The research «gives ironclad proof» of the existence of
moonlets in the F ring, says astronomer Douglas Hamilton of the University of Maryland, College Park.
Instead, it will be left in orbit, becoming a long - lived mechanical
moonlet of Ceres once its mission ends.
A new study led by University of Idaho researchers suggests there could be two tiny, previously undiscovered
moonlets orbiting near two of the planet's rings.
The Pluto system has
moonlets with orbits that focus on the point that the Pluto / Charon pair both orbit.
This unique structure might be caused by gravitational disturbances of a
small moonlet in an eccentric orbit that has apparently criss - crossed the F ring for almost 9 months.
University of Idaho researchers believe Uranus has two previously
undiscovered moonlets in the planet's alpha and beta ring.
Some of Mars» several thousand elliptical craters may even have been formed by remnants of
such moonlets crashing to the surface at a grazing angle.
Esposito's model, which draws on work by former graduate students Joshua Colwell, Robin Canup, and John Barbara, takes into account
tiny moonlets within the rings that have enough of a gravitational attraction to hold on to the particles, keeping them in the system.
They found the pattern in Uranus» rings was similar to moon - related structures in Saturn's rings
called moonlet wakes.
The
hypothesized moonlet pushing a cooling magma ocean and its KREEP to the lunar near side would explain the dichotomy.
These planetary jewels, carved
by moonlets and shaped by gravity, could well have looked much the same now as they did billions of years ago — but only from afar.
There moonlets coagulate from the ring material before migrating outward.
Newfound moonlets only a few hundred feet wide contribute to the distortion, but other causes of the structural richness remain undetected.
Alternatively, they posit that small, rubble -
pile moonlets could be transporting the dense, icy particles as they migrate within the ring.
Within the rings themselves, Cassini spied
tumbling moonlets that sculpted the surrounding dust into towering waves and jagged ridges.
No other planet boasts such a singular and striking companion: Mercury and Venus have no moons at all, Mars has two tiny spud - shaped satellites, and the
many moonlets of the gas giants are tiny in comparison with their mother planets.
The latest images of Saturn's rings, which show propeller - shaped clumps and
moonlets shattered by an ancient impact, are also giving astronomers a lot to think about.
For instance, newly found arcs in the remote and tenuous G ring, reminiscent of the ring arcs of the planet Neptune, are probably caused by the gravitational influence of a
nearby moonlet, yet to be discovered.
In 2006 Cassini discovered football - field - size wakes caused by previously
undetected moonlets orbiting within the A ring.
Even larger objects, known
as moonlets, were suspected to be disrupting the ring in such a way as to cause periodic jets of dust to shoot hundreds of kilometers into space.
The actions of small
moonlets often force geysers of material to shoot out from Saturn's F ring.
As for the shifting braids, the researchers conclude that they result from the motion of as - yet -
identified moonlets through the ring — a hypothesis confirmed by computer models — and the occasional influence of Prometheus, a potato - shaped moon that orbits in the gap between the F ring and Saturn's much bigger A ring.
«I would be very pleased if these
proposed moonlets turn out to be real and we can use them to approach a solution.»
A near miss with a
pre-existing moonlet is more effective at producing capture than is actual collision — a larger prograde momentum (one in the direction of the planet's spin) is transferred to the captured moon.
As Cassini maneuvers for its eventual suicide dive between the planet and its rings, new shots
capture moonlets, density waves and other mysteries at the highest resolution yet
GRAIL, which will map the moon's gravitational field to expose variations in its near - surface density, may be able to detect the residual effects of a long -
lost moonlet pancaked across the lunar far side.
In Jutzi and Asphaug's computer simulations, the pancaking of a
solid moonlet against a partly molten moon would provide enough material to create the elevated highlands on one hemisphere and would displace huge amounts of magma to the opposite hemisphere.
This sequence of three images, obtained by NASA's Cassini spacecraft over the course of about 10 minutes, shows the path of a newly
found moonlet in a bright arc of Saturn's faint G ring.
Chancia and Hedman estimate the
supposed moonlets in the rings of Uranus, the seventh planet from the sun, are two to nine miles in diameter.
The
little moonlet, which according to The Verge is about 20 miles wide and resembles «a little space rock with what looks like two googly eyes,» resides in what is known as the Encke Gap, a 200 - mile - wide space between Saturn's rings that is caused by the diminutive object itself.
In addition, Cassini participating scientist and imaging team associate Matt Tiscareno of SETI Institute, Mountain View, California, provided new details about the whimsically named ring features called propellers, which are wakes in the rings created by small,
unseen moonlets.
«It's likely that
such moonlets were later ejected, or collided with Earth or with each other to form bigger moons.»
On September 13 and 14, Cassini took a last look around the Saturn system's greatest hits, taking a color mosaic image of Saturn and the rings, a movie sequence of Enceladus setting behind Saturn, Titan and
tiny moonlets in the rings that pull the icy ring particles around themselves to form features called propellers.
A model of recent formation processes near Saturn's rings fits well with the planet's observed population of so - called moonlets
The researchers estimate the
hypothesized moonlets in Uranus» rings would be 2 to 9 miles (4 to 14 kilometers) in diameter — as small as some identified moons of Saturn, but smaller than any of Uranus» known moons.
Launched in 1997, the Cassini mission has been working since July 2004 to study the gas giant and its huge family of 62 moons and several
smaller moonlets.
Now, decades later, a study from University of Idaho researchers suggests the planet could have two previously
undiscovered moonlets.
These formations might result from the extreme compression of material passing around small «
moonlets» that have been caught in the resonance at the ring's edge like rushing water splashing against a large cliff face on the shore.
The end result is a neatly ordered satellite system, with small moons on the inside built from few
moonlets and large moons farther out built from numerous moonlets.
As the ring system spits out
moonlet after moonlet, the small objects merge to form larger moons, which may merge in turn as they spiral outward from the planet.
The moonlets could disperse the icy chunks in the middle A ring as they break up there under the gravitational influence of Saturn and its larger moons.
Eventually, gravitational tugs from the sun would destabilise
the moonlets, making them crash into the bigger one.
While Enceladus and Titan stole the show, Cassini, on its way to taking a total of more than 450,000 images, documented the intricacies of Saturn and its orbiting rings and
moonlets.
Astronomers believe large
moonlets up to at least a half - mile in size may hide among the rings, which themselves are only about 30 feet thick; the taller vertical structures visible here could be ring material that «splashes» up when the fine particles of the rings collide with these moonlets, much as water at the sea's edge can splash up and over a rock.
In the hours before Cassini becomes a miniscule spark spiraling into Saturn's massive atmosphere, one of its final tasks will be capturing and sending back images of its most cherished targets: Titan and its methano - logical weather; Enceladus and its watery plumage setting behind Saturn's northern rim;
a moonlet nicknamed «Peggy» being born at the edge of a ring; and a family portrait of the planet and its rings.
Because Charon is a moon of Pluto, we could say
these moonlets orbit a moon.
To check the conditions for the formation of such mini-moons or
moonlets the researchers ran 800 simulations of impacts with Earth.
Collisions between
the moonlets and smaller bits of debris in the rings knock new material loose from the moonlets, keeping the recycling process going, he concludes: «Individual rings survive only a few million years, but the system lasts indefinitely.»
In fact, that's a mystery in itself: The F ring is believed to contain many large boulders and
moonlets, which would make it hard for a small satellite to survive multiple crossings.
Now a European team has caught
this moonlet in the act.