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A natural satellite is, in the most common usage, an astronomical body that orbits a planet, dwarf planet, or small Solar System body (or sometimes another natural satellite). Natural satellites are colloquially referred to as moons, a derivation from the Moon of Earth.

In the Solar System, there are six planetary satellite systems containing 288 known natural satellites altogether. Seven objects commonly considered dwarf planets by astronomers are also known to have natural satellites: Orcus, Pluto, Haumea, Quaoar, Makemake, Gonggong, and Eris. As of January 2022, there are 447 other minor planets known to have natural satellites.

A planet usually has at least around 10,000 times the mass of any natural satellites that orbit it, with a correspondingly much larger diameter. The Earth–Moon system is a unique exception in the Solar System; at 3,474 kilometres (2,158 miles) across, the Moon is 0.273 times the diameter of Earth and about 1⁄80 of its mass. The next largest ratios are the Neptune–Triton system at 0.055 (with a mass ratio of about 1 to 4790), the Saturn–Titan system at 0.044 (with the second mass ratio next to the Earth–Moon system, 1 to 4220), the Jupiter–Ganymede system at 0.038, and the Uranus–Titania system at 0.031. For the category of dwarf planets, Charon has the largest ratio, being 0.52 the diameter and 12.2% the mass of Pluto.

Terminology

The first known natural satellite was the Moon, but it was considered a "planet" until Copernicus' introduction of De revolutionibus orbium coelestium in 1543. Until the discovery of the Galilean satellites in 1610 there was no opportunity for referring to such objects as a class. Galileo chose to refer to his discoveries as Planetæ ("planets"), but later discoverers chose other terms to distinguish them from the objects they orbited.

The first to use the term satellite to describe orbiting bodies was the German astronomer Johannes Kepler in his pamphlet Narratio de Observatis a se quatuor Iouis satellitibus erronibus ("Narration About Four Satellites of Jupiter Observed") in 1610. He derived the term from the Latin word satelles, meaning "guard", "attendant", or "companion", because the satellites accompanied their primary planet in their journey through the heavens.

The term satellite thus became the normal one for referring to an object orbiting a planet, as it avoided the ambiguity of "moon". In 1957, however, the launching of the artificial object Sputnik created a need for new terminology. The terms man-made satellite and artificial moon were very quickly abandoned in favor of the simpler satellite. As a consequence, the term has become linked primarily with artificial objects flown in space.

Because of this shift in meaning, the term moon, which had continued to be used in a generic sense in works of popular science and fiction, has regained respectability and is now used interchangeably with natural satellite, even in scientific articles. When it is necessary to avoid both the ambiguity of confusion with Earth's natural satellite the Moon and the natural satellites of the other planets on the one hand, and artificial satellites on the other, the term natural satellite (using "natural" in a sense opposed to "artificial") is used. To further avoid ambiguity, the convention is to capitalize the word Moon when referring to Earth's natural satellite (a proper noun), but not when referring to other natural satellites (common nouns).

Many authors define "satellite" or "natural satellite" as orbiting some planet or minor planet, synonymous with "moon" – by such a definition all natural satellites are moons, but Earth and other planets are not satellites. A few recent authors define "moon" as "a satellite of a planet or minor planet", and "planet" as "a satellite of a star" – such authors consider Earth as a "natural satellite of the Sun".

Definition of a moon

There is no established lower limit on what is considered a "moon". Every natural celestial body with an identified orbit around a planet of the Solar System, some as small as a kilometer across, has been considered a moon, though objects a tenth that size within Saturn's rings, which have not been directly observed, have been called moonlets. Small asteroid moons (natural satellites of asteroids), such as Dactyl, have also been called moonlets.

The upper limit is also vague. Two orbiting bodies are sometimes described as a double planet rather than a primary and satellite. Asteroids such as 90 Antiope are considered double asteroids, but they have not forced a clear definition of what constitutes a moon. Some authors consider the Pluto–Charon system to be a double (dwarf) planet. The most common dividing line on what is considered a moon rests upon whether the barycentre is below the surface of the larger body, though this is somewhat arbitrary because it depends on distance as well as relative mass.

Origin and orbital characteristics

The natural satellites orbiting relatively close to the planet on prograde, uninclined circular orbits (regular satellites) are generally thought to have been formed out of the same collapsing region of the protoplanetary disk that created its primary. In contrast, irregular satellites (generally orbiting on distant, inclined, eccentric and/or retrograde orbits) are thought to be captured asteroids possibly further fragmented by collisions. Most of the major natural satellites of the Solar System have regular orbits, while most of the small natural satellites have irregular orbits. The Moon and the Moons of Pluto are exceptions among large bodies in that they are thought to have originated from the collision of two large protoplanetary objects early in the Solar System's history (see the giant impact hypothesis). The material that would have been placed in orbit around the central body is predicted to have reaccreted to form one or more orbiting natural satellites. As opposed to planetary-sized bodies, asteroid moons are thought to commonly form by this process. Triton is another exception; although large and in a close, circular orbit, its motion is retrograde and it is thought to be a captured dwarf planet.

Temporary satellites

The capture of an asteroid from a heliocentric orbit is not always permanent. According to simulations, temporary satellites should be a common phenomenon. The only observed examples are 1991 VG, 2006 RH120, 2020 CD3.

2006 RH120 was a temporary satellite of Earth for nine months in 2006 and 2007.

Tidal locking

Most regular moons (natural satellites following relatively close and prograde orbits with small orbital inclination and eccentricity) in the Solar System are tidally locked to their respective primaries, meaning that the same side of the natural satellite always faces its planet. This phenomenon comes about through a loss of energy due to tidal forces raised by the planet, slowing the rotation of the satellite until it is negligible. Exceptions are known; one such exception is Saturn's natural satellite Hyperion, which rotates chaotically because of the gravitational influence of Titan. Pluto's four, circumbinary small moons also rotate chaotically due to Charon's influence.

In contrast, the outer natural satellites of the giant planets (irregular satellites) are too far away to have become locked. For example, Jupiter's Himalia, Saturn's Phoebe, and Neptune's Nereid have rotation periods in the range of ten hours, whereas their orbital periods are hundreds of days.

Satellites of satellites

No "moons of moons" or subsatellites (natural satellites that orbit a natural satellite of a planet) are currently known. In most cases, the tidal effects of the planet would make such a system unstable.

However, calculations performed after the 2008 detection of a possible ring system around Saturn's moon Rhea indicate that satellites orbiting Rhea could have stable orbits. Furthermore, the suspected rings are thought to be narrow, a phenomenon normally associated with shepherd moons. However, targeted images taken by the Cassini spacecraft failed to detect rings around Rhea.

It has also been proposed that Saturn's moon Iapetus had a satellite in the past; this is one of several hypotheses that have been put forward to account for its equatorial ridge.

Light-curve analysis suggests that Saturn's irregular satellite Kiviuq is extremely prolate, and is likely a contact binary or even a binary moon.

Trojan satellites

Two natural satellites are known to have small companions at both their L₄ and L₅ Lagrangian points, sixty degrees ahead and behind the body in its orbit. These companions are called trojan moons, as their orbits are analogous to the trojan asteroids of Jupiter. The trojan moons are Telesto and Calypso, which are the leading and following companions, respectively, of the Saturnian moon Tethys; and Helene and Polydeuces, the leading and following companions of the Saturnian moon Dione.

Asteroid satellites

The discovery of 243 Ida's natural satellite Dactyl in the early 1990s confirmed that some asteroids have natural satellites; indeed, 87 Sylvia has two. Some, such as 90 Antiope, are double asteroids with two comparably sized components.

Shape

Neptune's moon Proteus is the largest irregularly shaped natural satellite; the shapes of Eris' moon Dysnomia and Orcus' moon Vanth are unknown. All other known natural satellites that are at least the size of Uranus's Miranda have lapsed into rounded ellipsoids under hydrostatic equilibrium, i.e. are "round/rounded satellites" and are sometimes categorized as planetary-mass moons. (Dysnomia's density is known to be high enough that it is probably a solid ellipsoid as well.) The larger natural satellites, being tidally locked, tend toward ovoid (egg-like) shapes: squat at their poles and with longer equatorial axes in the direction of their primaries (their planets) than in the direction of their motion. Saturn's moon Mimas, for example, has a major axis 9% greater than its polar axis and 5% greater than its other equatorial axis. Methone, another of Saturn's moons, is only around 3 km in diameter and visibly egg-shaped. The effect is smaller on the largest natural satellites, where their gravity is greater relative to the effects of tidal distortion, especially those that orbit less massive planets or, as in the case of the Moon, at greater distances.

Geological activity

Of the twenty known natural satellites in the Solar System that are large enough to be gravitationally rounded, several remain geologically active today. Io is the most volcanically active body in the Solar System, while Europa, Enceladus, Titan and Triton display evidence of ongoing tectonic activity and cryovolcanism. In the first three cases, the geological activity is powered by the tidal heating resulting from having eccentric orbits close to their giant-planet primaries. (This mechanism would have also operated on Triton in the past before its orbit was circularized.) Many other natural satellites, such as Earth's Moon, Ganymede, Tethys, and Miranda, show evidence of past geological activity, resulting from energy sources such as the decay of their primordial radioisotopes, greater past orbital eccentricities (due in some cases to past orbital resonances), or the differentiation or freezing of their interiors. Enceladus and Triton both have active features resembling geysers, although in the case of Triton solar heating appears to provide the energy. Titan and Triton have significant atmospheres; Titan also has hydrocarbon lakes. All four of the Galilean moons have atmospheres, though they are extremely thin. Four of the largest natural satellites, Europa, Ganymede, Callisto, and Titan, are thought to have subsurface oceans of liquid water, while smaller Enceladus also supports a global subsurface ocean of liquid water.

Occurrence in the Solar System

Besides planets and dwarf planets objects within our Solar System known to have natural satellites are 76 in the asteroid belt (five with two each), four Jupiter trojans, 39 near-Earth objects (two with two satellites each), and 14 Mars-crossers. There are also 84 known natural satellites of trans-Neptunian objects. Some 150 additional small bodies have been observed within the rings of Saturn, but only a few were tracked long enough to establish orbits. Planets around other stars are likely to have satellites as well, and although numerous candidates have been detected to date, none have yet been confirmed.

Of the inner planets, Mercury and Venus have no natural satellites; Earth has one large natural satellite, known as the Moon; and Mars has two tiny natural satellites, Phobos and Deimos. The giant planets have extensive systems of natural satellites, including half a dozen comparable in size to Earth's Moon: the four Galilean moons, Saturn's Titan, and Neptune's Triton. Saturn has an additional six mid-sized natural satellites massive enough to have achieved hydrostatic equilibrium, and Uranus has five. It has been suggested that some satellites may potentially harbour life.

Among the objects generally agreed by astronomers to be dwarf planets, Ceres and Sedna have no known natural satellites. Pluto has the relatively large natural satellite Charon and four smaller natural satellites; Styx, Nix, Kerberos, and Hydra. Haumea has two natural satellites; Orcus, Quaoar, Makemake, Gonggong, and Eris have one each. The Pluto–Charon system is unusual in that the center of mass lies in open space between the two, a characteristic sometimes associated with a double-planet system.

The seven largest natural satellites in the Solar System (those bigger than 2,500 km across) are Jupiter's Galilean moons (Ganymede, Callisto, Io, and Europa), Saturn's moon Titan, Earth's moon, and Neptune's captured natural satellite Triton. Triton, the smallest of these, has more mass than all smaller natural satellites together. Similarly in the next size group of nine mid-sized natural satellites, between 1,000 km and 1,600 km across, Titania, Oberon, Rhea, Iapetus, Charon, Ariel, Umbriel, Dione, and Tethys, the smallest, Tethys, has more mass than all smaller natural satellites together. As well as the natural satellites of the various planets, there are also over 80 known natural satellites of the dwarf planets, minor planets and other small Solar System bodies. Some studies estimate that up to 15% of all trans-Neptunian objects could have satellites.

The following is a comparative table classifying the natural satellites in the Solar System by diameter. The column on the right includes some notable planets, dwarf planets, asteroids, and trans-Neptunian objects for comparison. The natural satellites of the planets are named after mythological figures. These are predominantly Greek, except for the Uranian natural satellites, which are named after Shakespearean characters. The twenty satellites massive enough to be round are in bold in the table below. Minor planets and satellites where there is disagreement in the literature on roundness are italicized in the table below.

See also

• Circumplanetary disk – Accumulation of matter around a planet
• Co-orbital moon – Configuration of two or more astronomical objectsPages displaying short descriptions of redirect targets
• Exomoon – Moon beyond the Solar System
• Inner moon – Natural satellite orbiting inside the orbit of a larger moon
• Irregular moon – Captured satellite following an irregular orbit
• Regular moon – Satellites that formed around their parent planet
• List of natural satellites
• Naming of moons
• Quasi-satellite – Type of satellite in sync with another orbit
• Subsatellite – A satellite that orbits a natural satellite (aka Submoon)
• Timeline of discovery of Solar System planets and their moons
• Trojan moon – Configuration of two or more astronomical objectsPages displaying short descriptions of redirect targets
• Tug of war (astronomy) – Ratio of gravitational forces on a satellite from the Sun and host planet

Moons of planets

• The Moon, Earth's natural satellite
• Moons of Mars
• Moons of Jupiter
• Moons of Saturn
• Moons of Uranus
• Moons of Neptune

Moons of dwarf planets and small Solar System bodies

• Minor-planet moon
• Moons of Pluto
• Dysnomia, Eris's natural satellite
• Moons of Haumea
• S/2015 (136472) 1, Makemake's natural satellite
• Xiangliu, Gonggong's natural satellite
• Weywot, Quaoar's natural satellite
• Vanth, Orcus' binary natural satellite

References

1. "Planet and Satellite Names and Discoverers". International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). Retrieved 27 January 2012.
2. ^ Wm. Robert Johnston (30 September 2018). "Asteroids with Satellites". Johnston's Archive. Retrieved 22 October 2018.
3. Canup, Robin M.; Ward, William R. (June 2006). "A common mass scaling for satellite systems of gaseous planets". Nature. 441 (7095): 834–839. Bibcode:2006Natur.441..834C. doi:10.1038/nature04860. ISSN 1476-4687. PMID 16778883. S2CID 4327454.
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6. Kenneth R. Lang. "The Cambridge Guide to the Solar System" Archived 4 January 2023 at the Wayback Machine. 2011. p. 15. quote: "Any object that orbits a planet is now called a satellite, and a natural satellite is also now called a moon."
7. Thérèse Encrenaz, et al. "The Solar System". 2004. p. 30.
8. Tilman Spohn, Doris Breuer, Torrence Johnson. "Encyclopedia of the Solar System" Archived 4 January 2023 at the Wayback Machine. 2014. p. 18.
9. David Andrew Weintraub. "Is Pluto a Planet?: A Historical Journey Through the Solar System". p. 65 quote: "... the general concept of a "moon" as a satellite of a planet and "planet" as a satellite of a star."
10. "Satellite". www.merriam-webster.com. Merriam Webster. Retrieved 16 November 2015.
11. Stillman, Dan (16 June 2015). "What Is a Satellite?". www.nasa.gov. NASA. Retrieved 16 November 2015.
12. F. Marchis, et al. (2005). "Discovery of the triple asteroidal system 87 Sylvia". Nature. 436 (7052): 822–824. Bibcode:2005Natur.436..822M. doi:10.1038/nature04018. PMID 16094362. S2CID 4412813.
13. Canup, Robin M.; Ward, William R. (2008). Origin of Europa and the Galilean Satellites. University of Arizona Press. p. 59. arXiv:0812.4995. Bibcode:2009euro.book...59C. ISBN 978-0-8165-2844-8.
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18. Camille M. Carlisle (30 December 2011). "Pseudo-moons Orbit Earth". Sky & Telescope.
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20. "2006 RH120 ( = 6R10DB9) (A second moon for the Earth?)". Great Shefford Observatory. 14 September 2017. Archived from the original on 6 February 2015. Retrieved 13 November 2017.
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23. Northon, Karen (3 June 2015). "NASA's Hubble Finds Pluto's Moons Tumbling in Absolute Chaos". NASA. Retrieved 25 October 2015.
24. Jones, G. H.; et al. (2008). "The Dust Halo of Saturn's Largest Icy Moon, Rhea – Jones et al. 319 (5868): 1380 – Science" (PDF). Science. 319 (5868): 1380–1384. Bibcode:2008Sci...319.1380J. doi:10.1126/science.1151524. PMID 18323452. S2CID 206509814. Archived from the original (PDF) on 8 March 2018.
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27. "How Iapetus, Saturn's outermost moon, got its ridge". 13 December 2010.
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External links

All moons

• Natural Satellite Physical Parameters (JPL-NASA, with refs – last updated July 2006)
• Moons of the Solar System (The Planetary Society, as of March 2009)
• The JPL's Solar System Dynamics page
• "How Many Solar System Bodies". NASA/JPL Solar System Dynamics. Retrieved 26 January 2012.
• Planetary Names: Planet and Satellite Names and Discoverers
• "Upper size limit for moons explained" Kelly Young. Nature (vol 441, p. 834) 14 June 2006
• Images of planets and major moons (not to scale)
• The Planetary Society – Moon Montage(s)
• Album of moon images by Kevin M. Gill
• The Atlas of Moons by the National Geographic Society

Jupiter's moons

• Sheppard, Scott S. "The Jupiter Satellite and Moon Page". Department of Terrestrial Magnetism at Carnegie Institution for Science. Archived from the original on 31 May 2018. Retrieved 8 March 2018.* Scott S. Sheppard
• Scott S. Sheppard

Saturn's moons

• Satellite-hunters find four new moons of the planet Saturn David Brand | 26 October 2000
• Saturn's New Satellite S/2003 S1 Scott S. Sheppard

v t e Natural satellites of the Solar System
v t e Moons of terrestrial planets and asteroids Earth Mars Asteroid moons The Moon Phobos Deimos Binaries List
v t e Moons of Jupiter Listed in increasing approximate distance from Jupiter Inner moons Metis Adrastea Amalthea Thebe Galilean moons Io Europa Ganymede Callisto Themisto Themisto Himalia group (9) Leda Ersa S/2018 J 2 Himalia Pandia Lysithea Elara S/2011 J 3 Dia Carpo group (2) S/2018 J 4 Carpo Valetudo Valetudo Ananke group (26) Euporie Jupiter LV Eupheme S/2021 J 3 Jupiter LII Jupiter LIV Mneme Euanthe S/2003 J 16 Harpalyke Orthosie S/2022 J 3 Helike S/2021 J 2 Praxidike Jupiter LXIV S/2021 J 1 S/2003 J 12 Jupiter LXVIII Thelxinoe Thyone S/2003 J 2 Ananke Iocaste Hermippe Jupiter LXX Carme group (30) S/2022 J 1 S/2022 J 2 S/2016 J 3 Pasithee Jupiter LXIX S/2021 J 6 S/2003 J 24 Chaldene Jupiter LXIII Isonoe S/2021 J 4 Kallichore Erinome Kale Eirene Aitne Eukelade Arche Taygete Jupiter LXXII Carme Herse Jupiter LXI Jupiter LI S/2003 J 9 Jupiter LXVI Kalyke S/2018 J 3 S/2021 J 5 S/2003 J 10 Pasiphae group (18) Philophrosyne Eurydome Jupiter LVI S/2003 J 4 S/2016 J 4 Jupiter LXVII Hegemone Pasiphae Sponde Megaclite Cyllene Sinope Jupiter LIX Aoede Autonoe Callirrhoe S/2003 J 23 Kore See also Rings of Jupiter Jupiter's moons in fiction Category
v t e Moons of Saturn Listed in approximate increasing distance from Saturn Ring moonlets S/2009 S 1 Aegaeon Ring shepherds Pan Daphnis Prometheus Epimetheus Janus Other inner moons Atlas Pandora Alkyonides Methone Anthe Pallene Large moons (with trojans) Mimas Enceladus Tethys Telesto Calypso Dione Helene Polydeuces Rhea Titan Hyperion Iapetus Inuit group (13) Kiviuq subgroup S/2019 S 1 Kiviuq S/2005 S 4 S/2020 S 1 Ijiraq Paaliaq subgroup Paaliaq Siarnaq subgroup S/2004 S 31 Tarqeq S/2019 S 14 Siarnaq S/2020 S 3 S/2019 S 6 S/2020 S 5 Gallic group (7) Albiorix Bebhionn S/2007 S 8 Saturn LX Erriapus Tarvos S/2020 S 4 Norse group (100) Phoebe subgroup Phoebe S/2006 S 20 S/2006 S 9 Skathi S/2007 S 5 S/2007 S 7 S/2007 S 2 S/2004 S 37 S/2004 S 47 S/2004 S 40 S/2019 S 2 S/2019 S 3 S/2020 S 7 Skoll S/2020 S 2 S/2019 S 4 S/2004 S 41 S/2004 S 42 Hyrrokkin Greip S/2004 S 13 S/2007 S 6 Mundilfari S/2006 S 1 S/2004 S 43 S/2006 S 10 S/2019 S 5 Gridr Bergelmir Jarnsaxa Narvi Suttungr S/2004 S 44 S/2007 S 3 S/2004 S 45 Hati S/2004 S 17 S/2006 S 11 S/2004 S 12 Eggther S/2006 S 13 S/2007 S 9 S/2019 S 7 S/2019 S 8 Farbauti Thrymr Bestla S/2019 S 9 S/2004 S 46 Angrboda S/2019 S 11 Aegir S/2019 S 10 Beli S/2019 S 12 Gerd S/2019 S 13 S/2006 S 14 Gunnlod S/2019 S 15 S/2020 S 6 S/2004 S 7 S/2006 S 3 S/2005 S 5 Skrymir S/2006 S 16 S/2006 S 15 S/2004 S 28 S/2020 S 8 Alvaldi Kari S/2004 S 48 Geirrod Fenrir S/2004 S 50 S/2006 S 17 S/2004 S 49 S/2019 S 17 Surtur S/2006 S 18 Loge Ymir S/2019 S 19 S/2019 S 18 S/2004 S 21 S/2004 S 39 S/2019 S 16 S/2004 S 53 S/2004 S 36 Thiazzi S/2019 S 20 S/2006 S 19 Saturn LXIV Fornjot S/2004 S 51 S/2020 S 10 S/2020 S 9 Saturn LVIII S/2019 S 21 S/2004 S 52 Outlier prograde irregular moons S/2006 S 12 S/2004 S 24 Rings of Saturn Cassini–Huygens Chiron Chrysalis Themis S/2004 S 3 S/2004 S 4 S/2004 S 6 Peggy Bleriot In fiction
v t e Moons of Uranus Listed in approximately increasing distance from Uranus Inner Rings of Uranus Cordelia Ophelia Bianca Cressida Desdemona Juliet Portia Rosalind Cupid Belinda Perdita Puck Mab Major (spheroid) Miranda Ariel Umbriel Titania Oberon Outer (irregular) Prograde Margaret Retrograde Francisco Caliban Stephano S/2023 U 1 Trinculo Sycorax Prospero Setebos Ferdinand Geological features Arielian Kachina Chasmata Yangoor Mirandian Verona Rupes Oberonian Hamlet Mommur Chasma Puckian Titanian Gertrude Messina Chasmata Ursula Rousillon Rupes Umbrielian Wunda Vuver Skynd
v t e Moons of Neptune Listed in approximately increasing distance from Neptune Regular (inner) Naiad Thalassa Despina Galatea Larissa Hippocamp Proteus Irregular Triton Triton atmosphere climate geology Prograde Nereid Sao S/2002 N 5 Laomedeia Retrograde Halimede Psamathe Neso S/2021 N 1 See also Neptune trojans Rings of Neptune Category Portal
v t e Moons of likely dwarf planets Pluto Haumea Eris Makemake Gonggong Charon Styx Nix Kerberos Hydra ring Namaka Hiʻiaka Dysnomia S/2015 (136472) 1 Xiangliu Quaoar Orcus Salacia Varda 2013 FY27 rings Weywot Vanth Actaea Ilmarë 2013 FY27 I
v t e Natural satellites of the Solar System Planetary satellites of Earth Mars Jupiter Saturn Uranus Neptune Dwarf planet satellites of Orcus Pluto Haumea Quaoar Makemake Gonggong Eris Minor-planet moons Near-Earth Florence Didymos Dimorphos Moshup Squannit 1994 CC 2001 SN263 Main belt Kalliope Linus Euphrosyne Daphne Peneius Eugenia Petit-Prince Sylvia Romulus Remus Minerva Aegis Gorgoneion Camilla Elektra Kleopatra Alexhelios Cleoselene Ida Dactyl Roxane Olympias Pulcova Balam Dinkinesh (Selam) Jupiter trojans Patroclus Menoetius Hektor Skamandrios Eurybates Queta TNOs Lempo Hiisi Paha 2002 UX25 Sila–Nunam Salacia Actaea Varda Ilmarë Gǃkúnǁʼhòmdímà Gǃòʼé ǃHú 2013 FY27 Ranked by size Ganymede largest: 5268 km / 0.413 Earths Titan Callisto Io Moon Europa Triton Titania Rhea Oberon Iapetus Charon Umbriel Ariel Dione Tethys Dysnomia Enceladus Miranda Vanth Proteus Mimas Ilmarë Nereid Hiʻiaka Actaea Hyperion Phoebe ... Discovery timeline Inner moons Irregular moons List Planetary-mass moons Naming Subsatellite Regular moons Trojan moons
Discovery timeline Inner moons Irregular moons List Naming Subsatellite Regular moons Trojan moons

v t e Solar System
Sun Mercury Venus Earth Mars Ceres Jupiter Saturn Uranus Neptune Orcus Pluto Haumea Quaoar Makemake Gonggong Eris Sedna
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