Moons of Jupiter facts for kids

A montage of Jupiter and its four largest moons (distance and sizes not to scale)

There are 95 moons of Jupiter with confirmed orbits as of 5 February  2024 (2024 -02-05)^[update]. This number does not include a number of meter-sized moonlets thought to be shed from the inner moons, nor hundreds of possible kilometer-sized outer irregular moons that were only briefly captured by telescopes. All together, Jupiter's moons form a satellite system called the Jovian system. The most massive of the moons are the four Galilean moons: Io, Europa, Ganymede, and Callisto, which were independently discovered in 1610 by Galileo Galilei and Simon Marius and were the first objects found to orbit a body that was neither Earth nor the Sun. Much more recently, beginning in 1892, dozens of far smaller Jovian moons have been detected and have received the names of lovers or daughters of the Roman god Jupiter or his Greek equivalent Zeus. The Galilean moons are by far the largest and most massive objects to orbit Jupiter, with the remaining 91 known moons and the rings together composing just 0.003% of the total orbiting mass.

Of Jupiter's moons, eight are regular satellites with prograde and nearly circular orbits that are not greatly inclined with respect to Jupiter's equatorial plane. The Galilean satellites are nearly spherical in shape due to their planetary mass, and are just massive enough that they would be considered major planets if they were in direct orbit around the Sun. The other four regular satellites, known as the inner moons, are much smaller and closer to Jupiter; these serve as sources of the dust that makes up Jupiter's rings. The remainder of Jupiter's moons are outer irregular satellites whose prograde and retrograde orbits are much farther from Jupiter and have high inclinations and eccentricities. The largest of these moons were likely asteroids that were captured from solar orbits by Jupiter before impacts with other small bodies shattered them into many kilometer-sized fragments, forming collisional families of moons sharing similar orbits. Jupiter is expected to have about 100 irregular moons larger than 1 km (0.6 mi) in diameter, plus around 500 more smaller retrograde moons down to diameters of 0.8 km (0.5 mi). Of the 87 known irregular moons of Jupiter, 38 of them have not yet been officially named.

Characteristics

The Galilean moons. From left to right, in order of increasing distance from Jupiter: Io; Europa; Ganymede; Callisto.

The physical and orbital characteristics of the moons vary widely. The four Galileans are all over 3,100 kilometres (1,900 mi) in diameter; the largest Galilean, Ganymede, is the ninth largest object in the Solar System, after the Sun and seven of the planets, Ganymede being larger than Mercury. All other Jovian moons are less than 250 kilometres (160 mi) in diameter, with most barely exceeding 5 kilometres (3.1 mi). Their orbital shapes range from nearly perfectly circular to highly eccentric and inclined, and many revolve in the direction opposite to Jupiter's rotation (retrograde motion). Orbital periods range from seven hours (taking less time than Jupiter does to rotate around its axis), to almost three Earth years.

Origin and evolution

The relative masses of the Jovian moons. Those smaller than Europa are not visible at this scale, and combined would only be visible at 100× magnification.

Jupiter's regular satellites are believed to have formed from a circumplanetary disk, a ring of accreting gas and solid debris analogous to a protoplanetary disk. They may be the remnants of a score of Galilean-mass satellites that formed early in Jupiter's history.

Simulations suggest that, while the disk had a relatively high mass at any given moment, over time a substantial fraction (several tens of a percent) of the mass of Jupiter captured from the solar nebula was passed through it. However, only 2% of the proto-disk mass of Jupiter is required to explain the existing satellites. Thus, several generations of Galilean-mass satellites may have been in Jupiter's early history. Each generation of moons might have spiraled into Jupiter, because of drag from the disk, with new moons then forming from the new debris captured from the solar nebula. By the time the present (possibly fifth) generation formed, the disk had thinned so that it no longer greatly interfered with the moons' orbits. The current Galilean moons were still affected, falling into and being partially protected by an orbital resonance with each other, which still exists for Io, Europa, and Ganymede: they are in a 1:2:4 resonance. Ganymede's larger mass means that it would have migrated inward at a faster rate than Europa or Io. Tidal dissipation in the Jovian system is still ongoing and Callisto will likely be captured into the resonance in about 1.5 billion years, creating a 1:2:4:8 chain.

The outer, irregular moons are thought to have originated from captured asteroids, whereas the protolunar disk was still massive enough to absorb much of their momentum and thus capture them into orbit. Many are believed to have been broken up by mechanical stresses during capture, or afterward by collisions with other small bodies, producing the moons we see today.

History and discovery

Visual observations

Jupiter and the Galilean moons as seen through a 25 cm (10 in) Meade LX200 telescope

Chinese historian Xi Zezong claimed that the earliest record of a Jovian moon (Ganymede or Callisto) was a note by Chinese astronomer Gan De of an observation around 364 BC regarding a "reddish star". However, the first certain observations of Jupiter's satellites were those of Galileo Galilei in 1609. By January 1610, he had sighted the four massive Galilean moons with his 20× magnification telescope, and he published his results in March 1610.

Simon Marius had independently discovered the moons one day after Galileo, although he did not publish his book on the subject until 1614. Even so, the names Marius assigned are used today: Ganymede, Callisto, Io, and Europa. No additional satellites were discovered until E. E. Barnard observed Amalthea in 1892.

Photographic and spacecraft observations

Voyager 1 discovery image of the inner moon Metis on 4 March 1979, showing the moon's tiny silhouette against the backdrop of Jupiter's clouds

With the aid of telescopic photography with photographic plates, further discoveries followed quickly over the course of the 20th century. Himalia was discovered in 1904, Elara in 1905, Pasiphae in 1908, Sinope in 1914, Lysithea and Carme in 1938, Ananke in 1951, and Leda in 1974.

By the time that the Voyager space probes reached Jupiter, around 1979, thirteen moons had been discovered, not including Themisto, which had been observed in 1975, but was lost until 2000 due to insufficient initial observation data. The Voyager spacecraft discovered an additional three inner moons in 1979: Metis, Adrastea, and Thebe.

Digital telescopic observations

No additional moons were discovered until two decades later, with the fortuitous discovery of Callirrhoe by the Spacewatch survey in October 1999. During the 1990s, photographic plates phased out as digital charge-coupled device (CCD) cameras began emerging in telescopes on Earth, allowing for wide-field surveys of the sky at unprecedented sensitivities and ushering in a wave of new moon discoveries. Scott Sheppard, then a graduate student of David Jewitt, demonstrated this extended capability of CCD cameras in a survey conducted with the Mauna Kea Observatory's 2.2-meter (88 in) UH88 telescope in November 2000, discovering eleven new irregular moons of Jupiter including the previously lost Themisto with the aid of automated computer algorithms.

From 2001 onward, Sheppard and Jewitt alongside other collaborators continued surveying for Jovian irregular moons with the 3.6-meter (12 ft) Canada-France-Hawaii Telescope (CFHT), discovering an additional eleven in December 2001, one in October 2002, and nineteen in February 2003. At the same time, another independent team led by Brett J. Gladman also used the CFHT in 2003 to search for Jovian irregular moons, discovering four and co-discovering two with Sheppard. From the start to end of these CCD-based surveys in 2000–2004, Jupiter's known moon count had grown from 17 to 63. All of these moons discovered after 2000 are faint and tiny, with apparent magnitudes between 22–23 and diameters less than 10 km (6.2 mi). As a result, many could not be reliably tracked and ended up becoming lost.

Beginning in 2009, a team of astronomers, namely Mike Alexandersen, Marina Brozović, Brett Gladman, Robert Jacobson, and Christian Veillet, began a campaign to recover Jupiter's lost irregular moons using the CFHT and Palomar Observatory's 5.1-meter (17 ft) Hale Telescope. They discovered two previously unknown Jovian irregular moons during recovery efforts in September 2010, prompting further follow-up observations to confirm these by 2011. One of these moons, S/2010 J 2 (now Jupiter LII), has an apparent magnitude of 24 and a diameter of only 1–2 km (0.62–1.2 mi), making it one of the faintest and smallest confirmed moons of Jupiter even as of 2023^[update]. Meanwhile, in September 2011, Scott Sheppard, now a faculty member of the Carnegie Institution for Science, discovered two more irregular moons using the institution's 6.5-meter (21 ft) Magellan Telescopes at Las Campanas Observatory, raising Jupiter's known moon count to 67. Although Sheppard's two moons were followed up and confirmed by 2012, both became lost due to insufficient observational coverage.

In 2016, while surveying for distant trans-Neptunian objects with the Magellan Telescopes, Sheppard serendipitously observed a region of the sky located near Jupiter, enticing him to search for Jovian irregular moons as a detour. In collaboration with Chadwick Trujillo and David Tholen, Sheppard continued surveying around Jupiter from 2016 to 2018 using the Cerro Tololo Observatory's 4.0-meter (13 ft) Víctor M. Blanco Telescope and Mauna Kea Observatory's 8.2-meter (27 ft) Subaru Telescope. In the process, Sheppard's team recovered several lost moons of Jupiter from 2003 to 2011 and reported two new Jovian irregular moons in June 2017. Then in July 2018, Sheppard's team announced ten more irregular moons confirmed from 2016 to 2018 observations, bringing Jupiter's known moon count to 79. Among these was Valetudo, which has an unusually distant prograde orbit that crosses paths with the retrograde irregular moons. Several more unidentified Jovian irregular satellites were detected in Sheppard's 2016–2018 search, but were too faint for follow-up confirmation.

From November 2021 to January 2023, Sheppard discovered twelve more irregular moons of Jupiter and confirmed them in archival survey imagery from 2003 to 2018, bringing the total count to 92. Among these was S/2018 J 4, a highly-inclined prograde moon that is now known to be in same orbital grouping as the moon Carpo, which was previously thought to be solitary. On 22 February 2023, Sheppard announced three more moons discovered in a 2022 survey, now bringing Jupiter's total known moon count to 95. In a February 2023 interview with NPR, Sheppard noted that he and his team are currently tracking even more moons of Jupiter, which should place Jupiter's moon count over 100 once confirmed over the next two years.

Many more irregular moons of Jupiter will inevitably be discovered in the future, especially after the beginning of deep sky surveys by the upcoming Vera C. Rubin Observatory and Nancy Grace Roman Space Telescope in the mid-2020s. The Rubin Observatory's 8.4-meter (28 ft) aperture telescope and 3.5 square-degree field of view will probe Jupiter's irregular moons down to diameters of 1 km (0.6 mi) at apparent magnitudes of 24.5, with the potential of increasing the known population by up to tenfold. Likewise, the Roman Space Telescope's 2.4-meter (7.9 ft) aperture and 0.28 square-degree field of view will probe Jupiter's irregular moons down to diameters of 0.3 km (0.2 mi) at magnitude 27.7, with the potential of discovering approximately 1,000 Jovian moons above this size. Discovering these many irregular satellites will help reveal their population's size distribution and collisional histories, which will place further constraints to how the Solar System formed. Discovery of outer planet moons

     Moons of Jupiter      Moons of Saturn      Moons of Uranus      Moons of Neptune

Naming

Galilean moons around Jupiter       Jupiter ·       Io ·       Europa ·       Ganymede ·       Callisto

Orbits of Jupiter's inner moons within its rings

The Galilean moons of Jupiter (Io, Europa, Ganymede, and Callisto) were named by Simon Marius soon after their discovery in 1610. However, these names fell out of favor until the 20th century. The astronomical literature instead simply referred to "Jupiter I", "Jupiter II", etc., or "the first satellite of Jupiter", "Jupiter's second satellite", and so on. The names Io, Europa, Ganymede, and Callisto became popular in the mid-20th century, whereas the rest of the moons remained unnamed and were usually numbered in Roman numerals V (5) to XII (12). Jupiter V was discovered in 1892 and given the name Amalthea by a popular though unofficial convention, a name first used by French astronomer Camille Flammarion.

The other moons were simply labeled by their Roman numeral (e.g. Jupiter IX) in the majority of astronomical literature until the 1970s. Several different suggestions were made for names of Jupiter's outer satellites, but none were universally accepted until 1975 when the International Astronomical Union's (IAU) Task Group for Outer Solar System Nomenclature granted names to satellites V–XIII, and provided for a formal naming process for future satellites still to be discovered. The practice was to name newly discovered moons of Jupiter after lovers and favorites of the god Jupiter (Zeus) and, since 2004, also after their descendants. All of Jupiter's satellites from XXXIV (Euporie) onward are named after descendants of Jupiter or Zeus, except LIII (Dia), named after a lover of Jupiter. Names ending with "a" or "o" are used for prograde irregular satellites (the latter for highly inclined satellites), and names ending with "e" are used for retrograde irregulars. With the discovery of smaller, kilometre-sized moons around Jupiter, the IAU has established an additional convention to limit the naming of small moons with absolute magnitudes greater than 18 or diameters smaller than 1 km (0.6 mi). Some of the most recently confirmed moons have not received names.

Some asteroids share the same names as moons of Jupiter: 9 Metis, 38 Leda, 52 Europa, 85 Io, 113 Amalthea, 239 Adrastea. Two more asteroids previously shared the names of Jovian moons until spelling differences were made permanent by the IAU: Ganymede and asteroid 1036 Ganymed; and Callisto and asteroid 204 Kallisto.

Groups

Regular satellites

These have prograde and nearly circular orbits of low inclination and are split into two groups:

• Inner satellites or Amalthea group: Metis, Adrastea, Amalthea, and Thebe. These orbit very close to Jupiter; the innermost two orbit in less than a Jovian day. The latter two are respectively the fifth and seventh largest moons in the Jovian system. Observations suggest that at least the largest member, Amalthea, did not form on its present orbit, but farther from the planet, or that it is a captured Solar System body. These moons, along with a number of seen and as-yet-unseen inner moonlets (see Amalthea moonlets), replenish and maintain Jupiter's faint ring system. Metis and Adrastea help to maintain Jupiter's main ring, whereas Amalthea and Thebe each maintain their own faint outer rings.
• Main group or Galilean moons: Io, Europa, Ganymede and Callisto. They are some of the largest objects in the Solar System outside the Sun and the eight planets in terms of mass, larger than any known dwarf planet. Ganymede exceeds (and Callisto nearly equals) even the planet Mercury in diameter, though they are less massive. They are respectively the fourth-, sixth-, first-, and third-largest natural satellites in the Solar System, containing approximately 99.997% of the total mass in orbit around Jupiter, while Jupiter is almost 5,000 times more massive than the Galilean moons. The inner moons are in a 1:2:4 orbital resonance. Models suggest that they formed by slow accretion in the low-density Jovian subnebula—a disc of the gas and dust that existed around Jupiter after its formation—which lasted up to 10 million years in the case of Callisto. Europa, Ganymede, and Callisto are suspected of having subsurface water oceans, and Io may have a subsurface magma ocean.

Irregular satellites

Orbits and positions of Jupiter's irregular satellites as of 1 January 2021. Prograde orbits are colored blue while retrograde orbits are colored red.

The irregular satellites are substantially smaller objects with more distant and eccentric orbits. They form families with shared similarities in orbit (semi-major axis, inclination, eccentricity) and composition; it is believed that these are at least partially collisional families that were created when larger (but still small) parent bodies were shattered by impacts from asteroids captured by Jupiter's gravitational field. These families bear the names of their largest members. The identification of satellite families is tentative, but the following are typically listed:

• Prograde satellites:
  • Themisto is the innermost irregular moon and is not part of a known family.
  • The Himalia group is confined within semi-major axes between 11–12 million km (6.8–7.5 million mi), inclinations between 27–29°, and eccentricities between 0.12 and 0.21. It has been suggested that the group could be a remnant of the break-up of an asteroid from the asteroid belt. The largest two members, Himalia and Elara, are respectively the sixth- and eighth-largest Jovian moons.
  • The Carpo group includes two known moons on very high orbital inclinations of 50° and semi-major axes between 16–17 million km (9.9–10.6 million mi). Due to their exceptionally high inclinations, the moons of the Carpo group are subject to gravitational perturbations that induce the Lidov–Kozai resonance in their orbits, which cause their eccentricities and inclinations to periodically oscillate in correspondence with each other. The Lidov–Kozai resonance can significantly alter the orbits of these moons: for example, the eccentricity and inclination of the group's namesake Carpo can fluctuate between 0.19–0.69 and 44–59°, respectively.
  • Valetudo is the outermost prograde moon and is not part of a known family. Its prograde orbit crosses paths with several moons that have retrograde orbits and may in the future collide with them.

• Retrograde satellites:
  • The Carme group is tightly confined within semi-major axes between 22–24 million km (14–15 million mi), inclinations between 164–166°, and eccentricities between 0.25 and 0.28. It is very homogeneous in color (light red) and is believed to have originated as collisional fragments from a D-type asteroid progenitor, possibly a Jupiter trojan.
  • The Ananke group has a relatively wider spread than the previous groups, with semi-major axes between 19–22 million km (12–14 million mi), inclinations between 144–156°, and eccentricities between 0.09 and 0.25. Most of the members appear gray, and are believed to have formed from the breakup of a captured asteroid.
  • The Pasiphae group is quite dispersed, with semi-major axes spread over 22–25 million km (14–16 million mi), inclinations between 141° and 157°, and higher eccentricities between 0.23 and 0.44. The colors also vary significantly, from red to grey, which might be the result of multiple collisions. Sinope, sometimes included in the Pasiphae group, is red and, given the difference in inclination, it could have been captured independently; Pasiphae and Sinope are also trapped in secular resonances with Jupiter.

Based on their survey discoveries in 2000–2003, Sheppard and Jewitt predicted that Jupiter should have approximately 100 irregular satellites larger than 1 km (0.6 mi) in diameter, or brighter than magnitude 24. Survey observations by Alexandersen et al. in 2010–2011 agreed with this prediction, estimating that approximately 40 Jovian irregular satellites of this size remained undiscovered in 2012.

In September 2020, researchers from the University of British Columbia identified 45 candidate irregular moons from an analysis of archival images taken in 2010 by the CFHT. These candidates were mainly small and faint, down to magnitude of 25.7 or above 0.8 km (0.5 mi) in diameter. From the number of candidate moons detected within a sky area of one square degree, the team extrapolated that the population of retrograde Jovian moons brighter than magnitude 25.7 is around 600+600
−300 within a factor of 2. Although the team considers their characterized candidates to be likely moons of Jupiter, they all remain unconfirmed due to insufficient observation data for determining reliable orbits. The true population of Jovian irregular moons is likely complete down to magnitude 23.2 at diameters over 3 km (1.9 mi) as of 2020^[update].

List

Orbital diagram of the orbital inclination and orbital distances for Jupiter's rings and moon system at various scales. Notable moons, moon groups, and rings are individually labeled. Open the image for full resolution.

The moons of Jupiter are listed below by orbital period. Moons massive enough for their surfaces to have collapsed into a spheroid are highlighted in bold. These are the four Galilean moons, which are comparable in size to the Moon. The other moons are much smaller. The Galilean moon with the smallest amount of mass is greater than 7,000 times more massive than the most massive of the other moons. The irregular captured moons are shaded light gray and orange when prograde and yellow, red, and dark gray when retrograde.

The orbits and mean distances of the irregular moons are highly variable over short timescales due to frequent planetary and solar perturbations, so proper orbital elements which are averaged over a period of time are preferably used. The proper orbital elements of the irregular moons listed here are averaged over a 400-year numerical integration by the Jet Propulsion Laboratory: for the above reasons, they may strongly differ from osculating orbital elements provided by other sources. Otherwise, recently-discovered irregular moons without published proper elements are temporarily listed here with inaccurate osculating orbital elements that are italicized to distinguish them from other irregular moons with proper orbital elements. Some of the irregular moons' proper orbital periods in this list may not scale accordingly with their proper semi-major axes due to the aforementioned perturbations. The irregular moons' proper orbital elements are all based on the reference epoch of 1 January 2000.

Some irregular moons have only been observed briefly for a year or two, but their orbits are known accurately enough that they will not be lost to positional uncertainties.

Label	Name	Pronunciation	Image	Abs. magn.	Diameter (km)	Mass (×1016 kg)	Semi-major axis (km)	Orbital period (d)	Inclination (°)	Eccentricity	Discovery year	Year announced	Discoverer	Group
16 XVI	Metis	/ˈmiːtəs/		10.5	43 (60 × 40 × 34)	3.6 ≈ 3.6	128000	0.2948 +0.2948 (+7h 04m 29s)	0.060	0.0002	1979	1980	Synnott (Voyager 1)	Inner
15 XV	Adrastea	/ædrəˈstiːə/		12.0	16.4 16.4 (20 × 16 × 14)	0.20 ≈ 0.20	129000	0.2983 +0.2983 (+7h 09m 30s)	0.030	0.0015	1979	1979	Jewitt (Voyager 2)	Inner
05 V	Amalthea	/æməlˈθiːə/		7.1	167 167 (250 × 146 × 128)	208	181400	0.4999 +0.4999 (+11h 59m 53s)	0.374	0.0032	1892	1892	Barnard	Inner
14 XIV	Thebe	/ˈθiːbiː/		9.0	98.6 98.6 (116 × 98 × 84)	43 ≈ 43	221900	0.6761 +0.6761 (+16h 13m 35s)	1.076	0.0175	1979	1980	Synnott (Voyager 1)	Inner
01 I	Io♠	/ˈaɪoʊ/		-1.7	3643.2 (3660 × 3637 × 3631)	8931900	421800	1.7627 +1.7627 (+1d 18h 18m 20s)	0.050	0.0041	1610	1610	Galileo	Galilean
02 II	Europa♠	/jʊəˈroʊpə/		-1.4	3121.6	4799800	671100	3.5255 +3.5255 (+3d 12h 36m 40s)	0.470	0.0090	1610	1610	Galileo	Galilean
03 III	Ganymede♠	/ˈɡænəmiːd/		-2.1	5268.2	14819000	1070400	7.1556 +7.1556	0.200	0.0013	1610	1610	Galileo	Galilean
04 IV	Callisto♠	/kəˈlɪstoʊ/		-1.2	4820.6	10759000	1882700	016.690 +16.690	0.192	0.0074	1610	1610	Galileo	Galilean
18 XVIII	Themisto†	/θəˈmɪstoʊ/		13.3	9 ≈ 9	0.038 ≈ 0.038	7398500	130.03 +130.03	43.8	0.340	1975/2000	1975	Kowal & Roemer/ Sheppard et al.	Themisto
13 XIII	Leda♣	/ˈliːdə/		12.7	21.5	0.52 ≈ 0.52	11146400	240.93 +240.93	28.6	0.162	1974	1974	Kowal	Himalia
71 LXXI	Ersa♣	/ˈɜːrsə/		16.0	3 ≈ 3	0.0014 ≈ 0.0014	11401000	249.23 +249.23	29.1	0.116	2018	2018	Sheppard	Himalia
L	S/2018 J 2♣			16.5	3 ≈ 3	0.0014 ≈ 0.0014	11419700	249.92 +249.92	28.3	0.152	2018	2022	Sheppard	Himalia
06 VI	Himalia♣	/hɪˈmeɪliə/		8.0	139.6 (150 × 120)	420	11440600	250.56 +250.56	28.1	0.160	1904	1905	Perrine	Himalia
65 LXV	Pandia♣	/pænˈdaɪə/		16.2	3 ≈ 3	0.0014 ≈ 0.0014	11481000	251.91 +251.91	29.0	0.179	2017	2018	Sheppard	Himalia
10 X	Lysithea♣	/laɪˈsɪθiə/		11.2	42.2	3.9 ≈ 3.9	11700800	259.20 +259.20	27.2	0.117	1938	1938	Nicholson	Himalia
07 VII	Elara♣	/ˈɛlərə/		9.7	79.9	27 ≈ 27	11712300	259.64 +259.64	27.9	0.211	1905	1905	Perrine	Himalia
I	S/2011 J 3♣			16.3	3 ≈ 3	0.0014 ≈ 0.0014	11716800	259.84 +259.84	27.6	0.192	2011	2022	Sheppard	Himalia
53 LIII	Dia♣	/ˈdaɪə/		16.1	4 ≈ 4	0.0034 ≈ 0.0034	12260300	278.21 +278.21	29.0	0.232	2000	2001	Sheppard et al.	Himalia
N	S/2018 J 4§			16.7	2 ≈ 2	0.00042 ≈ 0.00042	16328500	427.63 +427.63	50.2	0.177	2018	2023	Sheppard	Carpo
46 XLVI	Carpo§	/ˈkɑːrpoʊ/		16.2	3 ≈ 3	0.0014 ≈ 0.0014	17042300	456.29 +456.29	53.2	0.416	2003	2003	Sheppard	Carpo
62 LXII	Valetudo±	/væləˈtjuːdoʊ/		17.0	1 ≈ 1	0.000052 ≈ 0.000052	18694200	527.61 +527.61	34.5	0.217	2016	2018	Sheppard	Valetudo
34 XXXIV	Euporie♦	/ˈjuːpəriː/		16.3	2 ≈ 2	0.00042 ≈ 0.00042	19265800	550.69 −550.69	145.7	0.148	2001	2002	Sheppard et al.	Ananke
55 LV	S/2003 J 18♦			16.4	2 ≈ 2	0.00042 ≈ 0.00042	20336300	598.12 −598.12	145.3	0.090	2003	2003	Gladman	Ananke
60 LX	Eupheme♦	/juːˈfiːmiː/		16.6	2 ≈ 2	0.00042 ≈ 0.00042	20768600	617.73 −617.73	148.0	0.241	2003	2003	Sheppard	Ananke
Q	S/2021 J 3♦			17.2	2 ≈ 2	0.00042 ≈ 0.00042	20776700	618.33 −618.33	147.9	0.239	2021	2023	Sheppard	Ananke
52 LII	S/2010 J 2♦			17.4	1 ≈ 1	0.000052 ≈ 0.000052	20793000	618.84 −618.84	148.1	0.248	2010	2011	Veillet	Ananke
54 LIV	S/2016 J 1♦			17.0	1 ≈ 1	0.000052 ≈ 0.000052	20802600	618.49 −618.49	144.7	0.232	2016	2017	Sheppard	Ananke
40 XL	Mneme♦	/ˈniːmiː/		16.3	2 ≈ 2	0.00042 ≈ 0.00042	20821000	620.07 −620.07	148.0	0.247	2003	2003	Sheppard & Gladman	Ananke
33 XXXIII	Euanthe♦	/juːˈænθiː/		16.4	3 ≈ 3	0.0014 ≈ 0.0014	20827000	620.44 −620.44	148.0	0.239	2001	2002	Sheppard et al.	Ananke
F	S/2003 J 16♦			16.3	2 ≈ 2	0.00042 ≈ 0.00042	20882600	622.88 −622.88	148.0	0.243	2003	2003	Gladman	Ananke
22 XXII	Harpalyke♦	/hɑːrˈpæləkiː/		15.9	4 ≈ 4	0.0034 ≈ 0.0034	20892100	623.32 −623.32	147.7	0.232	2000	2001	Sheppard et al.	Ananke
35 XXXV	Orthosie♦	/ɔːrˈθoʊziː/		16.6	2 ≈ 2	0.00042 ≈ 0.00042	20901000	622.59 −622.59	144.3	0.299	2001	2002	Sheppard et al.	Ananke
45 XLV	Helike♦	/ˈhɛləkiː/		16.0	4 ≈ 4	0.0034 ≈ 0.0034	20915700	626.33 −626.33	154.4	0.153	2003	2003	Sheppard	Ananke
P	S/2021 J 2♦			17.3	1 ≈ 1	0.000052 ≈ 0.000052	20926600	625.14 −625.14	148.1	0.242	2021	2023	Sheppard	Ananke
27 XXVII	Praxidike♦	/prækˈsɪdəkiː/		14.9	7	0.018 ≈ 0.018	20935400	625.39 −625.39	148.3	0.246	2000	2001	Sheppard et al.	Ananke
64 LXIV	S/2017 J 3♦			16.5	2 ≈ 2	0.00042 ≈ 0.00042	20941000	625.60 −625.60	147.9	0.231	2017	2018	Sheppard	Ananke
O	S/2021 J 1♦			17.3	1 ≈ 1	0.000052 ≈ 0.000052	20954700	627.14 −627.14	150.5	0.228	2021	2023	Sheppard	Ananke
E	S/2003 J 12♦			17.0	1 ≈ 1	0.000052 ≈ 0.000052	20963100	627.24 −627.24	150.0	0.235	2003	2003	Sheppard	Ananke
68 LXVIII	S/2017 J 7♦			16.6	2 ≈ 2	0.00042 ≈ 0.00042	20964800	626.56 −626.56	147.3	0.233	2017	2018	Sheppard	Ananke
42 XLII	Thelxinoe♦	/θɛlkˈsɪnoʊiː/		16.3	2 ≈ 2	0.00042 ≈ 0.00042	20976000	628.03 −628.03	150.6	0.228	2003	2004	Sheppard & Gladman et al.	Ananke
29 XXIX	Thyone♦	/θaɪˈoʊniː/		15.8	4 ≈ 4	0.0034 ≈ 0.0034	20978000	627.18 −627.18	147.5	0.233	2001	2002	Sheppard et al.	Ananke
A	S/2003 J 2♦			16.7	2 ≈ 2	0.00042 ≈ 0.00042	20997700	628.79 −628.79	150.2	0.225	2003	2003	Sheppard	Ananke
12 XII	Ananke♦	/əˈnæŋkiː/		11.7	29.1	1.3 ≈ 1.3	21034500	629.79 −629.79	147.6	0.237	1951	1951	Nicholson	Ananke
W	S/2022 J 3♦			17.4	1 ≈ 1	0.000052 ≈ 0.000052	21047700	630.67 −630.67	148.2	0.249	2022	2023	Sheppard	Ananke
24 XXIV	Iocaste♦	/aɪəˈkæstiː/		15.5	5 ≈ 5	0.0065 ≈ 0.0065	21066700	631.59 −631.59	148.8	0.227	2000	2001	Sheppard et al.	Ananke
30 XXX	Hermippe♦	/hərˈmɪpiː/		15.5	4 ≈ 4	0.0034 ≈ 0.0034	21108500	633.90 −633.90	150.2	0.219	2001	2002	Sheppard et al.	Ananke
70 LXX	S/2017 J 9♦			16.2	3 ≈ 3	0.0014 ≈ 0.0014	21768700	666.11 −666.11	155.5	0.200	2017	2018	Sheppard	Ananke
58 LVIII	Philophrosyne‡	/fɪləˈfrɒzəniː/		16.7	2 ≈ 2	0.00042 ≈ 0.00042	22604600	702.54 −702.54	146.3	0.229	2003	2003	Sheppard	Pasiphae
J	S/2016 J 3♥			16.7	2 ≈ 2	0.00042 ≈ 0.00042	22719300	713.64 −713.64	164.6	0.251	2016	2023	Sheppard	Carme
U	S/2022 J 1♥			17.0	1 ≈ 1	0.000052 ≈ 0.000052	22725200	738.33 −738.33	164.5	0.257	2022	2023	Sheppard	Carme
38 XXXVIII	Pasithee♥	/ˈpæsəθiː/		16.8	2 ≈ 2	0.00042 ≈ 0.00042	22846700	719.47 −719.47	164.6	0.270	2001	2002	Sheppard et al.	Carme
69 LXIX	S/2017 J 8♥			17.1	1 ≈ 1	0.000052 ≈ 0.000052	22849500	719.76 −719.76	164.8	0.255	2017	2018	Sheppard	Carme
T	S/2021 J 6♥			17.3	1 ≈ 1	0.000052 ≈ 0.000052	22870300	720.97 −720.97	164.9	0.271	2021	2023	Sheppard et al.	Carme
H	S/2003 J 24♥			16.6	2 ≈ 2	0.00042 ≈ 0.00042	22887400	721.60 −721.60	164.5	0.259	2003	2021	Sheppard et al.	Carme
32 XXXII	Eurydome‡	/jʊəˈrɪdəmiː/		16.2	3 ≈ 3	0.0014 ≈ 0.0014	22899000	717.31 −717.31	149.1	0.294	2001	2002	Sheppard et al.	Pasiphae
56 LVI	S/2011 J 2‡			16.8	1 ≈ 1	0.000052 ≈ 0.000052	22909200	718.32 −718.32	151.9	0.355	2011	2012	Sheppard	Pasiphae
B	S/2003 J 4‡			16.7	2 ≈ 2	0.00042 ≈ 0.00042	22926500	718.10 −718.10	148.2	0.328	2003	2003	Sheppard	Pasiphae
21 XXI	Chaldene♥	/kælˈdiːniː/		16.0	4 ≈ 4	0.0034 ≈ 0.0034	22930500	723.71 −723.71	164.7	0.265	2000	2001	Sheppard et al.	Carme
63 LXIII	S/2017 J 2♥			16.4	2 ≈ 2	0.00042 ≈ 0.00042	22953200	724.71 −724.71	164.5	0.272	2017	2018	Sheppard	Carme
26 XXVI	Isonoe♥	/aɪˈsɒnoʊiː/		16.0	4 ≈ 4	0.0034 ≈ 0.0034	22981300	726.27 −726.27	164.8	0.249	2000	2001	Sheppard et al.	Carme
V	S/2022 J 2♥			17.6	1 ≈ 1	0.000052 ≈ 0.000052	23013800	781.56 −781.56	164.7	0.265	2022	2023	Sheppard	Carme
R	S/2021 J 4♥			17.4	1 ≈ 1	0.000052 ≈ 0.000052	23019700	728.28 −728.28	164.6	0.265	2021	2023	Sheppard	Carme
44 XLIV	Kallichore♥	/kəˈlɪkəriː/		16.3	2 ≈ 2	0.00042 ≈ 0.00042	23021800	728.26 −728.26	164.8	0.252	2003	2003	Sheppard	Carme
25 XXV	Erinome♥	/ɛˈrɪnəmiː/		16.0	3 ≈ 3	0.0014 ≈ 0.0014	23032900	728.48 −728.48	164.4	0.276	2000	2001	Sheppard et al.	Carme
37 XXXVII	Kale♥	/ˈkeɪliː/		16.3	2 ≈ 2	0.00042 ≈ 0.00042	23052600	729.64 −729.64	164.6	0.262	2001	2002	Sheppard et al.	Carme
57 LVII	Eirene♥	/aɪˈriːniː/		15.8	4 ≈ 4	0.0034 ≈ 0.0034	23055800	729.84 −729.84	164.6	0.258	2003	2003	Sheppard	Carme
31 XXXI	Aitne♥	/ˈeɪtniː/		16.0	3 ≈ 3	0.0014 ≈ 0.0014	23064400	730.10 −730.10	164.6	0.277	2001	2002	Sheppard et al.	Carme
47 XLVII	Eukelade♥	/juːˈkɛlədiː/		16.0	4 ≈ 4	0.0034 ≈ 0.0034	23067400	730.30 −730.30	164.6	0.277	2003	2003	Sheppard	Carme
43 XLIII	Arche♥	/ˈɑːrkiː/		16.2	3 ≈ 3	0.0014 ≈ 0.0014	23097800	731.88 −731.88	164.6	0.261	2002	2002	Sheppard	Carme
20 XX	Taygete♥	/teɪˈɪdʒətiː/		15.6	5 ≈ 5	0.0065 ≈ 0.0065	23108000	732.45 −732.45	164.7	0.253	2000	2001	Sheppard et al.	Carme
K	S/2016 J 4‡			17.3	1 ≈ 1	0.000052 ≈ 0.000052	23113800	727.01 −727.01	147.1	0.294	2016	2023	Sheppard	Pasiphae
72 LXXII	S/2011 J 1♥			16.7	2 ≈ 2	0.00042 ≈ 0.00042	23124500	733.21 −733.21	164.6	0.271	2011	2012	Sheppard	Carme
11 XI	Carme♥	/ˈkɑːrmiː/		10.6	46.7	5.3 ≈ 5.3	23144400	734.19 −734.19	164.6	0.256	1938	1938	Nicholson	Carme
50 L	Herse♥	/ˈhɜːrsiː/		16.5	2 ≈ 2	0.00042 ≈ 0.00042	23150500	734.52 −734.52	164.4	0.262	2003	2003	Gladman et al.	Carme
61 LXI	S/2003 J 19♥			16.6	2 ≈ 2	0.00042 ≈ 0.00042	23156400	734.78 −734.78	164.7	0.265	2003	2003	Gladman	Carme
51 LI	S/2010 J 1♥			16.5	2 ≈ 2	0.00042 ≈ 0.00042	23189800	736.51 −736.51	164.5	0.252	2010	2011	Jacobson et al.	Carme
C	S/2003 J 9♥			16.9	1 ≈ 1	0.000052 ≈ 0.000052	23199400	736.86 −736.86	164.8	0.263	2003	2003	Sheppard	Carme
66 LXVI	S/2017 J 5♥			16.5	2 ≈ 2	0.00042 ≈ 0.00042	23206200	737.28 −737.28	164.8	0.257	2017	2018	Sheppard	Carme
67 LXVII	S/2017 J 6‡			16.6	2 ≈ 2	0.00042 ≈ 0.00042	23245300	733.99 −733.99	149.7	0.336	2017	2018	Sheppard	Pasiphae
23 XXIII	Kalyke♥	/ˈkæləkiː/		15.4	6.9	0.017000 ≈ 0.017	23302600	742.02 −742.02	164.8	0.260	2000	2001	Sheppard et al.	Carme
39 XXXIX	Hegemone‡	/həˈdʒɛməniː/		15.9	3 ≈ 3	0.0014 ≈ 0.0014	23348700	739.81 −739.81	152.6	0.358	2003	2003	Sheppard	Pasiphae
M	S/2018 J 3♥			17.3	1 ≈ 1	0.000052 ≈ 0.000052	23400300	747.02 −747.02	164.9	0.268	2018	2023	Sheppard	Carme
S	S/2021 J 5♥			16.8	2 ≈ 2	0.00042 ≈ 0.00042	23414600	747.74 −747.74	164.9	0.272	2021	2023	Sheppard et al.	Carme
08 VIII	Pasiphae‡	/pəˈsɪfeɪiː/		10.1	57.8	10 ≈ 10	23468200	743.61 −743.61	148.4	0.412	1908	1908	Melotte	Pasiphae
36 XXXVI	Sponde‡	/ˈspɒndiː/		16.7	2 ≈ 2	0.00042 ≈ 0.00042	23543300	748.29 −748.29	149.3	0.322	2001	2002	Sheppard et al.	Pasiphae
D	S/2003 J 10♥			16.9	2 ≈ 2	0.00042 ≈ 0.00042	23576300	755.43 −755.43	164.4	0.264	2003	2003	Sheppard	Carme
19 XIX	Megaclite‡	/ˌmɛɡəˈklaɪtiː/		15.0	5 ≈ 5	0.0065 ≈ 0.0065	23644600	752.86 −752.86	149.8	0.421	2000	2001	Sheppard et al.	Pasiphae
48 XLVIII	Cyllene‡	/səˈliːniː/		16.3	2 ≈ 2	0.00042 ≈ 0.00042	23654700	751.97 −751.97	146.8	0.419	2003	2003	Sheppard	Pasiphae
09 IX	Sinope‡	/səˈnoʊpiː/		11.1	35	2.2 ≈ 2.2	23683900	758.85 −758.85	157.3	0.264	1914	1914	Nicholson	Pasiphae
59 LIX	S/2017 J 1‡			16.8	2 ≈ 2	0.00042 ≈ 0.00042	23744800	756.41 −756.41	145.8	0.328	2017	2017	Sheppard	Pasiphae
41 XLI	Aoede‡	/eɪˈiːdiː/		15.6	4 ≈ 4	0.0034 ≈ 0.0034	23778200	761.42 −761.42	155.7	0.436	2003	2003	Sheppard	Pasiphae
28 XXVIII	Autonoe‡	/ɔːˈtɒnoʊiː/		15.5	4 ≈ 4	0.0034 ≈ 0.0034	23792500	761.00 −761.00	150.8	0.330	2001	2002	Sheppard et al.	Pasiphae
17 XVII	Callirrhoe‡	/kəˈlɪroʊiː/		14.0	9.6	0.046 ≈ 0.046	23795500	758.87 −758.87	145.1	0.297	1999	2000	Scotti et al.	Pasiphae
G	S/2003 J 23‡			16.6	2 ≈ 2	0.00042 ≈ 0.00042	23829300	760.00 −760.00	144.7	0.313	2003	2004	Sheppard	Pasiphae
49 XLIX	Kore‡	/ˈkɔːriː/		16.6	2 ≈ 2	0.00042 ≈ 0.00042	24205200	776.76 −776.76	141.5	0.328	2003	2003	Sheppard	Pasiphae

Exploration

The orbit and motion of the Galilean moons around Jupiter, as captured by JunoCam aboard the Juno spacecraft

Ganymede taken by Juno during its 34th perijove

Nine spacecraft have visited Jupiter. The first were Pioneer 10 in 1973, and Pioneer 11 a year later, taking low-resolution images of the four Galilean moons and returning data on their atmospheres and radiation belts. The Voyager 1 and Voyager 2 probes visited Jupiter in 1979, discovering the volcanic activity on Io and the presence of water ice on the surface of Europa. Ulysses further studied Jupiter's magnetosphere in 1992 and then again in 2000.

The Galileo spacecraft was the first to enter orbit around Jupiter, arriving in 1995 and studying it until 2003. During this period, Galileo gathered a large amount of information about the Jovian system, making close approaches to all of the Galilean moons and finding evidence for thin atmospheres on three of them, as well as the possibility of liquid water beneath the surfaces of Europa, Ganymede, and Callisto. It also discovered a magnetic field around Ganymede.

Then the Cassini probe to Saturn flew by Jupiter in 2000 and collected data on interactions of the Galilean moons with Jupiter's extended atmosphere. The New Horizons spacecraft flew by Jupiter in 2007 and made improved measurements of its satellites' orbital parameters.

In 2016, the Juno spacecraft imaged the Galilean moons from above their orbital plane as it approached Jupiter orbit insertion, creating a time-lapse movie of their motion. With a mission extension, Juno has since begun close flybys of the Galileans, flying by Ganymede in 2021 followed by Europa and Io in 2022. It flew by Io again in late 2023 and once more in early 2024.

See also

In Spanish: Satélites de Júpiter para niños

• Jupiter's moons in fiction
• Satellite system (astronomy)