Rings of Saturn

The rings of Saturn are the most extensive planetary ring system of any planet in the Solar System. They consist of countless small particles, ranging in size from micrometres to metres,[1] that form clumps that in turn orbit about Saturn. The ring particles are made almost entirely of water ice, with some contamination from dust and other chemicals.

Although reflection from the rings increases Saturn's brightness, they are not visible from Earth with unaided vision. In 1610, the year after Galileo Galilei first turned a telescope to the sky, he became the very first person to observe Saturn's rings, though he could not see them well enough to discern their true nature. In 1655, Christiaan Huygens was the first person to describe them as a disk surrounding Saturn.[2] Although many people think of Saturn's rings as being made up of a series of tiny ringlets (a concept that goes back to Laplace),[2] true gaps are few. It is more correct to think of the rings as an annular disk with concentric local maxima and minima in density and brightness.[citation needed] On the scale of the clumps within the rings there is much empty space.

There are several gaps within the rings: two opened by known moons embedded within them, and many others at locations of known destabilizing orbital resonances with Saturn's moons. Other gaps remain unexplained. Stabilizing resonances, on the other hand, are responsible for the longevity of several rings, such as the Titan Ringlet and the G Ring.

Well beyond the main rings is the Phoebe ring, which is tilted at an angle of 27 degrees to the other rings and, like Phoebe, orbits in retrograde fashion.

History

Galileo's work
Galileo was the first to observe the rings.

Galileo Galilei was the first to observe the rings in 1610 using his telescope, but was unable to identify them as such. He wrote to the Duke of Tuscany that "[t]he planet Saturn is not alone, but is composed of three, which almost touch one another and never move nor change with respect to one another. They are arranged in a line parallel to the zodiac, and the middle one (Saturn itself) is about three times the size of the lateral ones [the edges of the rings]." He also described Saturn as having "ears". In 1612, the plane of the rings was oriented directly at the Earth and the rings appeared to vanish. Mystified, Galileo wondered, "[h]as Saturn swallowed his children?", referencing the myth of Saturn's consumption of his children to prevent them from overthrowing him.[3] They reappeared again in 1613, further confusing Galileo.[4]

Early astronomers used anagrams as a form of commitment scheme to lay claim to new discoveries before their results were ready for publication. Galileo used smaismrmilmepoetaleumibunenugttauiras for Altissimum planetam tergeminum observavi ("I have observed the most distant planet to have a triple form") for discovering the rings of Saturn.[5]

Ring theory and observations
Robert Hooke noted the shadows (a and b) cast by both the globe and the rings on each other in this 1666 drawing of Saturn.

In 1655, Christiaan Huygens became the first person to suggest that Saturn was surrounded by a ring. Using a 50 power refracting telescope that he designed himself and far superior then those available to Galileo, Huygens observed Saturn and wrote that "It [Saturn] is surrounded by a thin, flat, ring, nowhere touching, inclined to the ecliptic."[4] Robert Hooke was another early observer of the rings of Saturn, and noted the casting of shadows on the rings.[6]

In 1675, Giovanni Domenico Cassini determined that Saturn's ring was composed of multiple smaller rings with gaps between them; the largest of these gaps was later named the Cassini Division. This division is a 4,800 km-wide region between the A Ring and B Ring.[7]

In 1787, Pierre-Simon Laplace suggested that the rings were composed of a large number of solid ringlets.[2]

In 1859, James Clerk Maxwell demonstrated that the rings could not be solid or they would become unstable and break apart. He proposed that the rings must be composed of numerous small particles, all independently orbiting Saturn.[8] Maxwell's theory was proven correct in 1895 through spectroscopic studies of the rings carried out by James Keeler of Lick Observatory.

Physical characteristics
The dark Cassini Division separates the wide inner B Ring and outer A Ring in this image from the HST's ACS (March 22, 2004). The less prominent C Ring is just inside the B Ring.

The dense main rings extend from 7,000 km to 80,000 km above Saturn's equator, with an estimated local thickness of only 10 metres,[9] and are composed of 99.9 percent pure water ice with a smattering of impurities that may include tholins or silicates.[10] The main rings are primarily composed of particles ranging in size from 1 centimetre to 10 metres.[11]

The total mass of the rings is about 3 x 1019 kg. This is a small fraction of the total mass of Saturn (about 50 ppb) and is just a little less than the moon Mimas.[12] There have been recent claims, yet unverified, that this is an underestimate due to clumping in the rings and the mass may be three times this figure.[13]

While the largest gaps in the rings, such as the Cassini Division and Encke Gap, can be seen from Earth, both Voyager spacecraft discovered that the rings have an intricate structure of thousands of thin gaps and ringlets. This structure is thought to arise, in several different ways, from the gravitational pull of Saturn's many moons. Some gaps are cleared out by the passage of tiny moonlets such as Pan,[14] many more of which may yet be discovered, and some ringlets seem to be maintained by the gravitational effects of small shepherd satellites (similar to Prometheus and Pandora's maintenance of the F ring). Other gaps arise from resonances between the orbital period of particles in the gap and that of a more massive moon further out; Mimas maintains the Cassini division in this manner.[15]Still more structure in the rings consists of spiral waves raised by the inner moons' periodic gravitational perturbations at less disruptive resonances.

Cassini space probe view of the unilluminated side of Saturn's rings (May 9, 2007).

Data from the Cassini space probe indicate that the rings of Saturn possess their own atmosphere, independent of that of the planet itself. The atmosphere is composed of molecular oxygen gas (O2) produced when ultraviolet light from the Sun interacts with water ice in the rings. Chemical reactions between water molecule fragments and further ultraviolet stimulation create and eject, among other things, O2. According to models of this atmosphere, H2 is also present. The O2 and H2 atmospheres are so sparse that if the entire atmosphere were somehow condensed onto the rings, it would be about one atom thick.[16] The rings also have a similarly sparse OH (hydroxide) atmosphere. Like the O2, this atmosphere is produced by the disintegration of water molecules, though in this case the disintegration is done by energetic ions that bombard water molecules ejected by Saturn's moon Enceladus. This atmosphere, despite being extremely sparse, was detected from Earth by the Hubble Space Telescope.[17]
Cassini mosaic of Saturn's rings on August 12, 2009, a day after equinox. With the rings pointed at the sun, illumination is from light reflected off Saturn, except on thicker or out-of-plane sections, like the F Ring.

Saturn shows complex patterns in its brightness.[18] Most of the variability is due to the changing aspect of the rings,[19][20] and this goes through two cycles every orbit. However, superimposed on this is variability due to the eccentricity of the planet's orbit that causes the planet to display brighter oppositions in the northern hemisphere than it does in the southern.[21]

In 1980, Voyager 1 made a fly-by of Saturn that showed the F-ring to be composed of three narrow rings that appeared to be braided in a complex structure; it is now known that the outer two rings consist of knobs, kinks and lumps that give the illusion of braiding, with the less bright third ring lying inside them.[citation needed]

New images of the rings taken around the 11 August 2009 equinox of Saturn by NASA's Cassini spacecraft have shown that the rings extend significantly out of the nominal ring plane in a few places. This displacement reaches as much as 2.5 miles (4 km) at the border of the Keeler Gap, due to the out-of-plane orbit of Daphnis, the moon that creates the gap.[22]

Formation
A 2007 artist impression of the aggregates of icy particles that form the 'solid' portions of Saturn's rings. These elongated clumps are continually forming and dispersing. The largest particles are a few metres across.

Saturn's rings may be very old, dating to the formation of Saturn itself. There are two main theories regarding the origin of Saturn's rings. One theory, originally proposed by Édouard Roche in the 19th century, is that the rings were once a moon of Saturn whose orbit decayed until it came close enough to be ripped apart by tidal forces (see Roche limit).[23] A variation of this theory is that the moon disintegrated after being struck by a large comet or asteroid.[24] The second theory is that the rings were never part of a moon, but are instead left over from the original nebular material from which Saturn formed.[citation needed]

It seems likely however that they are composed of debris from the disruption of a moon about 300 km in diameter, bigger than Mimas. The last time there were collisions large enough to be likely to disrupt a moon that large was during the Late Heavy Bombardment some four billion years ago.[25]

The brightness and purity of the water ice in Saturn's rings has been cited as evidence that the rings are much younger than Saturn, perhaps just 100 million years old, as the infall of meteoric dust would have led to darkening of the rings. However, new research indicates that the B Ring may be massive enough to have diluted infalling material and thus avoided substantial darkening over the age of the Solar system. Ring material may be recycled as clumps form within the rings and are then disrupted by impacts. This would explain the apparent youth of some of the material within the rings.[26]

The Cassini UVIS team, led by Larry Esposito, used stellar occultation to discover 13 objects, ranging from 27 metres to 10 km across, within the F ring. They are translucent, suggesting they are temporary aggregates of ice boulders a few metres across. Esposito believes this to be the basic structure of the Saturnian rings, particles clumping together, then being blasted apart.[27]

Subdivisions and structures within the rings

The densest parts of the Saturnian ring system are the A and B Rings, which are separated by the Cassini Division (discovered in 1675 by Giovanni Domenico Cassini). Along with the C Ring, which was discovered in 1850 and is similar in character to the Cassini Division, these regions comprise the main rings. The main rings are denser and contain larger particles than the tenuous dusty rings. The latter include the D Ring, extending inward to Saturn's cloud tops, the G and E Rings and others beyond the main ring system. These diffuse rings are characterised as "dusty" because of the small size of their particles (often about a micrometre); their chemical composition is, like the main rings, almost entirely of water ice. The narrow F Ring, just off the outer edge of the A Ring, is more difficult to categorize; parts of it are very dense, but it also contains a great deal of dust-size particles.

Natural-color mosaic of Cassini narrow-angle camera images of the unilluminated side of Saturn's D, C, B, A and F rings (left to right) taken on May 9, 2007.
The illuminated side of Saturn's rings with the major subdivisions labeled

Tabulated data

Notes:
(1) distance is to centre of gaps, rings and ringlets that are narrower than 1,000 km
(2) unofficial name
(3) Names as designated by the International Astronomical Union, unless otherwise noted. Broader separations between named rings are termed divisions, while narrower separations within named rings are called gaps.
(4) Data mostly from the Gazetteer of Planetary Nomenclature, a NASA factsheet and several papers.[28][29][30]

Major subdivisions of the rings

Name(3)	Distance from Saturn (from center, in km)(4)	Width (km)(4)	Named after
D Ring	66,900   –  74,510	7,500
C Ring	74,658   –   92,000	17,500
B Ring	92,000   –  117,580	25,500
Cassini Division	117,580   –   122,170	4,700	Giovanni Cassini
A Ring	122,170   –   136,775	14,600
Roche Division	136,775   –   139,380	2,600	Édouard Roche
F Ring	140,180 (1)	30   –  500
Janus/Epimetheus Ring(2)	149,000   –  154,000	5,000	Janus and Epimetheus
G Ring	166,000   –  175,000	9,000
Methone Ring Arc(2)	194,230	?	Methone
Anthe Ring Arc(2)	197,665	?	Anthe
Pallene Ring(2)	211,000   –  213,500	2,500	Pallene
E Ring	180,000   –  480,000	300,000
Phoebe Ring	~4,000,000 – >13,000,000		Phoebe

Structures within the C Ring

Name(3)	Distance from Saturn's center (km)(4)	Width (km)(4)	Named after
Colombo Gap	77,870 (1)	150	Giuseppe "Bepi" Colombo
Titan Ringlet	77,870 (1)	25	Titan, moon of Saturn
Maxwell Gap	87,491 (1)	270	James Clerk Maxwell
Maxwell Ringlet	87,491 (1)	64	James Clerk Maxwell
Bond Gap	88,705 (1)	30	William Cranch Bond and George Phillips Bond
1.470RS Ringlet	88,716 (1)	16	its radius
1.495RS Ringlet	90,171 (1)	62	its radius
Dawes Gap	90,210 (1)	20	William Rutter Dawes

Structures within the Cassini Division

* Source:[31]

Name(3)	Distance from Saturn's center (km)(4)	Width (km)(4)	Named after
Huygens Gap	117,680 (1)	285–400	Christiaan Huygens
Huygens Ringlet	117,848 (1)	~17	Christiaan Huygens
Herschel Gap	118,234 (1)	102	William Herschel
Russell Gap	118,614 (1)	33	Henry Norris Russell
Jeffreys Gap	118,950 (1)	38	Harold Jeffreys
Kuiper Gap	119,405 (1)	3	Gerard Kuiper
Laplace Gap	119,967 (1)	238	Pierre-Simon Laplace
Bessel Gap	120,241 (1)	10	Friedrich Bessel
Barnard Gap	120,312 (1)	13	Edward Emerson Barnard

Structures within the A Ring

Name(3)	Distance from Saturn's center (km)(4)	Width (km)(4)	Named after
Encke Gap	133,589 (1)	325	Johann Encke
Keeler Gap	136,530 (1)	35	James Keeler

Oblique (4 degree angle) Cassini images of Saturn's C, B, and A rings (left to right; the F ring is faintly visible in the full size upper image if viewed at sufficient brightness). Upper image: natural color mosaic of Cassini narrow-angle camera photos of the illuminated side of the rings taken on December 12, 2004. Lower image: simulated view constructed from a radio occultation observation conducted on May 3, 2005. Color in the lower image is used to represent information about ring particle sizes.

D Ring
A Cassini image of Saturn's D ring processed to show faint ripples within it; the much brighter C ring appears in the upper left.

The D Ring is the innermost ring, and is very faint. In 1980, Voyager 1 detected within this ring three ringlets designated D73, D72 and D68, with D68 being the discrete ringlet nearest to Saturn. Some 25 years later Cassini images showed that D72 had become significantly fainter and moved planetward by 200 kilometres. Present in the gap between the C ring and D73 is finescale structure with waves 30 kilometres apart.[32]

C Ring

The C Ring is a wide but faint ring located inward of the B Ring. It was discovered in 1850 by William and George Bond, though William R. Dawes and Johann Galle also saw it independently. William Lassell termed it the "Crepe Ring" because it seemed to be composed of darker material than the brighter A and B Rings.[33]

Its vertical thickness is estimated at 5 metres, its mass at around 1.1 × 1018 kilograms, and its optical depth varies from 0.05 to 0.12.[citation needed] That is, between 5 and 12 percent of light shining perpendicularly through the ring is blocked, so that when seen from above, the ring is close to transparent.
The Maxwell Gap and the Maxwell Ringlet on its right side are above and right of center. The Bond Gap is above a broad light band towards the upper right; the Dawes Gap is within a dark band just below the upper right corner.

Colombo Gap and Titan Ringlet

The Colombo Gap lies in the inner C Ring. Within the gap lies the bright but narrow Colombo Ringlet, centered at 77,883 kilometres from Saturn's center, which is slightly elliptical rather than circular. This ringlet is also called the Titan Ringlet as it is governed by an orbital resonance with the moon Titan.[citation needed] At this location within the rings, the length of a ring particle's apsidal precession is equal to the length of Titan's orbital motion, so that the outer end of this eccentric ringlet always points towards Titan.

Maxwell Gap and Ringlet

The Maxwell Gap lies within the outer part of the C Ring. It also contains a dense non-circular ringlet, the Maxwell Ringlet. In many respects this ringlet is similar to the ε ring of Uranus. There are wave-like structures in the middle of both rings. While the wave in the ε ring is thought to be caused by Uranian moon Cordelia, no moon has been discovered in the Maxwell gap as of July 2008.[27]

B Ring

The B Ring is the largest, brightest, and most massive of the rings. Its thickness is estimated as 5 to 15 metres, its mass at 2.8 × 1019 kg, and its optical depth varies from 0.4 to 2.5, meaning that well over 99% of the light passing through some parts of the B Ring is blocked.[citation needed] The B Ring contains a great deal of variation in its density and brightness, nearly all of it unexplained. These are concentric, appearing as narrow ringlets, though the B Ring does not contain any gaps.[citation needed]

Spokes

Dark spokes mark the B ring's sunlit side in low phase angle Cassini images. This is a low bitrate video. Full size video with high bitrate of 471kbps;

Until 1980, the structure of the rings of Saturn was explained as being caused exclusively by the action of gravitational forces. Then images from the Voyager spacecraft showed radial features in the B ring, known as spokes, which could not be explained in this manner, as their persistence and rotation around the rings was not consistent with orbital mechanics.[34] The spokes appear dark in backscattered light, and bright in forward-scattered light (see images in gallery); the transition occurs at a phase angle near 45°. The leading theory regarding the spokes' composition is that they consist of microscopic dust particles suspended away from the main ring by electrostatic repulsion, as they rotate almost synchronously with the magnetosphere of Saturn. The precise mechanism generating the spokes is still unknown, although it has been suggested that the electrical disturbances might be caused by either lightning bolts in Saturn's atmosphere or micrometeoroid impacts on the rings.[35]

The spokes were not observed again until some twenty-five years later, this time by the Cassini space probe. The spokes were not visible when Cassini arrived at Saturn in early 2004. Some scientists speculated that the spokes would not be visible again until 2007, based on models attempting to describe their formation. Nevertheless, the Cassini imaging team kept looking for spokes in images of the rings, and they were next seen in images taken on 5 September 2005.[36]

The spokes appear to be a seasonal phenomenon, disappearing in the Saturnian midwinter and midsummer and reappearing as Saturn comes closer to equinox. Suggestions that the spokes may be a seasonal effect, varying with Saturn's 29.7-year orbit, were supported by their gradual reappearance in the later years of the Cassini mission.[37]

Moonlet

In 2009, during equinox, a moonlet embedded in the B ring was discovered from the shadow it cast. It is estimated to be 400 m in diameter.[1]. It took the provisional designation S/2009 S 1.

Cassini Division
The Cassini Division imaged from the Cassini spacecraft. The Huygens Gap lies at its right border; the Laplace Gap is towards the center. A number of other, narrower gaps are also present.

The Cassini Division is a 4,800 km (2,980 mile) wide region between the A Ring and B Ring. It was discovered in 1675 by Giovanni Cassini. From Earth it appears as a thin black gap in the rings. However, Voyager discovered that the gap is itself populated by ring material bearing much similarity to the C Ring.[27] The division may appear bright in views of the unlit side of the rings, since the relatively low density of material allows more light to be transmitted through the thickness of the rings (see second image in gallery).

The inner edge of the Cassini Division is governed by a strong orbital resonance. Ring particles at this location orbit twice for every orbit of the moon Mimas.[2] The resonance causes Mimas' pulls on these ring particles to accumulate, destabilizing their orbits and leading to a sharp cutoff in ring density. Many of the other gaps between ringlets within the Cassini Division, however, are unexplained.

Huygens Gap

The Huygens Gap is located at the inner edge of the Cassini Division. It contains a dense eccentric ringlet named Huygens Ringlet in the middle. This ringlet demonstrates irregular azimuthal variations of the geometrical width and optical depth, which can be caused by the nearby strong 2:1 resonance with Mimas and by the influence of the eccentric outer edge of the B-ring. There is an additional narrow ringlet just outside the Huygens Ringlet.[27]

A Ring
The central ringlet of the A ring's Encke Gap coincides with Pan’s orbit, implying its particles oscillate in horseshoe orbits.

The A Ring is the outermost of the large, bright rings. Its inner boundary is the Cassini Division and its sharp outer boundary is close to the orbit of the small moon Atlas. The A Ring is interrupted at a location 22% of the ring width from its outer edge by the Encke Gap. A narrower gap 2% of the ring width from the outer edge is called the Keeler Gap.

The thickness of the A Ring is estimated as 10 to 30 metres, its mass as 6.2 × 1018 kg (about the mass of Hyperion), and its optical depth varies from 0.4 to 1.0.[citation needed]

Similarly to the B Ring, the A Ring's outer edge is maintained by an orbital resonance, in this case the 7:6 resonance with Janus and Epimetheus.[citation needed] Other orbital resonances also excite many spiral density waves in the A Ring (and, to a lesser extent, other rings as well), which account for most of its structure. These waves are described by the same physics that describes the spiral arms of galaxies. Spiral bending waves, also present in the A Ring and also described by the same theory, are vertical corrugations in the ring rather than compression waves.[citation needed]

Encke Gap
Waves in the Keeler gap edges induced by the passage of Daphnis.
Near Saturn's equinox, Daphnis and its waves cast shadows on the A Ring.

The Encke Gap is a 325-kilometre-wide gap within the A Ring, centered at a distance of 133,590 kilometres from Saturn's center.[38] It is caused by the presence of the small moon Pan,[39] which orbits within it. Images from the Cassini probe have shown that there are at least three thin, knotted ringlets within the gap.[27] Spiral density waves visible on both sides of it are induced by resonances with nearby moons exterior to the rings, while Pan induces an additional set of spiraling wakes (see image in gallery).[27]

Johann Encke himself did not observe this gap; it was named in honour of his ring observations. The gap itself was discovered by James Edward Keeler in 1888.[40] The second major gap in the A Ring, discovered by Voyager, was named the Keeler Gap in his honor.[41]

The Encke Gap is a gap because it is entirely within the A Ring. There was some ambiguity between the terms gap and division until the IAU clarified the definitions in 2008; before that, the separation was sometimes called the "Encke Division".[citation needed]

Keeler Gap

The Keeler Gap is a 42-kilometre-wide gap in the A Ring, approximately 250 kilometres from the ring's outer edge. The small moon Daphnis, discovered 1 May 2005, orbits within it, keeping it clear.[42] The moon induces waves in the edges of the gap.[27] Because the orbit of Daphnis is slightly inclined to the ring plane, the waves have a component that is perpendicular to the ring plane, reaching a distance of 1.5 km (0.93 mi) "above" the plane.[43][44]

The Keeler gap was discovered by Voyager, and named in honor of the astronomer James Edward Keeler. Keeler had in turn discovered and named the Encke Gap in honor of Johann Encke.[40]

Moonlets
Location of the first four moonlets detected in the A ring.

In 2006, four tiny "moonlets" were found in Cassini images of the A Ring.[45] The moonlets themselves are only about a hundred metres in diameter, too small to be seen directly; what Cassini sees are the "propeller"-shaped disturbances the moonlets create, which are several kilometres across. It is estimated that the A Ring contains thousands of such objects. In 2007, the discovery of eight more moonlets revealed that they are largely confined to a 3000-km belt, about 130,000 km from Saturn's center,[46] and by 2008 over 150 propeller moonlets had been detected.[47]

Roche Division
The Roche Division (passing through image center) between the A Ring and the narrow F Ring. Atlas can be seen within it. The Encke and Keeler gaps are also visible.

The separation between the A Ring and the F Ring has been named the Roche Division in honor of the French physicist Édouard Roche.[3] The Roche Division should not be confused with the Roche limit, a physical concept that describes when a large object gets so close to a planet (such as Saturn) that the planet's tidal forces will pull it apart.[citation needed] Lying at the outer edge of the main ring system, the Roche Division is in fact close to Saturn's Roche limit, which is why the rings have been unable to accrete into a moon.[citation needed]

Like the Cassini Division, the Roche Division is not empty but contains a sheet of material.[citation needed] The character of this material is similar to the tenuous and dusty D, E, and G Rings.[citation needed] Two locations in the Roche Division have a higher concentration of dust than the rest of the region. These were discovered by the Cassini probe imaging team and were given temporary designations: R/2004 S 1, which lies along the orbit of the moon Atlas; and R/2004 S 2, centered at 138,900 km from Saturn's center, inward of the orbit of Prometheus.[citation needed]

F Ring

The shepherd moons Pandora (left) and Prometheus (right) orbit on either side of the F ring; Prometheus is followed by dark channels that it has carved into the inner strands of the ring.

The F Ring is the outermost discrete ring of Saturn and perhaps the most active ring in the Solar system, with features changing on a timescale of hours.[48] It is located 3,000 km beyond the outer edge of the A Ring.[49] It was discovered in 1979 by the Pioneer 11 imaging team.[50] It is very thin, just a few hundred kilometres wide, and is held together by two shepherd moons, Prometheus and Pandora, which orbit inside and outside it.[39]

Recent closeup images from the Cassini probe show that the F Ring consists of one core ring and a spiral strand around it.[51] They also show that when Prometheus encounters the ring at its apoapsis, its gravitational attraction creates kinks and knots in the F Ring as the moon 'steals' material from it, leaving a dark channel in the inner part of the ring (see video link and additional F Ring images in gallery). Since Prometheus orbits Saturn more rapidly than the material in the F ring, each new channel is carved about 3.2 degrees in front of the previous one.[48]

In 2008, further dynamism was detected, suggesting that small unseen moons orbiting within the F Ring are continually passing through its narrow core because of perturbations from Prometheus. One of the small moons was tentatively identified as S/2004 S 6.[48]
A mosaic of 107 images showing 255° (about 70%) of the F Ring as it would appear if straightened out. The radial width (top to bottom) is 1,500 km.

Outer rings
The outer rings seen back-illuminated by the Sun
The Anthe Ring Arc. The bright spot is Anthe.
The backlit E ring, with Enceladus silhouetted against it. The moon's south polar jets erupt brightly below it.

Janus/Epimetheus Ring

A faint dust ring is present around the region occupied by the orbits of Janus and Epimetheus, as revealed by images taken in forward-scattered light by the Cassini spacecraft in 2006. The ring has a radial extent of about 5,000 km.[52] Its source is particles blasted off the moons' surfaces by meteoroid impacts, which then form a diffuse ring around their orbital paths.[53]

G Ring

The G Ring (see last image in gallery) is a very thin, faint ring about halfway between the F Ring and the beginning of the E Ring, with its inner edge about 15,000 km inside the orbit of Mimas. It contains a single distinctly brighter arc near its inner edge (similar to the arcs in the rings of Neptune) that extends about one sixth of its circumference, centered on the half-kilometre diameter moonlet Aegaeon, which is held in place by a 7:6 orbital resonance with Mimas.[54][55] The arc is believed to be composed of icy particles up to a few metres in diameter, with the rest of the G Ring consisting of dust released from within the arc. The radial width of the arc is about 250 km, compared to a width of 9,000 km for the G Ring as a whole.[54] The arc is thought contain matter equivalent to a small icy moonlet about a hundred metres in diameter.[54] Dust released from Aegaeon and other source bodies within the arc by micrometeoroid impacts drifts outward from the arc because of interaction with Saturn's magnetosphere (whose plasma corotates with Saturn's magnetic field, which rotates much more rapidly than the orbital motion of the G Ring). These tiny particles are steadily eroded away by further impacts and dispersed by plasma drag. Over the course of thousands of years the ring gradually loses mass,[56] which is replenished by further impacts on Aegaeon.
[edit] Methone Ring Arc

A faint ring arc, first detected in September 2006, covering a longitudinal extent of about 10 degrees is associated with the moon Methone. The material in the arc is believed to represent dust ejected from Methone by micrometeoroid impacts. The confinement of the dust within the arc is attributable to a 14:15 resonance with Mimas (similar to the mechanism of confinement of the arc within the G ring).[57] Under the influence of the same resonance, Methone librates back and forth in its orbit with an amplitude of 5° of longitude.

Anthe Ring Arc

A faint ring arc, first detected in June 2007, covering a longitudinal extent of about 20 degrees is associated with the moon Anthe. The material in the arc is believed to represent dust knocked off Anthe by micrometeoroid impacts. The confinement of the dust within the arc is attributable to a 10:11 resonance with Mimas. Under the influence of the same resonance, Anthe drifts back and forth in its orbit over 14° of longitude.[57]

Pallene Ring

A faint dust ring shares Pallene's orbit, as revealed by images taken in forward-scattered light by the Cassini spacecraft in 2006.[52] The ring has a radial extent of about 2,500 km. Its source is particles blasted off Pallene's surface by meteoroid impacts, which then form a diffuse ring around its orbital path.[53]

E Ring

The E Ring is the outermost ring, and is extremely wide, beginning at the orbit of Mimas and ending somewhere around the orbit of Rhea. It is a diffuse disk consisting mostly of ice, with silicates, carbon dioxide and ammonia.[58] Unlike the other rings, it is composed of microscopic rather than macroscopic particles. In 2005, the source of the E Ring's material was determined to be cryovolcanic plumes[59][60] emanating from the "tiger stripes" of the south polar region of the moon Enceladus.

Phoebe ring
The Phoebe ring's huge extent dwarfs the main rings. Inset: 24 micron Spitzer image of part of the ring.

On 6 October 2009, the discovery of a tenuous disk of material in the plane of and just interior to the orbit of Phoebe was announced. This disk can be loosely described as another ring. Although very large, the ring is virtually invisible – it was discovered using NASA's infra-red Spitzer Space Telescope.[61] The ring was seen over the entire range of the observations, which extended from 128 to 207 times the radius of Saturn,[62] with calculations indicating that it may extend outward up to 300 Saturn radii and inward to the orbit of Iapetus at 59 Saturn radii;[63] Phoebe orbits the planet at an average distance of 215 radii. The ring is about 20 times as thick as the diameter of the planet.[64] Since the ring's particles are presumed to have originated from impacts (micrometeoroid and larger) on Phoebe, they should share its retrograde orbit,[63] which is opposite to the orbital motion of the next inner moon, Iapetus. This ring lies in the plane of Saturn's orbit, or roughly the ecliptic, and thus is tilted 27 degrees from Saturn's equatorial plane and the other rings. Phoebe is inclined by 5° with respect to Saturn's orbit plane (often written as 175°, due to Phoebe's retrograde orbital motion), and its resulting vertical excursions above and below the ring plane agree closely with the ring's observed thickness of 40 Saturn radii.

The existence of the ring was proposed in the 1970s by Steven Soter.[63] The discovery was made by Anne J. Verbiscer and Michael F. Skrutskie (of the University of Virginia) and Douglas P. Hamilton (of the University of Maryland, College Park).[62][65] Verbiscer, Skrutskie and Hamilton had been graduate students together at Cornell University.[66]

Ring material migrates inward due to reemission of solar radiation,[62] and would thus strike the leading hemisphere of Iapetus. Infall of this material causes a slight darkening and reddening of the leading hemisphere of Iapetus (similar to what is seen on the Uranian moons Oberon and Titania) but does not directly create the dramatic two-tone coloration of that moon.[67] Rather, the infalling material initiates a positive feedback thermal self-segregation process of ice sublimation from warmer regions, followed by vapor condensation onto cooler regions. This leaves a dark residue of "lag" material covering most of the equatorial region of Iapetus's leading hemisphere, which contrasts with the bright ice deposits covering the polar regions and most of the trailing hemisphere.[68][69][70]

Possible ring system around Rhea
Main article: Rings of Rhea

Saturn's second largest moon Rhea may have a tenuous ring system of its own consisting of three narrow bands embedded in a disk of solid particles.[71][72] These rings have not been imaged, but their existence has been inferred from Cassini observations in November 2005 of a depletion of energetic electrons in Saturn's magnetosphere near Rhea. The Magnetospheric Imaging Instrument (MIMI) observed a gentle gradient punctuated by three sharp drops in plasma flow on each side of the moon in a nearly symmetric pattern. This could be explained if they were absorbed by solid material in the form of an equatorial disk containing denser rings or arcs, with particles perhaps several decimetres to approximately a metre in diameter. However, not all scientists are convinced that the observations were caused by a ring system. A more recent piece of evidence supporting the presence of Rhean rings is a set of small ultraviolet-bright spots distributed in a line that extends three quarters of the way around the moon's circumference, within 2 degrees of the equator. The spots presumably represent the impact points of deorbiting ring material.[73]

See also

* Édouard Roche – French astronomer who described how the breakup of a satellite could form the rings, when it comes within the Roche limit of a celestial body.
* Galileo Galilei – the first person to observe Saturn's rings, in 1610
* Christian Huygens – the first person to propose that there was a ring surrounding Saturn, in 1655
* Giovanni Cassini – discovered the separation between the A and B rings, in 1675 – (Cassini Division)

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External links

* Planetary Rings Node: Saturn's Ring System
* Saturn's Rings by NASA's Solar System Exploration
* Gazeteer of Planetary Nomenclature - Ring and Ring Gap Nomenclature (Saturn), USGS
* NASA finds giant ring around Saturn - Yahoo 7 news (retrieved 2009-10-07)