F ring close up
Visual-wavelength image
PandoraPandora
PrometheusPrometheus
Because of collisions among ring particles, planetary rings should spread outward.
The sharp outer edge of the A ring and the narrow F ring are confined by
shepherd satellitesthat gravitationally usher straying particles back into the rings.
Some gaps in the rings, such as the Cassini Division, are caused by
resonances with moons. A particle in the Cassini Division orbits Saturn twice
for each orbit of the moon Mimas. On every other orbit, the particle feels a
gravitational tug from Mimas. These tugs always
occur at the same places in the orbit and force
the orbit to become slightly elliptical. Such an
orbit crosses the orbits of other particles,
which results in collisions, and that
removes the particle from the gap.
The F ring is clumpy and
sometimes appears braided
because of two shepherd
satellites.
The Encke Gap is not
empty. Note the ripples
at the inner edge. A
small moon orbits inside
the gap.
Encke Gap
Waves in the A ring
Visual-
wavelength
images
Saturn does not have enough
moons to produce all of its
ringlets by resonances. Many
are produced by tightly wound
waves, much like the spiral
arms found in disk galaxies.
How do moons happen to be at just the right
places to confine the rings? That puts the
cosmic cart before the horse. The ring particles
get caught in the most stable orbits among
Saturn’s innermost moons. The rings push
against the inner moons, but those moons are
locked in place by resonances with larger,
outer moons. Without the moons, the rings
would spread and dissipate.
Saturn’s rings are a very thin layer of particles
and nearly vanish when the rings turn edge-on to
Earth. Although ripples in the rings caused by waves
may be hundreds of meters high, the sheet of particles
may be only about ten meters thick.
This image was recorded by
the Cassini spacecraft looking
up at the rings as they were
illuminated by sunlight from
below. Saturn’s shadow falls across
the upper side
of the rings.
This combination of UV images has been
given false color to show the ratio of
mineral material to pure ice. Blue regions
such as the A ring are the purest ice, and
red regions such as the Cassini Division
are the dirtiest ice. How the particles
become sorted by composition is
unknown.
A ring
Cassini Division Encke Gap
This combination of UV images has been
given false color to show the ratio of
mineral material to pure ice. Blue regions
such as the A ring are the purest ice, and
red regions such as the Cassini Division
are the dirtiest ice. How the particles
become sorted by composition is
unknown.
F ring
A ring
Cassini Division Encke Gap
Ultraviolet imageUltraviolet image
NASA/JPL/Space Science Institute
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