
reflect red light. Haumea revolves
around the Sun in an orbital path
out past Neptune and into the
farthest reach of Pluto's orbit. A
previous Picture of the Day
considered other remote objects
called Centaurs. Along with Mars and
the moons under discussion, they are
also colorful. Some are green and
some are blue, but the primary color
is a brick or rust-red.
The Electric Universe suggests a
reason for the different colored
planets and moons, as well as for
the different chemical compositions.
Stars are formed when cosmic
Birkeland currents twist around one
another, creating z-pinch regions
that compress plasma. Laboratory
experiments have shown that such
compression zones are likely
candidates for star formation.
Stars that are under extreme
electrical stress may will split
into two or more daughter stars,
thereby reducing each one's
electrical potential. Further
activity may result in the ejection
of stars with too little electrical
energy to glow, so the resulting
objects will be gas giant planets in
dark mode. Gas giants, in turn, will
eject rocky objects from their
plasma cores if there is a
disequilibrium.
All of the daughter objects in orbit
about their parents are connected to
them in vast electric circuits.
Those circuits were once energized
to an awesome extent and carried
material from one to another along
cosmic electrical transmission lines
called Birkeland currents. The
charged nuclei of ionized iron,
oxygen, sulfur flowed along those
currents between the celestial
bodies in an exchange of elements.
Stephen Smith
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