List of gravitationally rounded objects of the Solar System
Template:Short description Template:Main other Template:Use dmy dates Template:Contains special characters This is a list of most likely gravitationally rounded objects (GRO) of the Solar System, which are objects that have a rounded, ellipsoidal shape due to their own gravity (but are not necessarily in hydrostatic equilibrium). Apart from the Sun itself, these objects qualify as planets according to common geophysical definitions of that term. The radii of these objects range over three orders of magnitude, from planetary-mass objects like dwarf planets and some moons to the planets and the Sun. This list does not include small Solar System bodies, but it does include a sample of possible planetary-mass objects whose shapes have yet to be determined. The Sun's orbital characteristics are listed in relation to the Galactic Center, while all other objects are listed in order of their distance from the Sun.
Star
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The Sun is a G-type main-sequence star. It contains almost 99.9% of all the mass in the Solar System.[1]
| Sun[2][3] | ||
|---|---|---|
| File:Sun white.jpg | ||
| Symbol (image)<templatestyles src="Citation/styles.css"/>[q] | File:Sun symbol (fixed width).svg | |
| Symbol (Unicode)<templatestyles src="Citation/styles.css"/>[q] | ☉ | |
| Discovery year | Prehistoric | |
| Mean distance from the Galactic Center |
km light years |
≈ 2.5Template:E ≈ 26,000 |
| Mean radius | km :E<templatestyles src="Citation/styles.css"/>[f] |
695,508 109.3 |
| Surface area | km2 :E<templatestyles src="Citation/styles.css"/>[f] |
6.0877Template:E 11,990 |
| Volume | km3 :E<templatestyles src="Citation/styles.css"/>[f] |
1.4122Template:E 1,300,000 |
| Mass | kg :E<templatestyles src="Citation/styles.css"/>[f] |
1.9855Template:E 332,978.9 |
| Gravitational parameter | m3/s2 | 1.327×1020 |
| Density | g/cm3 | 1.409 |
| Equatorial gravity | m/s2 g |
274.0 27.94 |
| Escape velocity | km/s | 617.7 |
| Rotation period | days<templatestyles src="Citation/styles.css"/>[g] | 25.38 |
| Orbital period about Galactic Center[4] | million years | 225–250 |
| Mean orbital speed[4] | km/s | ≈ 220 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i] to the ecliptic | deg. | 7.25 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i] to the galactic plane | deg. | 67.23 |
| Mean surface temperature | K | 5,778 |
| Mean coronal temperature[5] | K | 1–2Template:E |
| Photospheric composition | H, He, O, C, Fe, S | |
Planets
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In 2006, the International Astronomical Union (IAU) defined a planet as a body in orbit around the Sun that was large enough to have achieved hydrostatic equilibrium and to have "cleared the neighbourhood around its orbit".[6] The practical meaning of "cleared the neighborhood" is that a planet is comparatively massive enough for its gravitation to control the orbits of all objects in its vicinity. In practice, the term "hydrostatic equilibrium" is interpreted loosely. Mercury is round but not actually in hydrostatic equilibrium, but it is universally regarded as a planet nonetheless.[7]
According to the IAU's explicit count, there are eight planets in the Solar System; four terrestrial planets (Mercury, Venus, Earth, and Mars) and four giant planets, which can be divided further into two gas giants (Jupiter and Saturn) and two ice giants (Uranus and Neptune). When excluding the Sun, the four giant planets account for more than 99% of the mass of the Solar System.
| * Terrestrial planet |
| ° Gas giant |
| × Ice giant |
| *Mercury[8][9][10] | *Venus[11][12][10] | *Earth[13][14][10] | *Mars[15][16][10] | °Jupiter[17][18][10] | °Saturn[19][20][10] | ×Uranus[21][22] | ×Neptune[23][24][10] | ||
|---|---|---|---|---|---|---|---|---|---|
| File:Mercury in true color.jpg | File:PIA23791-Venus-NewlyProcessedView-20200608.jpg | File:The Earth seen from Apollo 17.jpg | File:Mars - August 30 2021 - Flickr - Kevin M. Gill.png | File:Jupiter and its shrunken Great Red Spot.jpg | File:Saturn during Equinox.jpg | File:Uranus Voyager2 color calibrated.png | File:Neptune Voyager2 color calibrated.png | ||
| Symbol<templatestyles src="Citation/styles.css"/>[q] | File:Mercury symbol (fixed width).svg | File:Venus symbol (fixed width).svg | File:Earth symbol (fixed width).svg | File:Mars symbol (fixed width).svg | File:Jupiter symbol (fixed width).svg | File:Saturn symbol (fixed width).svg | File:Uranus symbol (fixed width).svg or File:Uranus Herschel symbol (fixed width).svg | File:Neptune symbol (fixed width).svg | |
| Symbol (Unicode)<templatestyles src="Citation/styles.css"/>[q] | ☿ | ♀ | 🜨 | ♂ | ♃ | ♄ | ⛢ or ♅ | ♆ | |
| Discovery year | Prehistoric | Prehistoric | Prehistoric | Prehistoric | Prehistoric | Prehistoric | 1781 | 1846 | |
| Mean distance from the Sun |
km AU |
57,909,175 0.38709893 |
108,208,930 0.72333199 |
149,597,890 1.00000011 |
227,936,640 1.52366231 |
778,412,010 5.20336301 |
1,426,725,400 9.53707032 |
2,870,972,200 19.19126393 |
4,498,252,900 30.06896348 |
| Equatorial radius | km :E<templatestyles src="Citation/styles.css"/>[f] |
2,440.53 0.3826 |
6,051.8 0.9488 |
6,378.1366 1 |
3,396.19 0.53247 |
71,492 11.209 |
60,268 9.449 |
25,559 4.007 |
24,764 3.883 |
| Surface area | km2 :E<templatestyles src="Citation/styles.css"/>[f] |
75,000,000 0.1471 |
460,000,000 0.9020 |
510,000,000 1 |
140,000,000 0.2745 |
64,000,000,000 125.5 |
44,000,000,000 86.27 |
8,100,000,000 15.88 |
7,700,000,000 15.10 |
| Volume | km3 :E<templatestyles src="Citation/styles.css"/>[f] |
6.083Template:E 0.056 |
9.28Template:E 0.857 |
1.083Template:E 1 |
1.6318Template:E 0.151 |
1.431Template:E 1,321.3 |
8.27Template:E 763.62 |
6.834Template:E 63.102 |
6.254Template:E 57.747 |
| Mass | kg :E<templatestyles src="Citation/styles.css"/>[f] |
3.302Template:E 0.055 |
4.8690Template:E 0.815 |
5.972Template:E 1 |
6.4191Template:E 0.107 |
1.8987Template:E 318 |
5.6851Template:E 95 |
8.6849Template:E 14.5 |
1.0244Template:E 17 |
| Gravitational parameter | m3/s2 | 2.203×1013 | 3.249×1014 | 3.986×1014 | 4.283×1013 | 1.267×1017 | 3.793×1016 | 5.794×1015 | 6.837×1015 |
| Density | g/cm3 | 5.43 | 5.24 | 5.52 | 3.940 | 1.33 | 0.70 | 1.30 | 1.76 |
| Equatorial gravity | m/s2 g |
3.70 0.377 |
8.87 0.904 |
9.8 1.00 |
3.71 0.378 |
24.79 2.528 |
10.44 1.065 |
8.87 0.904 |
11.15 1.137 |
| Escape velocity | km/s | 4.25 | 10.36 | 11.18 | 5.02 | 59.54 | 35.49 | 21.29 | 23.71 |
| Rotation period<templatestyles src="Citation/styles.css"/>[g] | days | 58.646225 | 243.0187 | 0.99726968 | 1.02595675 | 0.41354 | 0.44401 | 0.71833 | 0.67125 |
| Orbital period<templatestyles src="Citation/styles.css"/>[g] | days years |
87.969 0.2408467 |
224.701 0.61519726 |
365.256363 1.0000174 |
686.971 1.8808476 |
4,332.59 11.862615 |
10,759.22 29.447498 |
30,688.5 84.016846 |
60,182 164.79132 |
| Mean orbital speed | km/s | 47.8725 | 35.0214 | 29.7859 | 24.1309 | 13.0697 | 9.6724 | 6.8352 | 5.4778 |
| Eccentricity | 0.20563069 | 0.00677323 | 0.01671022 | 0.09341233 | 0.04839266 | 0.05415060 | 0.04716771 | 0.00858587 | |
| Inclination<templatestyles src="Citation/styles.css"/>[f] | deg. | 7.00 | 3.39 | 0[13] | 1.85 | 1.31 | 2.48 | 0.76 | 1.77 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i] | deg. | 0.0 | 177.3<templatestyles src="Citation/styles.css"/>[h] | 23.44 | 25.19 | 3.12 | 26.73 | 97.86<templatestyles src="Citation/styles.css"/>[h] | 28.32 |
| Mean surface temperature | K | 440–100 | 730 | 287 | 227 | 152 <templatestyles src="Citation/styles.css"/>[j] | 134 <templatestyles src="Citation/styles.css"/>[j] | 76 <templatestyles src="Citation/styles.css"/>[j] | 73 <templatestyles src="Citation/styles.css"/>[j] |
| Mean air temperature<templatestyles src="Citation/styles.css"/>[k] | K | 288 | 165 | 135 | 76 | 73 | |||
| Atmospheric composition | He, Na+ K+ |
CO2, N2, SO2 | N2, O2, Ar, CO2 | CO2, N2 Ar |
H2, He | H2, He | H2, He CH4 |
H2, He CH4 | |
| Number of known moons<templatestyles src="Citation/styles.css"/>[v] | 0 | 0 | 1 | 2 | 97 | 274 | 28 | 16 | |
| Rings? | No | No | No | No | Yes | Yes | Yes | Yes | |
| Planetary discriminant<templatestyles src="Citation/styles.css"/>[l]<templatestyles src="Citation/styles.css"/>[o] | 9.1Template:E | 1.35Template:E | 1.7Template:E | 1.8Template:E | 6.25Template:E | 1.9Template:E | 2.9Template:E | 2.4Template:E | |
Dwarf planets
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Dwarf planets are bodies orbiting the Sun that are massive and warm enough to have achieved hydrostatic equilibrium, but have not cleared their neighbourhoods of similar objects. Since 2008, there have been five dwarf planets recognized by the IAU, although only Pluto has actually been confirmed to be in hydrostatic equilibrium[25] (Ceres is close to equilibrium, though some anomalies remain unexplained).[26] Ceres orbits in the asteroid belt, between Mars and Jupiter. The others all orbit beyond Neptune.
| † Asteroid belt |
| ‡ Kuiper belt |
| § Scattered disc |
| × Sednoid |
| †Template:Dwarfplanet[27] | ‡Template:Dwarfplanet[28][29] | ‡Template:Dwarfplanet[30][31][32] | ‡Template:Dwarfplanet[33][34] | §Template:Dwarfplanet[35] | ||
|---|---|---|---|---|---|---|
| File:Ceres - RC3 - Haulani Crater (22381131691) (cropped).jpg | File:Pluto in True Color - High-Res.jpg | File:Haumea Hubble.png | File:Makemake moon Hubble image with legend (cropped).jpg | File:Eris and dysnomia2.jpg | ||
| Symbol<templatestyles src="Citation/styles.css"/>[q] | File:Ceres symbol (fixed width).svg | File:Pluto monogram (fixed width).svg or File:Pluto symbol (large orb, fixed width).svg | File:Haumea symbol (fixed width).svg | File:Makemake symbol (fixed width).svg | File:Eris symbol (fixed width).svg | |
| Symbol (Unicode)<templatestyles src="Citation/styles.css"/>[q] | ⚳ | ♇ or ⯓ | 🝻 | 🝼 | ⯰ | |
| Minor planet number | 1 | 134340 | 136108 | 136472 | 136199 | |
| Discovery year | 1801 | 1930 | 2004 | 2005 | 2005 | |
| Mean distance from the Sun |
km AU |
413,700,000 2.766 |
5,906,380,000 39.482 |
6,484,000,000 43.335 |
6,850,000,000 45.792 |
10,210,000,000 67.668 |
| Mean radius | km :E<templatestyles src="Citation/styles.css"/>[f] |
473 0.0742 |
1,188.3[10] 0.186 |
816 (Template:Val)Script error: No such module "Check for unknown parameters". 0.13[36][37] |
715 0.11[38] |
1,163 0.18[39] |
| Volume | km3 :E<templatestyles src="Citation/styles.css"/>[f] |
4.21Template:E 0.00039<templatestyles src="Citation/styles.css"/>[b] |
6.99Template:E 0.0065 |
1.98Template:E 0.0018 |
1.7Template:E 0.0016<templatestyles src="Citation/styles.css"/>[b] |
6.59Template:E 0.0061<templatestyles src="Citation/styles.css"/>[b] |
| Surface area | km2 :E<templatestyles src="Citation/styles.css"/>[f] |
2,770,000 0.0054<templatestyles src="Citation/styles.css"/>[a] |
17,700,000 0.035 |
8,140,000 0.016<templatestyles src="Citation/styles.css"/>[y] |
6,900,000 0.0135<templatestyles src="Citation/styles.css"/>[a] |
17,000,000 0.0333<templatestyles src="Citation/styles.css"/>[a] |
| Mass | kg :E<templatestyles src="Citation/styles.css"/>[f] |
9.39Template:E ≈ 0.0002 |
1.30Template:E 0.0022 |
4.01 ± 0.04Template:E 0.0007[40] |
≈ 3.1Template:E 0.0005 |
1.65Template:E 0.0028 |
| Gravitational parameter | m3/s2 | 6.263 × 1010 | 8.710 × 1011 | 2.674 × 1011 | 2.069 × 1011 | 1.108 × 1012 |
| Density | g/cm3 | 2.16 | 1.87 | 2.02[36] | 2.03 | 2.43 |
| Equatorial gravity | m/s2 g |
0.27<templatestyles src="Citation/styles.css"/>[d] 0.028 |
0.62 0.063 |
0.63<templatestyles src="Citation/styles.css"/>[d] 0.064 |
0.40 0.041 |
0.82<templatestyles src="Citation/styles.css"/>[d] 0.084 |
| Escape velocity | km/s<templatestyles src="Citation/styles.css"/>[e] | 0.51 | 1.21 | 0.91 | 0.54 | 1.37 |
| Rotation period<templatestyles src="Citation/styles.css"/>[g] | days | 0.3781 | 6.3872 | 0.1631 | 0.9511 | 15.7859 |
| Orbital period<templatestyles src="Citation/styles.css"/>[g] | years | 4.599 | 247.9 | 283.8 | 306.2 | 559 |
| Mean orbital speed | km/s | 17.882 | 4.75 | 4.48<templatestyles src="Citation/styles.css"/>[o] | 4.40<templatestyles src="Citation/styles.css"/>[o] | 3.44<templatestyles src="Citation/styles.css"/>[n] |
| Eccentricity | 0.080 | 0.249 | 0.195 | 0.161 | 0.436 | |
| Inclination<templatestyles src="Citation/styles.css"/>[f] | deg. | 10.59 | 17.14 | 28.21 | 28.98 | 44.04 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i] | deg. | 4 | 119.6<templatestyles src="Citation/styles.css"/>[h] | ≈ 126<templatestyles src="Citation/styles.css"/>[h] | ? | ≈ 78 |
| Mean surface temperature<templatestyles src="Citation/styles.css"/>[w] | K | 167[41] | 40[42] | <50[43] | 30 | 30 |
| Atmospheric composition | H2O | N2, CH4, CO | ? | N2, CH4[44] | N2, CH4[45] | |
| Number of known moons<templatestyles src="Citation/styles.css"/>[v] | 0 | 5 | 2[46] | 1[47] | 1[48] | |
| Rings? | No | No | Yes | ? | ? | |
| Planetary discriminant<templatestyles src="Citation/styles.css"/>[l]<templatestyles src="Citation/styles.css"/>[o] | 0.33 | 0.077 | 0.023 | 0.02 | 0.10 | |
Astronomers usually refer to solid bodies such as Ceres as dwarf planets, even if they are not strictly in hydrostatic equilibrium. They generally agree that several other trans-Neptunian objects (TNOs) may be large enough to be dwarf planets, given current uncertainties. However, there has been disagreement on the required size. Early speculations were based on the small moons of the giant planets, which attain roundness around a threshold of 200 km radius.[49] However, these moons are at higher temperatures than TNOs and are icier than TNOs are likely to be. Estimates from an IAU question-and-answer press release from 2006, giving 800 km radius and Template:Val mass as cut-offs that normally would be enough for hydrostatic equilibrium, while stating that observation would be needed to determine the status of borderline cases.[50] Many TNOs in the 200–500 km radius range are dark and low-density bodies, which suggests that they retain internal porosity from their formation, and hence are not planetary bodies (as planetary bodies have sufficient gravitation to collapse out such porosity).[51]
In 2023, Emery et al. wrote that near-infrared spectroscopy by the James Webb Space Telescope (JWST) in 2022 suggests that Sedna, Gonggong, and Quaoar underwent internal melting, differentiation, and chemical evolution, like the larger dwarf planets Pluto, Eris, Haumea, and Makemake, but unlike "all smaller KBOs". This is because light hydrocarbons are present on their surfaces (e.g. ethane, acetylene, and ethylene), which implies that methane is continuously being resupplied, and that methane would likely come from internal geochemistry. On the other hand, the surfaces of Sedna, Gonggong, and Quaoar have low abundances of CO and CO2, similar to Pluto, Eris, and Makemake, but in contrast to smaller bodies. This suggests that the threshold for dwarf planethood in the trans-Neptunian region is around 500 km radius.[52]
In 2024, Kiss et al. found that Quaoar has an ellipsoidal shape incompatible with hydrostatic equilibrium for its current spin. They hypothesised that Quaoar originally had a rapid rotation and was in hydrostatic equilibrium, but that its shape became "frozen in" and did not change as it spun down due to tidal forces from its moon Weywot.[53] If so, this would resemble the situation of Saturn's moon Iapetus, which is too oblate for its current spin.[54][55] Iapetus is generally still considered a planetary-mass moon nonetheless,[56] though not always.[57]
The table below gives Orcus, Quaoar, Gonggong, and Sedna as additional consensus dwarf planets; slightly smaller Salacia, which is larger than 400 km radius, has been included as a borderline case for comparison, (and is therefore italicized).
| ‡Orcus[58] | ‡Salacia[59] | ‡Quaoar[60] | §Gonggong[61] | ×Sedna[62] | ||
|---|---|---|---|---|---|---|
| File:Orcus-vanth hst2.jpg | File:Salacia Hubble.png | File:Quaoar-weywot hst.jpg | File:2007 OR10 and its moon.png | File:Sedna PRC2004-14d.jpg | ||
| Symbol<templatestyles src="Citation/styles.css"/>[q] | File:Orcus symbol (fixed width).svg | File:Quaoar symbol (fixed width).svg | File:Gonggong symbol (fixed width).svg | File:Sedna symbol (fixed width).svg | ||
| Symbol (Unicode)<templatestyles src="Citation/styles.css"/>[q] | 🝿 | 🝾 | 🝽 | ⯲ | ||
| Minor-planet number | 90482 | 120347 | 50000 | 225088 | 90377 | |
| Discovery year | 2004 | 2004 | 2002 | 2007 | 2003 | |
| Semi-major axis | km AU |
5,896,946,000 39.419 |
6,310,600,000 42.18 |
6,535,930,000 43.69 |
10,072,433,340 67.33 |
78,668,000,000 525.86 |
| Mean radius<templatestyles src="Citation/styles.css"/>[s] | km :E<templatestyles src="Citation/styles.css"/>[f] |
458.5[63] 0.0720 |
423[64] 0.0664 |
555[65] 0.0871 |
615[66] 0.0982 |
497.5[67] 0.0780 |
| Surface area<templatestyles src="Citation/styles.css"/>[a] | km2 :E<templatestyles src="Citation/styles.css"/>[f] |
2,641,700 0.005179 |
2,248,500 0.004408 |
3,870,800 0.007589 |
4,932,300 0.009671 |
3,110,200 0.006098 |
| Volume<templatestyles src="Citation/styles.css"/>[b] | km3 :E<templatestyles src="Citation/styles.css"/>[f] |
403,744,500 0.000373 |
317,036,800 0.000396 |
716,089,900 0.000661 |
1,030,034,600 0.000951 |
515,784,000 0.000476 |
| Mass<templatestyles src="Citation/styles.css"/>[t] | kg :E<templatestyles src="Citation/styles.css"/>[f] |
5.48Template:E[68] 0.0001 |
4.9Template:E[64] 0.0001 |
1.20Template:E[69] 0.0002 |
1.75Template:E[66] 0.0003 |
? |
| Density<templatestyles src="Citation/styles.css"/>[t] | g/cm3 | Template:Val[68] | Template:Val[64] | ≈ Template:Val | Template:Val | ? |
| Equatorial gravity<templatestyles src="Citation/styles.css"/>[d] | m/s2 g |
Template:Gr 0.017 |
Template:Gr 0.018 |
Template:Gr 0.025 |
Template:Gr 0.029 |
? |
| Escape velocity<templatestyles src="Citation/styles.css"/>[e] | km/s | Template:V2 | Template:V2 | Template:V2 | Template:V2 | ? |
| Rotation period<templatestyles src="Citation/styles.css"/>[g] | days | 9.54?[68] | ? | 0.7367[69] | 0.9333 | 0.4280[70] |
| Orbital period<templatestyles src="Citation/styles.css"/>[g] | years | 247.49 | 273.98 | 287.97 | 552.52 | 12,059 |
| Mean orbital speed | km/s | 4.68 | 4.57 | 4.52 | 3.63 | 1.04 |
| Eccentricity | 0.226 | 0.106 | 0.038 | 0.506 | 0.855 | |
| Inclination<templatestyles src="Citation/styles.css"/>[f] | deg. | 20.59 | 23.92 | 7.99 | 30.74 | 11.93 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i] | deg. | ? | ? | 13.6[69] or 14.0[71] | ? | ? |
| Mean surface temperature<templatestyles src="Citation/styles.css"/>[w] | K | ≈ 42 | ≈ 43 | ≈ 41 | ≈ 30 | ≈ 12 |
| Number of known moons | 1[72] | 1 | 1[73] | 1 | 0 | |
| Rings? | ? | ? | Yes[69] | ? | ? | |
| Planetary discriminant<templatestyles src="Citation/styles.css"/>[l]<templatestyles src="Citation/styles.css"/>[o] | 0.003 | <0.1 | 0.0015 | <0.1 | ?<templatestyles src="Citation/styles.css"/>[x] | |
| Absolute magnitude (H) | 2.3 | 4.1 | 2.71 | 1.8 | 1.5 | |
As for objects in the asteroid belt, none are generally agreed as dwarf planets today among astronomers other than Ceres. The second- through fifth-largest asteroids have been discussed as candidates. Vesta (radius Template:Val), the second-largest asteroid, appears to have a differentiated interior and therefore likely was once a dwarf planet, but it is no longer very round today.[74] Pallas (radius Template:Val), the third-largest asteroid, appears never to have completed differentiation and likewise has an irregular shape. Vesta and Pallas are nonetheless sometimes considered small terrestrial planets anyway by sources preferring a geophysical definition, because they do share similarities to the rocky planets of the inner solar system.[56] The fourth-largest asteroid, Hygiea (radius Template:Val), is icy. The question remains open if it is currently in hydrostatic equilibrium: while Hygiea is round today, it was probably previously catastrophically disrupted and today might be just a gravitational aggregate of the pieces.[75] The fifth-largest asteroid, Interamnia (radius Template:Val), is icy and has a shape consistent with hydrostatic equilibrium for a slightly shorter rotation period than it now has.[76]
Satellites
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There are at least 19 natural satellites in the Solar System that are known to be massive enough to be close to hydrostatic equilibrium: seven of Saturn, five of Uranus, four of Jupiter, and one each of Earth, Neptune, and Pluto. Alan Stern calls these satellite planets, although the term major moon is more common. The smallest natural satellite that is gravitationally rounded is Saturn I Mimas (radius Template:Val). This is smaller than the largest natural satellite that is known not to be gravitationally rounded, Neptune VIII Proteus (radius Template:Val).
Several of these were once in equilibrium but are no longer: these include Earth's moon[77] and all of the moons listed for Saturn apart from Titan and Rhea.[55] The status of Callisto, Titan, and Rhea is uncertain, as is that of the moons of Uranus, Pluto[25] and Eris.[51] The other large moons (Io, Europa, Ganymede, and Triton) are generally believed to still be in equilibrium today. Other moons that were once in equilibrium but are no longer very round, such as Saturn IX Phoebe (radius Template:Val), are not included. In addition to not being in equilibrium, Mimas and Tethys have very low densities and it has been suggested that they may have non-negligible internal porosity,[78][79] in which case they would not be satellite planets.
The moons of the trans-Neptunian objects (other than Charon) have not been included, because they appear to follow the normal situation for TNOs rather than the moons of Saturn and Uranus, and become solid at a larger size (900–1000 km diameter, rather than 400 km as for the moons of Saturn and Uranus). Eris I Dysnomia and Orcus I Vanth, though larger than Mimas, are dark bodies in the size range that should allow for internal porosity, and in the case of Dysnomia a low density is known.[51]
Satellites are listed first in order from the Sun, and second in order from their parent body. For the round moons, this mostly matches the Roman numeral designations, with the exceptions of Iapetus and the Uranian system. This is because the Roman numeral designations originally reflected distance from the parent planet and were updated for each new discovery until 1851, but by 1892, the numbering system for the then-known satellites had become "frozen" and from then on followed order of discovery. Thus Miranda (discovered 1948) is Uranus V despite being the innermost of Uranus' five round satellites. The missing Saturn VII is Hyperion, which is not large enough to be round (mean radius Template:Val).
| 🜨 Satellite of Earth |
| ♃ Satellite of Jupiter |
| ♄ Satellite of Saturn |
| ⛢ Satellite of Uranus |
| ♆ Satellite of Neptune |
| ♇ Satellite of Pluto |
| 🜨Moon[80] | ♃Io[81] | ♃Europa[82] | ♃Ganymede[83] | ♃Callisto[84] | ♄Mimas<templatestyles src="Citation/styles.css"/>[p] | ♄Enceladus<templatestyles src="Citation/styles.css"/>[p] | ♄Tethys<templatestyles src="Citation/styles.css"/>[p] | ♄Dione<templatestyles src="Citation/styles.css"/>[p] | ♄Rhea<templatestyles src="Citation/styles.css"/>[p] | ||
|---|---|---|---|---|---|---|---|---|---|---|---|
| File:FullMoon2010.jpg | File:Io highest resolution true color.jpg | File:Europa in natural color.png | File:Ganymede - Perijove 34 Composite.png | File:Callisto - July 8 1979 (38926064465).jpg | File:Mimas Cassini.jpg | File:PIA17202 - Approaching Enceladus.jpg | File:PIA18317-SaturnMoon-Tethys-Cassini-20150411.jpg | File:Dione in natural light (cropped).jpg | File:PIA07763 Rhea full globe5.jpg | ||
| Roman numeral designation | Earth I | Jupiter I | Jupiter II | Jupiter III | Jupiter IV | Saturn I | Saturn II | Saturn III | Saturn IV | Saturn V | |
| Symbol<templatestyles src="Citation/styles.css"/>[q] | ☾ | JI | JII | JIII | JIV | SI | SII | SIII | SIV | SV | |
| Symbol (Unicode)<templatestyles src="Citation/styles.css"/>[q] | ☾ | ||||||||||
| Discovery year | Prehistoric | 1610 | 1610 | 1610 | 1610 | 1789 | 1789 | 1684 | 1684 | 1672 | |
| Mean distance from primary |
km | 384,399 | 421,600 | 670,900 | 1,070,400 | 1,882,700 | 185,520 | 237,948 | 294,619 | 377,396 | 527,108 |
| Mean radius | km :E<templatestyles src="Citation/styles.css"/>[f] |
1,737.1 0.272 |
1,815 0.285 |
1,569 0.246 |
2,634.1 0.413 |
2,410.3 0.378 |
198.30 0.031 |
252.1 0.04 |
533 0.084 |
561.7 0.088 |
764.3 0.12 |
| Surface area<templatestyles src="Citation/styles.css"/>[a] | 1Template:E km2 | 37.93 | 41.910 | 30.9 | 87.0 | 73 | 0.49 | 0.799 | 3.57 | 3.965 | 7.337 |
| Volume<templatestyles src="Citation/styles.css"/>[b] | 1Template:E km3 | 22 | 25.3 | 15.9 | 76 | 59 | 0.033 | 0.067 | 0.63 | 0.8 | 1.9 |
| Mass | 1Template:E kg | 7.3477 | 8.94 | 4.80 | 14.819 | 10.758 | 0.00375 | 0.0108 | 0.06174 | 0.1095 | 0.2306 |
| Density<templatestyles src="Citation/styles.css"/>[c] | g/cm3 | 3.3464 | 3.528 | 3.01 | 1.936 | 1.83 | 1.15 | 1.61 | 0.98 | 1.48 | 1.23 |
| Equatorial gravity<templatestyles src="Citation/styles.css"/>[d] | m/s2 g |
1.622 0.1654 |
1.796 0.1831 |
1.314 0.1340 |
1.428 0.1456 |
1.235 0.1259 |
0.0636 0.00649 |
0.111 0.0113 |
0.145 0.0148 |
0.231 0.0236 |
0.264 0.0269 |
| Escape velocity<templatestyles src="Citation/styles.css"/>[e] | km/s | 2.38 | 2.56 | 2.025 | 2.741 | 2.440 | 0.159 | 0.239 | 0.393 | 0.510 | 0.635 |
| Rotation period | days<templatestyles src="Citation/styles.css"/>[g] | 27.321582 (sync)<templatestyles src="Citation/styles.css"/>[m] |
1.7691378 (sync) |
3.551181 (sync) |
7.154553 (sync) |
16.68902 (sync) |
0.942422 (sync) |
1.370218 (sync) |
1.887802 (sync) |
2.736915 (sync) |
4.518212 (sync) |
| Orbital period about primary | days<templatestyles src="Citation/styles.css"/>[g] | 27.32158 | 1.769138 | 3.551181 | 7.154553 | 16.68902 | 0.942422 | 1.370218 | 1.887802 | 2.736915 | 4.518212 |
| Mean orbital speed<templatestyles src="Citation/styles.css"/>[o] | km/s | 1.022 | 17.34 | 13.740 | 10.880 | 8.204 | 14.32 | 12.63 | 11.35 | 10.03 | 8.48 |
| Eccentricity | 0.0549 | 0.0041 | 0.009 | 0.0013 | 0.0074 | 0.0202 | 0.0047 | 0.02 | 0.002 | 0.001 | |
| Inclination to primary's equator | deg. | 18.29–28.58 | 0.04 | 0.47 | 1.85 | 0.2 | 1.51 | 0.02 | 1.51 | 0.019 | 0.345 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i]<templatestyles src="Citation/styles.css"/>[u] | deg. | 6.68 | 0.000405 ± 0.00076[85] |
0.0965 ± 0.0069[85] |
0.155 ± 0.065[85] |
≈ 0–2[85]<templatestyles src="Citation/styles.css"/>[aa] | ≈ 0 | ≈ 0 | ≈ 0 | ≈ 0 | ≈ 0 |
| Mean surface temperature<templatestyles src="Citation/styles.css"/>[w] | K | 220 | 130 | 102 | 110[86] | 134 | 64 | 75 | 64 | 87 | 76 |
| Atmospheric composition | Ar, He Na, K, H |
SO2[87] | O2[88] | O2[89] | O2, CO2[90] | H2O, N2 CO2, CH4[91] |
|||||
| ♄Titan<templatestyles src="Citation/styles.css"/>[p] | ♄Iapetus<templatestyles src="Citation/styles.css"/>[p] | ⛢Miranda<templatestyles src="Citation/styles.css"/>[r] | ⛢Ariel<templatestyles src="Citation/styles.css"/>[r] | ⛢Umbriel<templatestyles src="Citation/styles.css"/>[r] | ⛢Titania<templatestyles src="Citation/styles.css"/>[r] | ⛢Oberon<templatestyles src="Citation/styles.css"/>[r] | ♆Triton[92] | ♇Charon[28] | ||
|---|---|---|---|---|---|---|---|---|---|---|
| File:Titan in true color.jpg | File:Iapetus true.jpg | File:Miranda mosaic in color - Voyager 2.png | File:Ariel in monochrome.jpg | File:PIA00040 Umbrielx2.47.jpg | File:Titania (moon) color cropped.jpg | File:Oberon in true color by Kevin M. Gill.jpg | File:Neptune’s Moon Triton Fosters Rare Icy Union (gemini1903a) (square crop).jpg | File:Charon in True Color - High-Res.jpg | ||
| Roman numeral designation | Saturn VI | Saturn VIII | Uranus V | Uranus I | Uranus II | Uranus III | Uranus IV | Neptune I | Pluto I | |
| Symbol | SVI | SVIII | UV | UI | UII | UIII | UIV | NI | PI | |
| Discovery year | 1655 | 1671 | 1948 | 1851 | 1851 | 1787 | 1787 | 1846 | 1978 | |
| Mean distance from primary |
km | 1,221,870 | 3,560,820 | 129,390 | 190,900 | 266,000 | 436,300 | 583,519 | 354,759 | 17,536 |
| Mean radius | km :E<templatestyles src="Citation/styles.css"/>[f] |
2,576 0.404 |
735.60 0.115 |
235.8 0.037 |
578.9 0.091 |
584.7 0.092 |
788.9 0.124 |
761.4 0.119 |
1,353.4 0.212 |
603.5 0.095 |
| Surface area<templatestyles src="Citation/styles.css"/>[a] | 1Template:E km2 | 83.0 | 6.7 | 0.70 | 4.211 | 4.296 | 7.82 | 7.285 | 23.018 | 4.580 |
| Volume<templatestyles src="Citation/styles.css"/>[b] | 1Template:E km3 | 71.6 | 1.67 | 0.055 | 0.81 | 0.84 | 2.06 | 1.85 | 10 | 0.92 |
| Mass | 1Template:E kg | 13.452 | 0.18053 | 0.00659 | 0.135 | 0.12 | 0.35 | 0.3014 | 2.14 | 0.152 |
| Density<templatestyles src="Citation/styles.css"/>[c] | g/cm3 | 1.88 | 1.08 | 1.20 | 1.67 | 1.40 | 1.72 | 1.63 | 2.061 | 1.65 |
| Equatorial gravity<templatestyles src="Citation/styles.css"/>[d] | m/s2 g |
1.35 0.138 |
0.22 0.022 |
0.08 0.008 |
0.27 0.028 |
0.23 0.023 |
0.39 0.040 |
0.35 0.036 |
0.78 0.080 |
0.28 0.029 |
| Escape velocity<templatestyles src="Citation/styles.css"/>[e] | km/s | 2.64 | 0.57 | 0.19 | 0.56 | 0.52 | 0.77 | 0.73 | 1.46 | 0.58 |
| Rotation period | days<templatestyles src="Citation/styles.css"/>[g] | 15.945 (sync)<templatestyles src="Citation/styles.css"/>[m] |
79.322 (sync) |
1.414 (sync) |
2.52 (sync) |
4.144 (sync) |
8.706 (sync) |
13.46 (sync) |
5.877 (sync) |
6.387 (sync) |
| Orbital period about primary | days | 15.945 | 79.322 | 1.4135 | 2.520 | 4.144 | 8.706 | 13.46 | 5.877 | 6.387 |
| Mean orbital speed<templatestyles src="Citation/styles.css"/>[o] | km/s | 5.57 | 3.265 | 6.657 | 5.50898 | 4.66797 | 3.644 | 3.152 | 4.39 | 0.2 |
| Eccentricity | 0.0288 | 0.0286 | 0.0013 | 0.0012 | 0.005 | 0.0011 | 0.0014 | 0.00002 | 0.0022 | |
| Inclination to primary's equator | deg. | 0.33 | 14.72 | 4.22 | 0.31 | 0.36 | 0.14 | 0.10 | 157<templatestyles src="Citation/styles.css"/>[h] | 0.001 |
| Axial tilt<templatestyles src="Citation/styles.css"/>[i]<templatestyles src="Citation/styles.css"/>[u] | deg. | ≈ 0.3[93] | ≈ 0 | ≈ 0 | ≈ 0 | ≈ 0 | ≈ 0 | ≈ 0 | ≈ 0.7[94] | ≈ 0 |
| Mean surface temperature<templatestyles src="Citation/styles.css"/>[w] | K | 93.7[95] | 130 | 59 | 58 | 61 | 60 | 61 | 38[96] | 53 |
| Atmospheric composition | N2, CH4[97] | N2, CH4[98] | ||||||||
See also
- List of Solar System objects by size
- Lists of astronomical objects
- List of former planets
- Planetary-mass object
Notes
Unless otherwise cited<templatestyles src="Citation/styles.css"/>[z]
Manual calculations (unless otherwise cited)
Individual calculations
Other notes
Template:Ordered list Template:Refend
References
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- ↑ Script error: No such module "Citation/CS1".
- ↑ NASA Solar System exploration Sun factsheet Template:Webarchive and NASA Sun factsheet Template:Webarchive NASA Retrieved 2008-11-17 (unless otherwise cited)
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- ↑ Cowen, R. (2007). Idiosyncratic Iapetus, Science News vol. 172, pp. 104–106. references Template:Webarchive
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