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List of exceptional asteroids
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The following is a collection of lists of asteroids of the Solar System that are exceptional in some way, such as their size or orbit. For the purposes of this article, "asteroid" refers to minor planets out to the orbit of Neptune, and includes the dwarf planet Ceres, the Jupiter trojans and the centaurs, but not trans-Neptunian objects (objects in the Kuiper belt, scattered disc or inner Oort cloud). For a complete list of minor planets in numerical order, see List of minor planets.
Asteroids are given minor planet numbers, but not all minor planets are asteroids. Minor planet numbers are also given to objects of the Kuiper belt, which is similar to the asteroid belt but farther out (around 30–60 AU). Asteroids are mostly between 2–3 AU from the Sun or at the orbit of Jupiter, 5 AU from the Sun. Comets are not typically included under minor planet numbers, and have their own naming conventions.
Asteroids are given a unique sequential identifying number once their orbit is precisely determined. Prior to this, they are known only by their systematic name or provisional designation, such as 1950 DA.
Physical characteristics
[edit]Largest by diameter
[edit]Estimating the sizes of asteroids from observations is difficult due to their irregular shapes, varying albedo, and small angular diameter. Observations by the Very Large Telescope of most large asteroids were published 2019–2021.[1][2]
| Name | Picture | Diameter (km) (geometric mean) |
Dimensions (km) | Mean distance from Sun (in AU) |
Inclination (°) | Date discovered | Discoverer | Class |
|---|---|---|---|---|---|---|---|---|
| 1 Ceres | 939.4±0.2 | 964.4 × 964.2 × 891.8 | 2.766 | 10.6 | January 1, 1801 | Piazzi, G. | G | |
| 4 Vesta | 525.4±0.2 | 572.6 × 557.2 × 446.4 ± 0.2 | 2.362 | 7.14 | March 29, 1807 | Olbers, H. W. | V | |
| 2 Pallas | 511±4[1] | 568×530×450 | 2.773 | 34.9 | March 28, 1802 | Olbers, H. W. | B | |
| 10 Hygiea | 433±8[1] | 450×430×424 | 3.139 | 5.1 | April 12, 1849 | de Gasparis, A. | C | |
| 704 Interamnia | 332±5[1] | 362×348×310 | 3.062 | 17.3 | October 2, 1910 | Cerulli, V. | F | |
| 52 Europa | 319±4[1] | 378×336×255 | 3.095 | 7.48 | February 4, 1858 | Goldschmidt, H. | C | |
| 511 Davida | 298±4[1] | 359×293×253 | 3.168 | 15.9 | May 30, 1903 | Dugan, R. S. | C | |
| 87 Sylvia | 271±5[1] | 363×249×191 or 374×248×194 |
3.485 | 10.9 | May 16, 1866 | Pogson, N. R. | X | |
| 15 Eunomia | 270±3[1] | 357×255×212 | 2.643 | 11.75 | July 29, 1851 | de Gasparis, A. | S | |
| 31 Euphrosyne | 268±4[1] | 294×280×248 | 3.149 | 26.3 | September 1, 1854 | Ferguson, J. | C | |
| 65 Cybele | 263±3 | 297 × 291 × 213 | 3.439 | 3.56 | March 8, 1861 | Tempel, E. W. | C | |
| 624 Hektor | 256±12 (if bilobe) |
403 × 201 | 5.235 | 18.66 | February 10, 1907 | Kopff, A. | D | |
| 3 Juno | 254±2[1] | 288×250×225 | 2.672 | 12.98 | September 1, 1804 | Harding, K. L. | S | |
| 451 Patientia | 254±3 | 3.059 | 15.2 | December 4, 1899 | Charlois, A. | |||
| 107 Camilla | 254±12[3] | 3.476 | 10 | November 17, 1868 | Pogson, N. R. | C | ||
| 324 Bamberga | 227±3[1] | 234×224×225 | 2.684 | 11.1 | February 25, 1892 | Palisa, J. | C | |
| 16 Psyche | 223±3[1] | 279×232×189 ± 10% | 2.924 | 3.1 | March 17, 1852 | de Gasparis, A. | M | |
| 88 Thisbe | 218±3[1] | 255×232×193 | 2.769 | 5.22 | June 15, 1866 | Peters, C. H. F. | B | |
| 48 Doris | 215±3[1] | 257×211×185 | 3.108 | 6.55 | September 19, 1857 | Goldschmidt, H. | C | |
| 19 Fortuna | 211±2[1] | 225×205×195 | 2.442 | 1.57 | August 22, 1852 | Hind, J. R. | G | |
| 121 Hermione | 209±5?[4] | 3.457 | 7.6 | May 12, 1872 | Watson, J. C. | C | ||
| 24 Themis | 208±3[1] | 232×220×176 | 3.136 | 0.76 | April 5, 1853 | de Gasparis, A. | C | |
| 94 Aurora | 205±4 ? (< 200 km)[1] | 225×173 | 3.160 | 7.97 | September 6, 1867 | Watson, J. C. | C | |
| 29 Amphitrite | 204±2[1] | 222×209×183 | 2.554 | 6.08 | March 1, 1854 | Marth, A. | S | |
| 13 Egeria | 202±3[1] | 238×199×182 | 2.576 | 16.54 | November 2, 1850 | de Gasparis, A. | G | |
| 130 Elektra | 199±2[1] | 262×205×164 | 3.127 | 22.78 | February 17, 1873 | C. H. F. Peters | C | |
| 7 Iris | 199±10[1] | 268×234×180[5] | 2.386 | 5.52 | August 13, 1847 | Hind, J. R. | S | |
| 6 Hebe | 195±3[1] | 205x185x170 | 2.426 | 14.75 | July 1, 1847 | Hencke, K. L. | S | |
| 375 Ursula | 192±4 | 3.126 | 15.94 | September 18, 1893 | Charlois, A. | C | ||
| 702 Alauda | 191±2 | 3.195 | 20.59 | July 16, 1910 | Helffrich, J. | C/B | ||
| 45 Eugenia | 188±2[1] | 252×191×138 | 2.720 | 6.61 | June 27, 1857 | Goldschmidt, H. | F | |
| 41 Daphne | 187±13[1] | 235×183×153 | 2.765 | 15.77 | May 22, 1856 | Goldschmidt, H. | C | |
| 154 Bertha | 186±2 | 3.195 | 20.972 | November 4, 1875 | Henry, P. M. | C | ||
| 423 Diotima | 176±4 | 3.065 | 11.23 | December 7, 1896 | Charlois, A. | C | ||
| 259 Aletheia | 174±1 | 3.135 | 10.81 | June 28, 1886 | Peters, C. H. F. | C/P/X | ||
| 372 Palma | 174±3 | 3.149 | 23.83 | August 19, 1893 | Charlois, A. | B | ||
| 9 Metis | 173±2[1] | 222×182×130 | 2.385 | 5.58 | April 25, 1848 | Graham, A. | S | |
| 532 Herculina | 168±1 | 2.772 | 16.31 | April 20, 1904 | Wolf, M. | S | ||
| 354 Eleonora | 165±3[1] | 191×162×144 | 2.798 | 18.4 | January 17, 1893 | Auguste Charlois | S | |
| 128 Nemesis | 163±5[1] | 178×163×147 | 2.751 | 6.25 | November 25, 1872 | Watson, J. C. | C | |
| (4:1 resonance) [sort by 'Mean Distance from Sun' to place in table] | 2.06 | (defines inner edge of main belt) | ||||||
| (3:1 resonance) | 2.50 | (separates inner from middle belt) | ||||||
| (5:2 resonance) | 2.82 | (separates middle from outer belt) | ||||||
| (7:3 resonance) | 2.95 | |||||||
| (2:1 resonance) | 3.27 | (defines outermost belt) | ||||||
| (1:1 resonance) | 5.20 | (Trojan asteroids – defines outer edge of main belt) | ||||||
The number of bodies grows rapidly as the size decreases. Based on IRAS data there are about 140 main-belt asteroids with a diameter greater than 120 km,[6] which is approximately the transition point between surviving primordial asteroids and fragments thereof.[7][8] For a more complete list, see List of Solar System objects by size.
The inner asteroid belt (defined as the region interior to the 3:1 Kirkwood gap at 2.50 AU) has few large asteroids. Of those in the above list, only 4 Vesta, 19 Fortuna, 6 Hebe, 7 Iris and 9 Metis orbit there. (Sort table by mean distance.)
Most massive
[edit]Below are the sixteen most-massive measured asteroids.[9] Ceres, at a third the estimated mass of the asteroid belt, is half again as massive as the next fifteen put together. The masses of asteroids are estimated from perturbations they induce on the orbits of other asteroids, except for asteroids that have been visited by spacecraft or have an observable moon, where a direct mass calculation is possible. Different sets of astrometric observations lead to different mass determinations; the biggest problem is accounting for the aggregate perturbations caused by all of the smaller asteroids.[10]
- Ceres 938 (39.2%)
- Vesta 259 (10.8%)
- Pallas 204 (8.52%)
- Hygiea 87 (3.64%)
- Interamnia 35 (1.46%)
- Eunomia 30 (1.25%)
- Juno 27 (1.13%)
- Davida 27 (1.13%)
- Europa 24 (1.00%)
- Psyche 23 (0.96%)
- Herculina 23 (0.96%)
- other 716 (29.9%)
| Name | Mass (×1018 kg) |
Precision | Approx. proportion of all asteroids |
|---|---|---|---|
| 1 Ceres | 938.35 | 0.001% (938.34–938.36) | 39.2% |
| 4 Vesta | 259.076 | 0.0004% (259.075–259.077) | 10.8% |
| 2 Pallas | 204 | 1.5% (201–207) | 8.5% |
| 10 Hygiea | 87 | 8% (80–94) | 3.6% |
| 704 Interamnia | 35 | 14% (30–40) | 1.5% |
| 15 Eunomia | 30 | 6% (29–32) | 1.3% |
| 3 Juno | 27 | 9% (25–29) | 1.1% |
| 511 Davida | 27 | 27% (19–34) | 1.1% |
| 52 Europa | 24 | 16% (20–28) | 1.0% |
| 16 Psyche | 23 | 13% (20–26) | 1.0% |
| 532 Herculina | ≈ 23 | ? | ≈ 1% |
| 31 Euphrosyne | 17 | 18% (14–19) | 0.7% |
| 65 Cybele | 15 | 12% (13–17) | 0.6% |
| 87 Sylvia | 14.76 | 0.4% (14.70–14.82)[12] | 0.6% |
| 7 Iris | 14 | 17% (11–16) | 0.6% |
| 29 Amphitrite | 13 | 16% (11–15) | 0.5% |
| 6 Hebe | 12 | 20% (10–15) | 0.5% |
| 88 Thisbe | 12 | 20% (9–14) | 0.5% |
| 107 Camilla | 11.2 | 1% (11.1–11.3)[3] | 0.5% |
| 324 Bamberga | 10 | 9% (9–11) | 0.4% |
| Total | 1781 | NA | 75% |
The proportions assume that the total mass of the asteroid belt is 2.39×1021 kg, or (12.4±1.0)×10−10 M☉.[13]
Outside the top four, the ranking of all the asteroids is uncertain, as there is a great deal of overlap among the estimates.
The largest asteroids with an accurately measured mass, because they have been studied by the probe Dawn, are 1 Ceres with a mass of (939.3±0.5)×1018 kg, and 4 Vesta at (259.076±0.001)×1018 kg. The third-largest asteroid with an accurately measured mass, because it has moons, is 87 Sylvia at (14.76±0.06)×1018 kg. Other large asteroids with masses measured from their moons are 107 Camilla and 130 Elektra.[3][14][1]
For a more complete list, see List of Solar System objects by size. Other large asteroids such as 423 Diotima currently only have estimated masses.[15][16]
Brightest from Earth
[edit]Only Vesta is regularly bright enough to be seen with the naked eye. Under ideal viewing conditions with very dark skies, a keen eye might be able to also see Ceres, as well as Pallas and Iris at their rare perihelic oppositions.[17] The following asteroids can all reach an apparent magnitude brighter than or equal to the +8.3 attained by Saturn's moon Titan at its brightest, which was discovered 145 years before the first asteroid was found owing to its closeness to the easily observed Saturn.
None of the asteroids in the outer part of the asteroid belt can ever attain this brightness. Even Hygiea and Interamnia rarely reach magnitudes of above 10.0. This is due to the different distributions of spectral types within different sections of the asteroid belt: the highest-albedo asteroids are all concentrated closer to the orbit of Mars, and much lower albedo C and D types are common in the outer belt.
Those asteroids with very high eccentricities will only reach their maximum magnitude rarely, when their perihelion is very close to a heliocentric conjunction with Earth, or (in the cases of 433 Eros, 99942 Apophis, (152680) 1998 KJ9, (153814) 2001 WN5, and 367943 Duende) when the asteroid passes very close to Earth.
| Asteroid | Magnitude when brightest[citation needed] |
Semi- major axis (AU) |
Eccentricity of orbit |
Diameter (km) |
Year of discovery |
|---|---|---|---|---|---|
| 99942 Apophis | 3.4* | 0.922 | 0.191 | 0.32 | 2004 |
| 4 Vesta | 5.20 | 2.361 | 0.089172 | 529 | 1807 |
| 2 Pallas | 6.49 | 2.773 | 0.230725 | 544 | 1802 |
| 1 Ceres | 6.65 | 2.766 | 0.079905 | 952 | 1801 |
| 7 Iris | 6.73 | 2.385 | 0.231422 | 200 | 1847 |
| 433 Eros | 6.8 | 1.458 | 0.222725 | 34 × 11 × 11 | 1898 |
| (153814) 2001 WN5 | 6.85 | 1.711 | 0.467207 | 0.93 | 2001 |
| 367943 Duende | 7.04 | 0.910 | 0.089319 | 0.04 × 0.02 | 2012 |
| 6 Hebe | 7.5 | 2.425 | 0.201726 | 186 | 1847 |
| 3 Juno | 7.5 | 2.668 | 0.258194 | 233 | 1804 |
| 18 Melpomene | 7.5 | 2.296 | 0.218708 | 141 | 1852 |
| (152680) 1998 KJ9 | 7.74 | 1.448 | 0.639770 | 0.5 | 1998 |
| 15 Eunomia | 7.9 | 2.643 | 0.187181 | 268 | 1851 |
| 8 Flora | 7.9 | 2.202 | 0.156207 | 128 | 1847 |
| 324 Bamberga | 8.0 | 2.682 | 0.338252 | 229 | 1892 |
| 1036 Ganymed | 8.1 | 2.6657 | 0.533710 | 32 | 1924 |
| 9 Metis | 8.1 | 2.387 | 0.121441 | 190 | 1848 |
| 192 Nausikaa | 8.2 | 2.404 | 0.246216 | 103 | 1879 |
| 20 Massalia | 8.3 | 2.409 | 0.142880 | 145 | 1852 |
* Apophis will only achieve that brightness on April 13, 2029.[18][19] It typically has an apparent magnitude of 20–22.
Slowest rotators
[edit]This list contains the slowest-rotating known minor planets with a period of at least 1000 hours, or 412⁄3 days, while most bodies have rotation periods between 2 and 20 hours. Also see Potentially slow rotators for minor planets with an insufficiently accurate period (U < 2).
| # | Minor planet designation | Rotation period (hours) |
Δmag | Quality (U) |
Orbit or family | Spectral type | Diameter (km) |
Abs. mag (H) |
Refs |
|---|---|---|---|---|---|---|---|---|---|
| 1. | (162058) 1997 AE12 | 1880 | 0.6 | 2 | NEO | S | 0.782 | 17.9 | LCDB · List |
| 2. | 846 Lipperta | 1641 | 0.30 | 2 | Themis | CBU: | 52.41 | 10.26 | LCDB · List |
| 3. | 2440 Educatio | 1561 | 0.80 | 2 | Flora | S | 6.51 | 13.1 | LCDB · List |
| 4. | 912 Maritima | 1332 | 0.18 | 3− | MBA (outer) | C | 82.14 | 9.30 | LCDB · List |
| 5. | 9165 Raup | 1320 | 1.34 | 3− | Hungaria | S | 4.62 | 13.60 | LCDB · List |
| 6. | 1235 Schorria | 1265 | 1.40 | 3 | Hungaria | CX: | 5.04 | 13.10 | LCDB · List |
| 7. | 50719 Elizabethgriffin | 1256 | 0.42 | 2 | Eunomia | S | 3.40 | 14.65 | LCDB · List |
| 8. | (75482) 1999 XC173 | 1234.2 | 0.69 | 2 | Vestian | S | 2.96 | 15.01 | LCDB · List |
| 9. | 288 Glauke | 1170 | 0.90 | 3 | MBA (outer) | S | 32.24 | 10.00 | LCDB · List |
| 10. | (39546) 1992 DT5 | 1167.4 | 0.80 | 2 | MBA (outer) | C | 5.34 | 15.09 | LCDB · List |
| 11. | 496 Gryphia | 1072 | 1.25 | 3 | Flora | S | 15.47 | 11.61 | LCDB · List |
| 12. | 4524 Barklajdetolli | 1069 | 1.26 | 2 | Flora | S | 7.14 | 12.90 | LCDB · List |
| 13. | 2675 Tolkien | 1060 | 0.75 | 2+ | Flora | S | 9.85 | 12.20 | LCDB · List |
| 14. | (219774) 2001 YY145 | 1007.7 | 0.86 | 2 | MBA (inner) | S | 1.54 | 16.43 | LCDB · List |
Fastest rotators
[edit]This list contains the fastest-rotating minor planets with a period of less than 100 seconds, or 0.0277 hours. Bodies with a highly uncertain period, having a quality of less than 2, are highlighted in dark-grey. The fastest rotating bodies are all unnumbered near-Earth objects (NEOs) with a diameter of less than 100 meters (see table).
Among the numbered minor planets with an unambiguous period solution are (459872) 2014 EK24, a 60-meter sized stony NEO with a period of 352 seconds, as well as (335433) 2005 UW163 and (60716) 2000 GD65, two main-belt asteroids, with a diameter of 0.86 and 2.25 kilometers and a period of 1.29 and 1.95 hours, respectively (see full list).
| # | Minor planet designation |
Rotation period | Δmag | Quality (U) |
Orbit or family |
Spectral type |
Diameter (km) |
Abs. mag (H) |
Refs | |
|---|---|---|---|---|---|---|---|---|---|---|
| (seconds) | (hours) | |||||||||
| 1. | 2014 RC | 16 | 0.004389 | 0.10 | n.a. | NEO | S | 0.012 | 26.80 | LCDB · MPC |
| 2. | 2015 SV6 | 18 | 0.00490 | 0.74 | 2 | NEO | S | 0.009 | 27.70 | LCDB · MPC |
| 3. | 2010 JL88 | 25 | 0.0068295 | 0.52 | 3 | NEO | S | 0.013 | 26.80 | LCDB · MPC |
| 4. | 2017 EK | 30 | 0.0083 | 0.30 | 2 | NEO | S | 0.045 | 24.10 | LCDB · MPC |
| 5. | 2010 WA | 31 | 0.0085799 | 0.22 | 3 | NEO | S | 0.003 | 30.00 | LCDB · MPC |
| 6. | 2017 UK8 | 31 | 0.0086309 | 1.30 | 3 | NEO | S | 0.007 | 28.20 | LCDB · MPC |
| 7. | 2016 GE1 | 34 | 0.009438 | 0.13 | 2 | NEO | S | 0.014 | 26.60 | LCDB · MPC |
| 8. | 2008 HJ | 43 | 0.01185 | 0.80 | 3− | NEO | S | 0.021 | 25.80 | LCDB · MPC |
| 9. | 2009 TM8 | 43 | 0.012 | – | n.a. | NEO | S | 0.006 | 28.40 | LCDB · MPC |
| 10. | 2015 SU | 46 | 0.0127 | 0.20 | 2− | NEO | S | 0.025 | 25.40 | LCDB · MPC |
| 11. | 2010 SK13 | 52 | 0.0144 | – | n.a. | NEO | S | 0.01 | 27.40 | LCDB · MPC |
| 12. | 2009 BF2 | 57 | 0.01593 | 0.80 | 3 | NEO | S | 0.02 | 25.90 | LCDB · MPC |
| 13. | 2016 GS2 | 66 | 0.0182725 | 0.06 | 1 | NEO | S | 0.075 | 23.00 | LCDB · MPC |
| 14. | 2010 TG19 | 70 | 0.0193935 | 1.10 | 3 | NEO | S | 0.049 | 23.90 | LCDB · MPC |
| 15. | 2008 WA14 | 70 | 0.0195 | – | n.a. | NEO | S | 0.075 | 23.00 | LCDB · MPC |
| 16. | 2007 KE4 | 77 | 0.021408 | 0.38 | 3− | NEO | S | 0.027 | 25.20 | LCDB · MPC |
| 17. | 2000 DO8 | 78 | 0.0217 | 1.39 | 3 | NEO | S | 0.037 | 24.54 | LCDB · MPC |
| 18. | 2014 GQ17 | 78 | 0.0217 | 0.08 | 2− | NEO | S | 0.011 | 27.10 | LCDB · MPC |
| 19. | 2014 TV | 79 | 0.02190 | 0.32 | 2 | NEO | S | 0.039 | 24.40 | LCDB · MPC |
| 20. | 2000 WH10 | 80 | 0.02221 | 0.66 | 3− | NEO | S | 0.094 | 22.50 | LCDB · MPC |
| 21. | 2012 HG2 | 82 | 0.0227 | – | n.a. | NEO | S | 0.012 | 27.00 | LCDB · MPC |
| 22. | 2010 TD54 | 83 | 0.0229317 | 0.92 | 3 | NEO | S | 0.005 | 28.90 | LCDB · MPC |
| 23. | 2010 TS19 | 83 | 0.023 | – | n.a. | NEO | S | 0.022 | 25.70 | LCDB · MPC |
| 24. | 2009 UD | 84 | 0.023246 | 0.66 | 2+ | NEO | S | 0.011 | 27.20 | LCDB · MPC |
| 25. | 2014 WB366 | 86 | 0.0238 | 0.46 | 2+ | NEO | S | 0.033 | 24.80 | LCDB · MPC |
| 26. | 2015 RF36 | 90 | 0.025 | 0.15 | 2 | NEO | S | 0.062 | 23.40 | LCDB · MPC |
| 27. | 2015 AK45 | 93 | 0.0258 | 0.24 | 2 | NEO | S | 0.016 | 26.40 | LCDB · MPC |
| 28. | 2010 XE11 | 96 | 0.0265846 | 0.50 | 3 | NEO | S | 0.075 | 23.00 | LCDB · MPC |
| 29. | 2000 UK11 | 96 | 0.026599 | 0.28 | 2 | NEO | S | 0.026 | 25.30 | LCDB · MPC |
| 30. | 2016 RB1 | 96 | 0.02674 | 0.18 | 2+ | NEO | S | 0.007 | 28.30 | LCDB · MPC |
| 31. | 2015 CM | 96 | 0.0268 | 0.53 | 3− | NEO | S | 0.018 | 26.10 | LCDB · MPC |
| 32. | 2008 TC3 | 97 | 0.0269409 | 1.02 | 3 | NEO | F | 0.004 | 30.90 | LCDB · MPC |
Orbital characteristics
[edit]Retrograde
[edit]Minor planets with orbital inclinations near or greater than 90° (the greatest possible is 180°) orbit in a retrograde direction. As of March 2018[update], of the near-800,000 minor planets known, there are only 99 known retrograde minor planets (0.01% of total minor planets known).[20] In comparison, there are over 2,000 comets with retrograde orbits. This makes retrograde minor planets the rarest group of all. High-inclination asteroids are either Mars-crossers (possibly in the process of being ejected from the Solar System) or damocloids. Some of these are temporarily captured in retrograde resonance with the gas giants.[21]
| Minor planet designation |
Inclination (°) | First observed/ Discovery date |
Condition code | Obs. × arc[2] | Comment | Refs |
|---|---|---|---|---|---|---|
| 2024 TF3 | 89.154° | March 8, 2010 | 40 | Extremely high-inclined trans-Neptunian object.[citation needed] | MPC | |
| 2017 UX51 | 90.517° | October 27, 2017 | 0 | 79254 | — | MPC |
| 2018 SQ13 | 90.973° | September 21, 2018 | 17407 | — | MPC | |
| 2015 TN178 | 91.093° | October 8, 2015 | 0 | 38805 | — | MPC |
| 2005 SB223 | 91.294° | September 30, 2005 | 1 | 12200 | Has a well-determined orbit | MPC |
| 2014 MH55 | 91.486° | June 29, 2014 | 6 | 96 | — | MPC |
| 2010 EQ169 | 91.607° | March 8, 2010 | ? | 15 | Most highly inclined known main-belt asteroid (orbit is not well-known)[citation needed] | MPC |
| 2015 RK245 | 91.616° | September 13, 2015 | 0 | 184680 | — | MPC |
| 2016 TK2 | 92.336° | July 13, 2016 | 2 | 6075 | — | MPC |
| (518151) 2016 FH13 | 93.551° | March 29, 2016 | 0 | 91561 | — | MPC |
| 2014 PP69 | 93.652° | August 5, 2014 | 1 | 8085 | — | MPC |
| 2015 BH311 | 94.160° | January 20, 2015 | ? | 39 | — | MPC |
| 2017 OX68 | 94.748° | July 26, 2017 | 8720 | — | MPC | |
| 2014 JJ57 | 95.924° | May 9, 2014 | 0 | 95710 | — | MPC |
| 2013 HS150 | 97.434° | April 16, 2013 | 220 | — | MPC | |
| (709487) 2013 BL76 | 98.592° | January 20, 2013 | 46716 | Has a semi-major axis of 1254 AU, giving it the third largest semi-major axis of any known minor planet | MPC | |
| 2010 GW147 | 99.835° | April 14, 2010 | 0 | 97888 | — | MPC |
| 2011 MM4 | 100.482° | June 24, 2011 | 0 | 364936 | — | MPC |
| 2017 NM2 | 101.295° | July 6, 2017 | 1 | 28014 | — | MPC |
| 2014 XS3 | 101.381° | December 8, 2014 | 0 | 23544 | — | MPC |
| 2013 BN27 | 101.828° | January 17, 2013 | 1400 | — | MPC | |
| (528219) 2008 KV42 | 103.396° | May 31, 2008 | 1 | 198550 | — | MPC |
| (342842) 2008 YB3 | 105.058° | December 18, 2008 | 0 | 1608789 | — | MPC |
| 2016 PN66 | 105.113° | August 14, 2016 | 0 | 63879 | — | MPC |
| 2010 GW64 | 105.226° | April 6, 2010 | 0 | 9072 | — | MPC |
| 2012 YO6 | 106.883° | December 22, 2012 | 3 | 6674 | — | MPC |
| 2009 DD47 | 107.449° | February 27, 2009 | ? | 1584 | — | MPC |
| 2017 UR52 | 108.218° | October 29, 2017 | 1638 | — | MPC | |
| 2007 VW266 | 108.328° | November 12, 2007 | 5 | 2204 | — | MPC |
| 2011 SP25 | 109.074° | September 20, 2011 | 3 | 3654 | — | MPC |
| 471325 Taowu | 110.104° | May 31, 2011 | 1 | 234828 | — | MPC |
| 2005 TJ50 | 110.226° | October 5, 2005 | 5 | 1488 | — | MPC |
| 2011 OR17 | 110.504° | May 21, 2010 | 71808 | — | MPC | |
| 2005 VX3 | 112.224° | November 1, 2005 | 4212 | Semi-major axis of 837AU, but has a somewhat short 81-day observation arc for such a large orbit | MPC | |
| 2017 SV13 | 113.243° | September 17, 2017 | 4 | 2160 | — | MPC |
| 2016 LS | 114.338° | June 27, 2015 | 0 | 26688 | — | MPC |
| 2015 YY18 | 118.243° | December 29, 2015 | 0 | 33454 | — | MPC |
| 2010 OM101 | 118.797° | July 28, 2010 | 2 | 3535 | — | MPC |
| (65407) 2002 RP120 | 118.970° | September 4, 2002 | 0 | 648554 | This outer-planet crosser is a damocloid and SDO. | MPC |
| 2010 PO58 | 121.179° | August 5, 2010 | 8 | 120 | — | MPC |
| 2010 LG61 | 123.886° | June 2, 2010 | 7 | 935 | — | MPC |
| (468861) 2013 LU28 | 125.356° | June 8, 2013 | 0 | 238336 | — | MPC |
| 2014 SQ339 | 128.506° | September 29, 2014 | 4 | 1334 | — | MPC |
| 2000 DG8 | 129.246° | February 25, 2000 | 2 | 42408 | A damocloid and SDO. Crosses all the outer planets except Neptune. Came within 0.03 AU of Ceres in 1930.[22] | MPC |
| 2016 CO264 | 129.820° | February 14, 2016 | 0 | 23800 | — | MPC |
| 2013 NS11 | 130.333° | July 5, 2013 | 0 | 143510 | — | MPC |
| 2005 NP82 | 130.505° | July 6, 2005 | 1 | 662673 | — | MPC |
| 2006 RG1 | 133.437° | September 1, 2006 | 4 | 750 | Has an orbit with a data arc of 25 days | MPC |
| 2012 YE8 | 136.049° | December 21, 2012 | 5 | 1066 | — | MPC |
| 2017 AX13 | 137.204° | January 2, 2017 | 3 | 1785 | — | MPC |
| 2009 QY6 | 137.668° | August 17, 2009 | 1 | 43990 | — | MPC |
| 2016 TP93 | 138.330° | October 9, 2016 | ? | 704 | — | MPC |
| 2016 YB13 | 139.682° | December 23, 2016 | 1 | 50718 | — | MPC |
| 2019 EJ3 | 139.758° | March 4, 2019 | ? | 576 | — | MPC |
| 2015 AO44 | 139.934° | November 27, 2014 | 0 | 115821 | — | MPC |
| (336756) 2010 NV1 | 140.773° | July 1, 2010 | 0 | 330022 | Perihelion at 9.4 AU, only 2008 KV42 has perihelion further out (154-day data arc) | MPC |
| 2011 WS41 | 141.645° | November 24, 2011 | ? | 108 | — | MPC |
| 2010 OR1 | 143.912° | January 25, 2010 | 1 | 35032 | — | MPC |
| 2010 BK118 | 143.914° | January 30, 2010 | 374596 | Semi-major axis of 408 AU with perihelion at 6.1 AU in April 2012 (1 year data arc) | MPC | |
| (523797) 2016 NM56 | 144.034° | November 1, 2012 | 0 | 227052 | — | MPC |
| 2017 UW51 | 144.203° | October 23, 2017 | 68442 | — | MPC | |
| 2010 CG55 | 146.262° | February 15, 2010 | 0 | 129000 | — | MPC |
| 2012 HD2 | 146.883° | April 18, 2012 | 0 | 31408 | — | MPC |
| 2009 YS6 | 147.767° | December 17, 2009 | 0 | 195734 | — | MPC |
| 2016 VY17 | 148.419° | November 5, 2016 | 0 | 108624 | — | MPC |
| 2017 QO33 | 148.826° | August 16, 2017 | 1 | 45360 | — | MPC |
| 2006 EX52 | 150.148° | March 5, 2006 | 0 | 62310 | q=2.58 AU and period=274 yr | MPC |
| (612093) 1999 LE31 | 151.816° | June 12, 1999 | 2 | 905838 | A damocloid, Jupiter- and Saturn-crossing minor planet.[23] | MPC |
| 2017 SN33 | 152.044° | September 19, 2017 | 7590 | — | MPC | |
| 2018 WB1 | 152.136° | November 19, 2018 | 7 | 351 | — | MPC |
| 2016 JK24 | 152.326° | March 3, 2016 | 0 | 181965 | — | MPC |
| 2017 CW32 | 152.438° | February 2, 2017 | 51500 | — | MPC | |
| 343158 Marsyas | 154.367° | April 29, 2009 | 0 | 771834 | NEO that sometimes has the highest relative velocity to Earth (79 km/s) of known objects that come within 0.5 AU of Earth. However, the relative velocity at 1 AU from the sun is less than 72 km/s. | MPC |
| 2013 LD16 | 154.736° | June 6, 2013 | 0 | 14148 | — | MPC |
| 2021 TH165 | 154.924° | October 11, 2021 | 3 | 2510 | Retrograde trans-Neptunian object close to a 3:–2 mean-motion orbital resonance with Neptune. | MPC |
| 2015 FK37 | 155.842° | March 20, 2015 | ? | 748 | — | MPC |
| 2010 EB46 | 156.376° | March 12, 2010 | 4 | 2460 | — | MPC |
| 2015 XR384 | 157.514° | December 9, 2015 | 2 | 5580 | — | MPC |
| 2000 HE46 | 158.535° | April 29, 2000 | 2 | 25960 | — | MPC |
| 2015 XX351 | 159.092° | December 9, 2015 | 0 | 21120 | — | MPC |
| 2012 TL139 | 160.027° | October 9, 2012 | 3 | 900 | — | MPC |
| 2019 CR | 160.341° | February 4, 2019 | 1 | 36993 | — | MPC |
| 20461 Dioretsa | 160.428° | June 8, 1999 | 0 | 256779 | most highly inclined known minor planet from June 8, 1999, to July 13, 2004 | MPC |
| 2018 DO4 | 160.475° | February 25, 2018 | 0 | 261726 | — | MPC |
| 2017 JB6 | 160.735° | May 4, 2017 | ? | 6844 | — | MPC |
| (523800) 2017 KZ31 | 161.695° | June 23, 2015 | 0 | 119280 | — | MPC |
| 514107 Kaʻepaokaʻāwela | 163.022° | November 26, 2014 | 0 | 74898 | A Jupiter co-orbital. First known example of a retrograde co-orbital asteroid with any of the planets. Might have an interstellar origin. | MPC Src |
| 2006 RJ2 | 164.601° | September 14, 2006 | 5 | 2849 | — | MPC |
| 2006 BZ8 | 165.311° | January 23, 2006 | 0 | 207459 | — | MPC |
| 2004 NN8 | 165.525° | July 13, 2004 | 23944 | Came within 0.80 AU of Saturn on 2007-Jun-05, most highly inclined known minor planet from 2004/07/13-2005/11/01 | MPC | |
| (459870) 2014 AT28 | 165.558° | November 26, 2013 | 0 | 186598 | — | MPC |
| 2016 DF2 | 167.030° | February 28, 2016 | ? | 26 | — | MPC |
| (330759) 2008 SO218 | 170.324° | September 30, 2008 | 0 | 1058616 | — | MPC |
| 2014 UV114 | 170.569° | October 26, 2014 | ? | 34 | — | MPC |
| 2014 CW14 | 170.764° | February 10, 2014 | 4 | 1938 | — | MPC |
| 2018 TL6 | 170.919° | October 5, 2018 | 7 | 270 | — | MPC |
| 2016 EJ203 | 170.988° | March 11, 2016 | 0 | 18081 | — | MPC |
| 2006 LM1 | 172.138° | June 3, 2006 | ? | 48 | Has a data arc of only 2 days, but has a very high inclination | MPC |
| (434620) 2005 VD | 172.872° | November 1, 2005 | 0 | 228965 | most highly inclined known minor planet from November 1, 2005, to June 1, 2013 | MPC |
| 2013 LA2 | 175.095° | June 1, 2013 | 6 | 1075 | Has the highest inclination of any known minor planet | MPC |
^ the value given when the number of observations is multiplied by the observation arc; larger values are generally better than smaller values depending on residuals.
Highly inclined
[edit]| Minor planet designation | Inclination | Discovery date | Comment | Refs |
|---|---|---|---|---|
| 1 Ceres | 10.593° | January 1, 1801 | most highly inclined known minor planet from January 1, 1801, to March 28, 1802 | MPC |
| 2 Pallas | 34.841° | March 28, 1802 | most highly inclined known minor planet from March 28, 1802, to October 31, 1920 | MPC |
| 944 Hidalgo | 42.525° | October 31, 1920 | most highly inclined known minor planet from October 31, 1920, to May 22, 1950 | MPC |
| 1373 Cincinnati | 38.949° | August 30, 1935 | First main-belt asteroid discovered to have an inclination greater than 2 Pallas. Most highly inclined known main-belt asteroid from August 30, 1935, to June 14, 1980 | MPC |
| 1580 Betulia | 52.083° | May 22, 1950 | most highly inclined known minor planet from May 22, 1950, to July 4, 1973 | MPC |
| 2938 Hopi | 41.436° | June 14, 1980 | Most highly inclined known main-belt asteroid from June 14, 1980, to September 20, 2000 | MPC |
| (5496) 1973 NA | 67.999° | July 4, 1973 | An Apollo asteroid, Mars-crosser and +1 km NEO; most highly inclined known minor planet from 4 July 1973 to 8 August 1999. | MPC |
| (22653) 1998 QW2 | 45.794° | August 17, 1998 | Most highly inclined known main-belt asteroid from August 17, 1998, to October 19, 1998 | MPC |
| (88043) 2000 UE110 | 51.998° | October 29, 2000 | First main-belt asteroid discovered and numbered to have an inclination greater than 50°. | MPC |
| (138925) 2001 AU43 | 72.132° | January 4, 2001 | A Mars-crosser and near-Earth object. | MPC |
| (127546) 2002 XU93 | 77.904° | December 4, 2002 | A damocloid and SDO. It is almost a Uranus outer-grazer. | MPC |
| (196256) 2003 EH1 | 70.790° | March 6, 2003 | A Mars-crosser, near-Earth object and Jupiter inner-grazer. | MPC |
| 1998 UQ1 | 64.281° | October 19, 1998 | Most highly inclined known main-belt asteroid from 1998/10/19-2007/11/01 | MPC |
| (467372) 2004 LG | 70.725° | June 9, 2004 | A Mercury- through Mars-crosser and near-Earth object. | MPC |
| 2007 VR6 | 68.659° | November 1, 2007 | Most highly inclined known main-belt asteroid from November 1, 2007, to September 26, 2008 | MPC |
| 2008 SB85 | 74.247° | September 26, 2008 | Most highly inclined known main-belt asteroid from September 26, 2008, to March 8, 2010[citation needed] | MPC |
Trojans
[edit]- Earth trojans: (706765) 2010 TK7 and (614689) 2020 XL5.
- Mars trojans: (121514) 1999 UJ7, 5261 Eureka, (101429) 1998 VF31, (311999) 2007 NS2, (385250) 2001 DH47, 2011 SC191, 2011 UN63, and the candidate 2011 SL25.
- Jupiter trojans: the first one was discovered in 1906, 588 Achilles, and the current total is over 15,000.
Record-setting close approaches to Earth
[edit]Viewed in detail
[edit]Spacecraft targets
[edit]| Name | Diameter (km) |
Discovered | Spacecraft | Year(s) | Closest approach (km) |
Closest approach (asteroid radii) |
Notes | Landmark(s) |
|---|---|---|---|---|---|---|---|---|
| 1 Ceres | 939.4 | January 1, 1801 | Dawn | 2014–2018 | 375 | 0.80 | Dawn took its first "close up" picture of Ceres in December 2014, and entered orbit in March 2015 | First likely dwarf planet visited by a spacecraft, largest asteroid visited by a spacecraft |
| 4 Vesta | 525.4 | March 29, 1807 | Dawn | 2011–2012 | 210 | 0.76 | Dawn broke orbit on 5 September 2012 and headed to Ceres, where it arrived in March 2015 | First "big four" asteroid visited by a spacecraft, largest asteroid visited by a spacecraft at the time |
| 21 Lutetia | 120×100×80 | November 15, 1852 | Rosetta | 2010 | 3,162 | 64.9 | Flyby on 10 July 2010 | Largest asteroid visited by a spacecraft at the time |
| 243 Ida | 56×24×21 | September 29, 1884 | Galileo | 1993 | 2,390 | 152 | Flyby; discovered Dactyl | First asteroid with a moon visited by a spacecraft, largest asteroid visited by spacecraft at the time |
| 253 Mathilde | 66×48×46 | November 12, 1885 | NEAR Shoemaker | 1997 | 1,212 | 49.5 | Flyby | Largest asteroid visited by a spacecraft at the time |
| 433 Eros | 13×13×33 | August 13, 1898 | NEAR Shoemaker | 1998–2001 | 0 | 0 | 1998 flyby; 2000 orbited (first asteroid studied from orbit); 2001 landing | First asteroid landing, first asteroid orbited by a spacecraft, first near-Earth asteroid (NEA) visited by a spacecraft |
| 951 Gaspra | 18.2×10.5×8.9 | July 30, 1916 | Galileo | 1991 | 1,600 | 262 | Flyby | First asteroid visited by a spacecraft |
| 2867 Šteins | 4.6 | November 4, 1969 | Rosetta | 2008 | 800 | 302 | Flyby | First asteroid visited by the ESA |
| 4179 Toutatis | 4.5×~2 | February 10, 1934 | Chang'e 2 | 2012 | 3.2 | 0.70 | Flyby[24] | Closest asteroid flyby, first asteroid visited by China |
| 5535 Annefrank | 4.0 | March 23, 1942 | Stardust | 2002 | 3,079 | 1230 | Flyby | |
| 9969 Braille | 2.2×0.6 | May 27, 1992 | Deep Space 1 | 1999 | 26 | 12.7 | Flyby; followed by flyby of Comet Borrelly | |
| 25143 Itokawa | 0.5×0.3×0.2 | September 26, 1998 | Hayabusa | 2005 | 0 | 0 | Landed; returned dust samples to Earth | First asteroid with returned samples, smallest asteroid visited by a spacecraft, first asteroid visited by a non-NASA spacecraft |
| 162173 Ryugu | 1.0 | May 10, 1999 | Hayabusa2 | 2018–2019 | 0 | 0 | Multiple landers/rovers, sample return | First rovers on an asteroid |
| 101955 Bennu | 0.492 | September 11, 1999 | OSIRIS-REx | 2018–2021 | 0 | 0 | Sample return | Smallest asteroid orbited, potentially hazardous object |
| 65803 Didymos | 0.492 | September 11, 1999 | DART/LICIACube | 2022 | 1.2 | 3.2 | Impactor/flyby | Moon Dimorphos impacted by DART spacecraft, flown by LICIACube |
| 152830 Dinkinesh | 0.790 | October 15, 1999 | Lucy | 2023 | 425 | 1076 | Flyby; first of 8 planned asteroid flybys | Smallest main-belt asteroid visited to date; discovered first contact binary satellite Selam |
| 52246 Donaldjohanson | 3.9 | March 2, 1981 | Lucy | 2025 | 960 | 240 | Flyby; second of 8 planned asteroid flybys |
Surface resolved by telescope or lightcurve
[edit]- 1 Ceres
- 2 Pallas
- 3 Juno
- 4 Vesta
- 5 Astraea
- 6 Hebe
- 7 Iris
- 8 Flora
- 9 Metis
- 10 Hygiea
- 12 Victoria
- 13 Egeria
- 14 Irene
- 15 Eunomia
- 16 Psyche
- 18 Melpomene
- 26 Proserpina
- 29 Amphitrite
- 35 Leukothea
- 37 Fides
- 51 Nemausa
- 52 Europa
- 65 Cybele
- 87 Sylvia
- 89 Julia
- 121 Hermione
- 130 Elektra
- 201 Penelope
- 216 Kleopatra
- 324 Bamberga
- 511 Davida
- 925 Alphonsina
- 1140 Crimea
- 9969 Braille
- (33342) 1998 WT24
- 66391 Moshup
- (136617) 1994 CC
- (285263) 1998 QE2
- (357439) 2004 BL86
Multiple systems resolved by telescope
[edit]Comet-like activity
[edit]Disintegration
[edit]Timeline
[edit]Landmark asteroids
[edit]| Name | Diameter (km) | Discovered | Comment |
|---|---|---|---|
| 1 Ceres | 939 | January 1, 1801 | First asteroid discovered |
| 5 Astraea | 117 | December 8, 1845 | First asteroid discovered after original four (38 years later) |
| 20 Massalia | 136 | September 19, 1852 | First asteroid named after city |
| 45 Eugenia | 202 | June 27, 1857 | First asteroid named after living person |
| 87 Sylvia | 261 | May 16, 1866 | First asteroid known to have more than one moon (determined in 2005) |
| 90 Antiope | 80×80 | October 1, 1866 | Double asteroid with two nearly equal components; its double nature was discovered using adaptive optics in 2000 |
| 216 Kleopatra | 217×94 | April 10, 1880 | Metallic asteroid with "ham-bone" shape and 2 satellites |
| 243 Ida | 56×24×21 | September 29, 1884 | First asteroid known to have a moon (determined in 1994) |
| 243 Ida I Dactyl | 1.4 | February 17, 1994 | Moon of 243 Ida, first confirmed satellite of an asteroid |
| 279 Thule | 127 | October 25, 1888 | Orbits in the asteroid belt's outermost edge in a 3:4 orbital resonance with Jupiter |
| 288 Glauke | 32 | February 20, 1890 | Exceptionally slow rotation period of about 1200 hours (2 months) |
| 323 Brucia | 36 | December 22, 1891 | First asteroid discovered by means of astrophotography rather than visual observation |
| 433 Eros | 13×13×33 | August 13, 1898 | First near-Earth asteroid discovered and the second largest; first asteroid to be detected by radar; first asteroid orbited and landed upon |
| 482 Petrina | 23.3 | March 3, 1902 | First asteroid named after dog |
| 490 Veritas | 115 | September 3, 1902 | Created in one of the largest asteroid-on-asteroid collisions of the past 100 million years |
| 588 Achilles | 135.5 | February 22, 1906 | First Jupiter trojan discovered |
| 624 Hektor | 370×195 | February 10, 1907 | Largest Jupiter trojan discovered |
| 719 Albert | 2.4 | October 3, 1911 | Last numbered asteroid to be lost then recovered |
| 935 Clivia | 6.4 | September 7, 1920 | First asteroid named after flower |
| 1090 Sumida | 13 | February 20, 1928 | Lowest numbered asteroid with no English Wikipedia entry |
| 1125 China | 27 | October 30, 1957 | First asteroid discovery to be credited to an institution rather than a person |
| 1566 Icarus | 1.4 | June 27, 1949 | First Mercury crosser discovered |
| 2309 Mr. Spock | 21.3 | August 16, 1971 | First asteroid named after cat |
| 3200 Phaethon | 5 | October 11, 1983 | First asteroid discovered from space; source of Geminids meteor shower. |
| 3753 Cruithne | 5 | October 10, 1986 | Unusual Earth-associated orbit |
| 4179 Toutatis | 4.5×2.4×1.9 | January 4, 1989 | Closely approached Earth on September 29, 2004 |
| 4769 Castalia | 1.8×0.8 | August 9, 1989 | First asteroid to be radar-imaged in sufficient detail for 3D modeling[25] |
| 5261 Eureka | ~2–4 | June 20, 1990 | First Mars trojan (Lagrangian point L5) discovered |
| 11885 Summanus | 1.3 | September 25, 1990 | First automated discovery of a near-Earth object (NEO) |
| (29075) 1950 DA | 1.1 | February 23, 1950 | Small chance to collide with Earth in 2880 (1 in 2,600 or 0.039%)[26] |
| 69230 Hermes | 0.3 | October 28, 1937 | Named but not numbered until its recovery in 2003 (65 years later) |
| 99942 Apophis | 0.3 | June 19, 2004 | First asteroid to rank greater than one on the Torino Scale (it was ranked at 2, then 4; now down to 0). Previously better known by its provisional designation 2004 MN4. |
| 152830 Dinkinesh I Selam | 0.22 | November 1, 2023 | First satellite discovered to be a contact-binary |
| (433953) 1997 XR2 | 0.23 | December 4, 1997 | First asteroid to rank greater than zero on the impact-risk Torino Scale (it was ranked 1; now at 0) |
| 1998 KY26 | 0.030 | June 2, 1998 | Approached within 800,000 km of Earth |
| 2002 AA29 | 0.1 | January 9, 2002 | Unusual Earth-associated orbit |
| 2004 FH | 0.030 | March 15, 2004 | Discovered before it approached within 43,000 km of Earth on March 18, 2004. |
| 2008 TC3 | ~0.003 | October 6, 2008 | First Earth-impactor to be spotted before impact (on October 7, 2008) |
| (706765) 2010 TK7 | ~0.3 | October 2010 | First Earth trojan to be discovered |
| 2014 RC | ~0.017 | September 1, 2014 | Asteroid with fastest rotation: 16.2 seconds |
Numbered minor planets that are also comets
[edit]| Name | Cometary name | Comment |
|---|---|---|
| 2060 Chiron | 95P/Chiron | First centaur discovered in 1977, later identified to exhibit cometary behaviour. Also one of two minor planets (excluding dwarf planets) known to have a ring system |
| 4015 Wilson–Harrington | 107P/Wilson–Harrington | In 1992, it was realized that asteroid 1979 VA's orbit matched it with the positions of the lost comet Wilson–Harrington (1949 III) |
| 7968 Elst–Pizarro | 133P/Elst–Pizarro | Discovered in 1996 as a comet, but orbitally matched to asteroid 1979 OW7 |
| 60558 Echeclus | 174P/Echeclus | Centaur discovered in 2000, comet designation assigned in 2006 |
| 118401 LINEAR | 176P/LINEAR (LINEAR 52) | Main-belt comet–asteroid discovered to have a coma on November 26, 2005 |
The above table lists only numbered asteroids that are also comets. Note there are several cases where a non-numbered minor planets turned out to be a comet, e.g. C/2001 OG108 (LONEOS), which was provisionally designated 2001 OG108.
Minor planets that were misnamed and renamed
[edit]In earlier times, before the modern numbering and naming rules were in effect, asteroids were sometimes given numbers and names before their orbits were precisely known. And in a few cases duplicate names were given to the same object (with modern use of computers to calculate and compare orbits with old recorded positions, this type of error no longer occurs). This led to a few cases where asteroids had to be renamed.[27]
| Minor planet name | Description |
|---|---|
| 330 Adalberta | An object discovered March 18, 1892, by Max Wolf with provisional designation "1892 X" was named 330 Adalberta, but was lost and never recovered. In 1982 it was determined that the observations leading to the designation of 1892 X were stars, and the object never existed. The name and number 330 Adalberta was then reused for another asteroid discovered by Max Wolf on February 2, 1910, which had the provisional designation A910 CB. |
| 525 Adelaide and 1171 Rusthawelia | The object A904 EB discovered March 14, 1904, by Max Wolf was named 525 Adelaide and was subsequently lost. Later, the object 1930 TA discovered October 3, 1930, by Sylvain Arend was named 1171 Rusthawelia. In those pre-computer days, it was not realized until 1958 that these were one and the same object. The name Rusthawelia was kept (and discovery credited to Arend); the name 525 Adelaide was reused for the object 1908 EKa discovered October 21, 1908, by Joel Hastings Metcalf. |
| 715 Transvaalia and 933 Susi | The object 1911 LX discovered April 22, 1911, by H. E. Wood was named 715 Transvaalia. On April 23, 1920, the object 1920 GZ was discovered and named 933 Susi. In 1928 it was realized that these were one and the same object. The name Transvaalia was kept, and the name and number 933 Susi was reused for the object 1927 CH discovered February 10, 1927, by Karl Reinmuth. |
| 864 Aase and 1078 Mentha | The object A917 CB discovered February 13, 1917, by Max Wolf was named 864 Aase, and the object 1926 XB discovered December 7, 1926, by Karl Reinmuth was named 1078 Mentha. In 1958 it was discovered that these were one and the same object. In 1974, this was resolved by keeping the name 1078 Mentha and reusing the name and number 864 Aase for the object 1921 KE, discovered September 30, 1921, by Karl Reinmuth. |
| 1095 Tulipa and 1449 Virtanen | The object 1928 DC discovered February 24, 1928, by Karl Reinmuth was named 1095 Tulipa, and the object 1938 DO discovered February 20, 1938, by Yrjö Väisälä was named 1449 Virtanen. In 1966 it was discovered that these were one and the same object. The name 1449 Virtanen was kept and the name and number 1095 Tulipa was reused for the object 1926 GS discovered April 14, 1926, by Karl Reinmuth. |
| 1125 China and 3789 Zhongguo | The object 1928 UF discovered October 25, 1928, by Zhang Yuzhe (Y. C. Chang) was named 1125 China, and was later lost. Later, the object 1957 UN1 was discovered on October 30, 1957, at Purple Mountain Observatory and was initially incorrectly believed to be the rediscovery of the object 1928 UF. The name and number 1125 China were then reused for the object 1957 UN1, and 1928 UF remained lost. In 1986, the object 1986 QK1 was discovered and proved to be the real rediscovery of 1928 UF. This object was given the new number and name 3789 Zhongguo. Note Zhongguo is the Mandarin Chinese word for "China", in pinyin transliteration. |
| Asteroid 1317 and 787 Moskva | The object 1914 UQ discovered April 20, 1914, by G. N. Neujmin was named 787 Moskva (and retains that name to this day). The object 1934 FD discovered on March 19, 1934, by C. Jackson was given the sequence number 1317. In 1938, G. N. Neujmin found that asteroid 1317 and 787 Moskva were one and the same object. The sequence number 1317 was later reused for the object 1935 RC discovered on September 1, 1935, by Karl Reinmuth; that object is now known as 1317 Silvretta. |
Landmark names
[edit]Asteroids were originally named after female mythological figures. Over time the rules loosened.
First asteroid with non-Classical and non-Latinized name: 64 Angelina (in honor of a research station)
First asteroid with a non-feminine name: 139 Juewa (ambiguous) or 141 Lumen
First asteroid with a non-feminized man's name: 433 Eros
Lowest-numbered unnamed asteroid (As of 2024[update]): (4596) 1981 QB
Landmark numbers
[edit]Many landmark numbers had specially chosen names for asteroids, and there was some debate about whether Pluto should have received number 10000, for example. This list includes some non-asteroids.
See also
[edit]- List of minor planets
- List of minor planets named after people
- List of minor planets named after places
- List of instrument-resolved minor planets
- List of minor planet moons
- List of Mercury-crossing minor planets
- List of Venus-crossing minor planets
- List of Earth-crossing asteroids
- List of Mars-crossing minor planets
- List of Jupiter-crossing minor planets
- List of Saturn-crossing minor planets
- List of Uranus-crossing minor planets
- List of Neptune-crossing minor planets
- List of Solar System objects by size
- Lists of astronomical objects
- List of predicted asteroid impacts on Earth
- Small Solar System body
- Amor asteroid
- Apollo asteroid
- Aten asteroid
- Atira asteroid
- Centaur (small Solar System body)
- ʻOumuamua
Books
[edit]- Dictionary of Minor Planet Names, 5th ed.: Prepared on Behalf of Commission 20 Under the Auspices of the International Astronomical Union, Lutz D. Schmadel, ISBN 3-540-00238-3
References
[edit]- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab P. Vernazza et al. (2021) VLT/SPHERE imaging survey of the largest main-belt asteroids: Final results and synthesis. Astronomy & Astrophysics 54, A56
- ^ As of Jan 2019, good rotational coverage (≥ 4 epochs) had also been obtained for 476 Hedwig and 596 Scheila.[1]
- ^ a b c M. Pajuelo, Benoit Carry, Frédéric Vachier, Michael Marsset et al. (March 2018) Physical, spectral, and dynamical properties of asteroid (107) Camilla and its satellites, Icarus 309
- ^ "Small-Body Database Lookup".
- ^ Hanuš, J.; Marsset, M.; Vernazza, P.; Viikinkoski, M.; Drouard, A.; Brož, M.; et al. (24 April 2019). "The shape of (7) Iris as evidence of an ancient large impact?". Astronomy & Astrophysics. 624 (A121): A121. arXiv:1902.09242. Bibcode:2018DPS....5040406H. doi:10.1051/0004-6361/201834541. S2CID 119089163.
- ^ "JPL Small-Body Database Search Engine: asteroids and orbital class (IMB or MBA or OMB) and diameter > 120 (km)". JPL Solar System Dynamics. Retrieved 2012-04-16.
- ^ Bottkejr, W; Durda, D; Nesvorny, D; Jedicke, R; Morbidelli, A; Vokrouhlicky, D; Levison, H (May 2005). "The fossilized size distribution of the main asteroid belt". Icarus. 175 (1): 111–140. Bibcode:2005Icar..175..111B. doi:10.1016/j.icarus.2004.10.026.
- ^ "NASA Astrobiology".
- ^ "Recent Asteroid Mass Determinations" Archived 2013-07-02 at the Wayback Machine. Maintained by Jim Baer. Last updated 2010-12-12. Access date 2011-09-02.
- ^ Baer, James; Steven R. Chesley (2008). "Astrometric masses of 21 asteroids, and an integrated asteroid ephemeris". Celestial Mechanics and Dynamical Astronomy. 100 (2008). Springer Science+Business Media: 27–42. Bibcode:2008CeMDA.100...27B. doi:10.1007/s10569-007-9103-8.
- ^ assuming a total Main Belt mass of 2394×1018 kg. The mass of Herculina is particularly uncertain
- ^ F. Marchis; et al. (2005). "Discovery of the triple asteroidal system 87 Sylvia" (PDF). Nature. 436 (7052): 822–4. Bibcode:2005Natur.436..822M. doi:10.1038/nature04018. PMID 16094362. S2CID 4412813
- ^ Pitjeva, E. V. (May 2005). "High-Precision Ephemerides of Planets—EPM and Determination of Some Astronomical Constants". Solar System Research. 39 (3). Springer Science+Business Media: 184. Bibcode:2005SoSyR..39..176P. CiteSeerX 10.1.1.475.9201. doi:10.1007/s11208-005-0033-2. S2CID 120467483.
- ^ Berdeu, Anthony; Langlois, Maud; Vachier, Frédéric (February 2021). "First observation of a quadruple asteroid. Detection of a third moon around (130) Elektra with SPHERE/IFS". Astronomy & Astrophysics. 658: 21.
- ^ Michalak, G. (2001). "Determination of asteroid masses". Astronomy & Astrophysics. 374 (2): 703–711. Bibcode:2001A&A...374..703M. doi:10.1051/0004-6361:20010731. Retrieved 2008-11-10.
- ^ Michalak, G. (2001), assumed masses of perturbing asteroids used in calculations of perturbations of the test asteroids.[clarification needed]
- ^ Martinez, Patrick (1994). The Observer's Guide to Astronomy. Cambridge University Press. p. 298.
- ^ "(99942) Apophis Ephemerides for 13 Apr 2029". NEODyS (Near Earth Objects Dynamic Site). Retrieved 2011-05-05.
- ^ "Minor Planet Ephemeris Service: Query Results". Minor Planet Center.
- ^ "JPL Small-Body Database Search Engine: Asteroids and i > 90 (deg)". JPL Solar System Dynamics. Retrieved 2019-03-31.
- ^ Morais, M.H.M.; F. Namouni (2013). "Asteroids in retrograde resonance with Jupiter and Saturn". Monthly Notices of the Royal Astronomical Society Letters. 436: L30 – L34. arXiv:1308.0216. Bibcode:2013MNRAS.436L..30M. doi:10.1093/mnrasl/slt106.
- ^ 2008 DG8 and Ceres in 1930
- ^ 1999 LE31 approaches to Jupiter and Saturn
- ^ Chang'E 2 images of Toutatis – December 13, 2012 – The Planetary Society
- ^ "1994 Release #9412" (Press release). NASA. 1994-02-18. Retrieved 2008-04-17.
- ^ "Sentry: Earth Impact Monitoring | 29075 (1950 DA) Earth Impact Risk Summary". JPL Center for Near Earth Object Studies. 24 January 2025. Retrieved 31 January 2025.
- ^ "Archived copy". Archived from the original on 2004-07-03. Retrieved 2004-04-27.
{{cite web}}: CS1 maint: archived copy as title (link)
External links
[edit]List of exceptional asteroids
View on GrokipediaPhysical Properties
Largest by Size and Mass
The sizes of asteroids are primarily determined through a combination of techniques, including stellar occultations, which provide precise silhouettes by observing the temporary dimming of background stars as the asteroid passes in front; radar ranging, which bounces radio waves off the surface to measure distances and derive shapes; and infrared thermal modeling, which infers diameters from the emitted heat radiation captured by telescopes like IRAS, AKARI, and WISE, assuming standard thermal properties.[7] Masses, on the other hand, are estimated via gravitational perturbations observed in the orbits of nearby bodies, such as Mars or smaller asteroids during close encounters, allowing astronomers to solve for the perturbing body's mass using dynamical models.[8] Among asteroids, the largest by mean volume-equivalent diameter are predominantly found in the main belt, with sizes derived from high-resolution imaging and modeling revealing irregular shapes for most. The top 10, based on recent adaptive optics observations from the VLT/SPHERE instrument (no significant updates as of 2025), include bodies ranging from highly elongated to nearly spherical forms, with estimated volumes calculated from 3D shape models and densities reflecting compositional variations. For instance, (4) Vesta has a mean diameter of 525 km and volume of approximately 7.6 × 10^7 km³, yielding a density of 3.46 g/cm³ indicative of a differentiated structure; (2) Pallas measures 512 km in diameter with a volume of about 7.0 × 10^7 km³ and density of 2.77 g/cm³, suggesting a more primitive, icy composition; and (10) Hygiea, at 434 km diameter and volume of 4.3 × 10^7 km³, has a lower density of around 2.18 g/cm³, consistent with a porous, carbonaceous makeup. These measurements highlight how larger asteroids often exhibit lower macroporosities compared to smaller ones, influencing their overall structural integrity.[9]| Rank | Asteroid | Mean Diameter (km) | Estimated Volume (×10^7 km³) | Density (g/cm³) |
|---|---|---|---|---|
| 1 | (4) Vesta | 525 | 7.6 | 3.46 |
| 2 | (2) Pallas | 512 | 7.0 | 2.77 |
| 3 | (10) Hygiea | 434 | 4.3 | 2.18 |
| 4 | (511) Davida | 326 | 1.8 | 2.54 |
| 5 | (704) Interamnia | 316 | 1.7 | 2.20 |
| 6 | (52) Europa | 302 | 1.4 | 2.72 |
| 7 | (87) Sylvia | 273 | 1.1 | 1.20 |
| 8 | (107) Camilla | 248 | 0.8 | 1.27 |
| 9 | (324) Bamberga | 235 | 0.7 | 2.21 |
| 10 | (121) Hermione | 228 | 0.6 | 1.40 |
Brightest and Most Visible
The absolute magnitude of an asteroid is defined as the visual magnitude it would exhibit if positioned 1 AU from the Sun, 1 AU from the observer, and at a phase angle of 0 degrees, providing a standardized measure of its intrinsic brightness independent of distance and viewing geometry.[13] Lower values indicate brighter asteroids, which appear more prominent from Earth during opposition when they are closest to our line of sight from the Sun. This metric correlates with an asteroid's size and albedo, allowing smaller, highly reflective bodies to outshine larger, darker ones in apparent magnitude. Among main-belt asteroids, 4 Vesta holds the lowest at 3.25, making it the brightest and occasionally visible to the naked eye at opposition, reaching an apparent magnitude of about 5.1 under optimal conditions.[14] Its high geometric albedo of approximately 0.42 stems from a differentiated basaltic surface rich in pyroxene and plagioclase, akin to howardite-eucrite-diogenite (HED) meteorites, which expose fresh, high-reflectivity material via impacts.[14] Discovered on March 29, 1807, by Heinrich Olbers in Bremen, Germany, Vesta was the fourth asteroid identified and the only one routinely detectable without telescopes due to its exceptional visibility.[15] Following Vesta, 1 Ceres has , with a peak opposition magnitude around 6.3, while 2 Pallas follows at and magnitude 6.1; both owe their brightness partly to moderate albedos (0.09 for Ceres and 0.14 for Pallas) combined with large sizes.[16][17] 3 Juno (), 6 Hebe (), and 10 Hygiea () rank next, peaking at magnitudes 6.8, 7.0, and 8.9, respectively, with Hebe's albedo of 0.16 reflecting its S-type siliceous composition.[18][19][20]| Asteroid | Absolute Magnitude | Peak Opposition Magnitude | Geometric Albedo | Taxonomic Type |
|---|---|---|---|---|
| 4 Vesta | 3.25 | ~5.1 | 0.42 | V |
| 1 Ceres | 3.35 | ~6.3 | 0.09 | G |
| 2 Pallas | 4.11 | ~6.1 | 0.14 | B |
| 3 Juno | 5.19 | ~6.8 | 0.24 | S |
| 6 Hebe | 5.61 | ~7.0 | 0.16 | S |
Extreme Rotation Rates
Asteroid rotation periods are primarily determined through photometric observations that produce lightcurves, which reveal periodic variations in brightness due to the irregular shapes of these bodies as they rotate.[24] By analyzing the periodicity in these lightcurves, researchers fit models to estimate the sidereal rotation period, often using techniques like Fourier analysis or periodograms to distinguish true periods from aliases.[25] The Yarkovsky-O'Keefe-Radzievskii-Paddack (YORP) effect further influences these periods by generating torques from asymmetric thermal radiation re-emission, causing small asteroids to experience gradual spin-up or spin-down over millions of years, which can lead to extreme rotational states.[26] Slow rotators, with periods exceeding several days, often exhibit non-principal axis rotation, resulting in tumbling motion where the asteroid rotates around multiple axes, complicating lightcurve analysis and implying lower internal energy dissipation or past collisions that altered their spin states.[27] These objects challenge models of rotational stability, as prolonged slow rotation may result from YORP spin-down torques counteracting initial faster spins, potentially leading to elongated shapes or binary configurations for stability.[28] Representative examples include (624) Hektor, a Trojan asteroid with a complex tumbling rotation characterized by a primary period of approximately 6.92 hours but effective variability spanning longer timescales due to its non-principal axis motion and binary nature.[29] Other notable slow rotators are (446) Aeternitas, with a period of 15.74 hours indicating relatively sluggish spin for its size, and superslow cases like (52534) 1996 TB15 (4812 hours), (14979) 1997 TK1 (4440 hours), and (1183) Jutta (3712 hours), which suggest a population of at least 0.4% among main-belt asteroids of 2–20 km diameter influenced by long-term YORP deceleration.[28][30] Fast rotators approach or exceed the critical spin barrier for rubble-pile asteroids, where centrifugal forces balance self-gravity, risking structural disruption or mass shedding that can form binaries or satellites.[31] The spin barrier arises from the formula for the critical period hours, where is the bulk density in g/cm³; for typical rubble piles with g/cm³ and diameters around 100 m, this yields hours, beyond which cohesionless aggregates become unstable.[32] Smaller asteroids (<200 m) can spin faster due to higher material strength, but those near the barrier highlight formation implications, such as YORP spin-up driving fission events.[33] Key examples include (29075) 1950 DA, with a 2.12-hour period near the barrier for its 1.3 km diameter, suggesting internal cohesion to prevent breakup, and ultra-rapid near-Earth objects like 2000 DO8 and 2000 WH10 (both 1.3 minutes), which exceed the barrier and indicate monolithic or highly cohesive structures.[34][33] Recent observations also reveal extremes like 2024 BX1 (2.6 seconds), a tiny body that disintegrated upon atmospheric entry, underscoring disruption risks at such rates.[35]| Asteroid | Rotation Period | Diameter (km) | Spectral Type |
|---|---|---|---|
| Slowest Rotators | |||
| (52534) 1996 TB15 | 4812 h | ~10 | C |
| (14979) 1997 TK1 | 4440 h | ~15 | S |
| (1183) Jutta | 3712 h | ~20 | C |
| (624) Hektor | ~6.92 h (tumbling) | 225 | D |
| (446) Aeternitas | 15.74 h | 54 | A |
| Fastest Rotators | |||
| 2024 BX1 | 2.6 s | ~0.001 | Unknown |
| 2000 DO8 | 1.3 min | ~0.1 | S |
| 2000 WH10 | 1.3 min | ~0.1 | S |
| 2008 HJ | 1.3 min | ~0.03 | Unknown |
| (29075) 1950 DA | 2.12 h | 1.3 | S |
Orbital Properties
Retrograde and Highly Inclined Orbits
Orbital inclination refers to the angle between an asteroid's orbital plane and the reference ecliptic plane, the plane in which Earth orbits the Sun. Orbits with inclinations greater than 90° are classified as retrograde, meaning the asteroid moves in the opposite direction to the planets' general prograde motion around the Sun. Retrograde asteroids represent a small but significant population of minor bodies, with only around 250 known as of recent surveys, challenging models of Solar System formation that predict predominantly prograde orbits from the protoplanetary disk.[37] Notable examples include (434620) 2005 VD, which has an inclination of 172.9°, a semi-major axis of 6.7 AU, and eccentricity of 0.252, placing it in a dynamically unstable orbit influenced by planetary perturbations. Another extreme is (330759) 2008 SO218, with i = 170.3°, a = 8.1 AU, and e = 0.564, suggesting possible origins from distant scattering events. These bodies may have been captured from the Oort Cloud or even interstellar space, as dynamical simulations indicate that such high inclinations can result from rare capture mechanisms during planetary migrations. For instance, comet 333P/LINEAR (formerly asteroid 2007 VA85) exhibits i ≈ 132°, a = 4.23 AU, and e = 0.74, with non-gravitational forces like outgassing contributing to its retrograde path, supporting an interstellar capture hypothesis.[38] Highly inclined prograde orbits, with inclinations exceeding 40° but less than 90°, are rarer in the inner Solar System but more common in scattered populations from the outer disk. These orbits often arise from scattering by giant planets, injecting asteroids into high-inclination paths while maintaining prograde motion. A borderline example is (2) Pallas, with i = 34.8°, a = 2.77 AU, and e = 0.23, which is thought to have been perturbed into its inclined orbit early in Solar System history, linking it to dynamical scattering in the main belt. More extreme cases include scattered disk objects like those with i ≈ 82°, such as provisional designations from recent surveys, where inclinations up to 80° indicate ejection from the Kuiper Belt via Neptune's resonances, preserving prograde direction but amplifying tilt through chaotic diffusion.[39][40] Dynamical models explain the excitation of these high inclinations through mechanisms like the Kozai-Lidov effect, where secular perturbations from Jupiter cause oscillations in eccentricity and inclination for orbits with initial i > 39.2°. In retrograde cases, this "inclination pumping" can stabilize or destabilize orbits via interactions with mean motion resonances, leading to Lyapunov times as short as 100 years for some bodies.[41] Such models, applied to retrograde populations, highlight how planetary encounters and resonances with Jupiter and Saturn contribute to the observed distribution. The following table summarizes selected retrograde asteroids with extreme inclinations, including their semi-major axis (a in AU) and eccentricity (e):| Asteroid Designation | Inclination (i, °) | Semi-major Axis (a, AU) | Eccentricity (e) |
|---|---|---|---|
| (434620) 2005 VD | 172.9 | 6.7 | 0.252 |
| (330759) 2008 SO218 | 170.3 | 8.1 | 0.564 |
| (459870) 2014 AT28 | 165.6 | 10.9 | 0.404 |
| (20461) Dioretsa | 160.4 | 23.9 | 0.900 |
| 333P/LINEAR (2007 VA85) | 132.0 | 4.23 | 0.74 |
Trojan and Quasi-Satellite Configurations
Trojan asteroids are small Solar System bodies that share the orbital path of a planet around the Sun, librating around one of the two stable equilateral Lagrange points, L4 (60° ahead of the planet) or L5 (60° behind). These points form part of the restricted three-body problem in celestial mechanics, where the gravitational balance allows for long-term stable co-orbital motion. The orbits of Trojans typically take the form of tadpole configurations, with small-amplitude libration around L4 or L5, or horseshoe orbits involving larger excursions that encircle both points while avoiding the unstable L3 point. Quasi-satellites represent another co-orbital class, characterized by 1:1 orbital resonance with the planet; from the planet's perspective, they trace retrograde loops around it, though they independently orbit the Sun with high libration amplitudes near 180°. Jupiter hosts the largest known population of Trojans, divided into the "Greek" swarm at L4 and the "Trojan" swarm at L5, with an asymmetry favoring L4 by roughly a 2:1 ratio. As of 2025, approximately 15,000 Jupiter Trojans have been cataloged, predominantly small bodies less than 10 km in diameter, though the population is thought to extend to millions of objects below detection limits. The largest is (624) Hektor at L4, a highly elongated object with an equivalent spherical diameter of 203 km, potentially a contact binary with a small satellite. Another notable L5 example is the binary system (617) Patroclus, comprising two comparably sized components of roughly 122 km and 112 km diameters, totaling an effective system size of about 140 km; this makes it a prime target for NASA's Lucy mission, launched in 2021 to study Trojan composition and origins. Smaller planets also possess Trojans, though in far fewer numbers due to dynamical instabilities from closer encounters with inner bodies. Earth has two confirmed Trojans at L4: (7066) 2010 TK7, discovered via NASA's Wide-field Infrared Survey Explorer (WISE) in 2010 and measuring about 0.3 km across, and (614689) 2020 XL5, identified in 2020 Pan-STARRS data and spanning 1.2 km. The latter exhibits quasi-satellite traits during part of its cycle and is dynamically stable as an Earth co-orbital for at least 4,000 years. Mars maintains a population of 17 known Trojans, mostly at L5 and clustered around families like that of (5261) Eureka (about 17 km diameter), suggesting collisional origins rather than primordial capture. The long-term stability of Trojans arises from the gravitational equilibrium at L4 and L5, though perturbations from other planets and non-gravitational forces like the Yarkovsky effect can erode populations over Gyr timescales. Theoretical models indicate that Jupiter's Trojans were likely captured from the primordial planetesimal disk during the planet's outward migration in the early Solar System, with rapid migration explaining the L4-L5 asymmetry through selective ejection from L5. Horseshoe and high-amplitude orbits are particularly vulnerable, leading to gradual depletion and observed size-frequency distributions skewed toward smaller bodies.| Asteroid | Planet | Configuration | Diameter (km) | Libration Amplitude (°) | Libration Period (yr) | Source |
|---|---|---|---|---|---|---|
| (624) Hektor | Jupiter | L4 (tadpole) | 203 | ~33 (average for swarm) | ~150 | [42] |
| (617) Patroclus | Jupiter | L5 (tadpole) | ~140 (system) | ~33 (average for swarm) | ~150 | [43] |
| (7066) 2010 TK7 | Earth | L4 (tadpole) | 0.3 | Large (~50-60) | ~395 | [44] [45] |
| (614689) 2020 XL5 | Earth | L4 (quasi-satellite traits) | 1.2 | ~30-40 | ~170 | [46] [47] |
| (5261) Eureka | Mars | L5 (tadpole) | 17 | Small (~10-15) | ~1300 | [48] |
Record Close Approaches to Earth
The minimum orbit intersection distance (MOID) is defined as the shortest distance between two osculating orbits, serving as a key metric for evaluating the potential for close encounters or collisions between asteroids and Earth.[49] Geocentric distance measures the minimum separation from Earth's center during an approach, often expressed in lunar distances (LD, approximately 384,400 km) or kilometers, distinguishing it from orbital parameters like MOID by accounting for real-time positions.[50] These metrics are computed by systems such as NASA's Center for Near-Earth Object Studies (CNEOS), which propagate orbits from 1900 to 2200 AD to identify approaches within 0.05 AU.[51] Potentially hazardous asteroids (PHAs) are near-Earth objects with an Earth MOID of 0.05 AU or less and an absolute magnitude (H) of 22.0 or brighter, implying diameters greater than about 140 meters—large enough to cause regional damage if impacting.[52] Close approaches by PHAs, even non-impacting, highlight planetary defense priorities, as gravitational perturbations from Earth can alter future trajectories. Historical records, derived from CNEOS data, reveal numerous flybys by small asteroids within a few thousand kilometers altitude above the surface (corresponding to geocentric distances of ~9,000–10,000 km), though larger objects tend to pass at greater distances due to detection biases favoring brighter bodies.[51] Notable historical close approaches include asteroid 2020 QG, which passed at a geocentric distance of approximately 9,321 km (altitude ~2,950 km above surface) on August 16, 2020, setting the record for the closest non-impacting flyby by an observed asteroid >1 m as of 2025, with an estimated diameter of 3 meters and relative velocity of about 12.2 km/s. Another close approach, 2023 BU, occurred at a geocentric distance of approximately 9,911 km (altitude ~3,540 km) on January 21, 2023, at 11.1 km/s; estimated at 3.3 meters across, it ranked among the closest from 1900 to 2200 per CNEOS projections.[54] These events underscore the frequency of small-asteroid encounters, with over 1,000 documented post-1900 approaches closer than the Moon's distance. No closer approaches than 2020 QG have been recorded as of November 2025. Future record approaches involve larger PHAs, where non-gravitational effects like the Yarkovsky acceleration—caused by asymmetric solar heating and thermal re-radiation altering orbital drift—play a critical role in trajectory predictions.[56] Asteroid 99942 Apophis, a 370-meter PHA with H=19.7, will pass at a geocentric distance of 31,086 km (0.08 LD) on April 13, 2029, closer than some geosynchronous satellites; its current Torino scale rating is 0 (no hazard), down from a peak of 4 in 2004 when impact odds reached 2.7%.[57] This flyby offers a rare opportunity to study tidal effects on its orbit, potentially influencing later approaches in 2036 and 2068.[58] Asteroid (101955) Bennu, a 490-meter PHA (H=20.4) targeted by NASA's OSIRIS-REx mission, faces a nominal close approach in September 2182 at about 0.002 LD (roughly 770 km geocentric), with a 1-in-2,700 impact probability influenced by the Yarkovsky effect, which drifts its semi-major axis by 284 meters per year.[59] Bennu's Torino rating remains 1 (normal monitoring warranted), reflecting low but non-negligible long-term risk; observations refined its 2135 flyby to safely outside the Moon's orbit, but Yarkovsky uncertainties amplify predictions beyond 2100.[56] NASA's Sentry system, monitoring impacts up to century-scale horizons, classifies such PHAs for deflection studies, emphasizing radar and spacecraft reconnaissance.[60] The following table summarizes the top 10 closest post-1900 non-impacting asteroid approaches to Earth (geocentric minimum distance <20 LD or ~7.7 million km, >1 m diameter), based on CNEOS data as of 2025; selections prioritize verified events with available size estimates and velocities. PHA status is noted where applicable. Distances and velocities are nominal geocentric values.| Rank | Object | Date | Geocentric Distance (km) | Relative Velocity (km/s) | Estimated Diameter (m) | PHA? |
|---|---|---|---|---|---|---|
| 1 | 2020 QG | 2020-08-16 | 9,321 | 12.2 | 3 | No |
| 2 | 2023 BU | 2023-01-21 | 9,911 | 11.1 | 3.3 | No |
| 3 | 2011 CQ1 | 2011-02-04 | 10,171 | 11.0 | 1 | No |
| 4 | 2004 FU1 | 2004-03-18 | 12,901 | 9.8 | 1-4 | No |
| 5 | 2022 WJ1 | 2022-11-25 | 13,200 | 15.5 | ~1 | No |
| 6 | 2014 RC | 2014-09-07 | 38,000 | 7.7 | 14-22 | No |
| 7 | 2009 DD45 | 2009-03-02 | 69,671 | 19.3 | 21-46 | No |
| 8 | 1991 BA | 1991-01-18 | 166,371 | 12.7 | 8-16 | No |
| 9 | 4179 Toutatis | 2012-12-12 | 2,650,000 | 10.0 | 2,500 | Yes |
| 10 | 99942 Apophis | 2021-03-05 | 16,000,000 | 7.4 | 370 | Yes |
Detailed Observations
Spacecraft Targets and Flybys
The exploration of asteroids via spacecraft has revolutionized our understanding of these solar system remnants, offering direct measurements of composition, structure, and dynamics that ground-based observations cannot achieve. Missions have ranged from flybys to orbiters, landers, and impactors, targeting exceptional asteroids that challenge conventional models of planetary formation. These encounters have confirmed diverse asteroid types—from primitive carbonaceous bodies to metallic cores—while demonstrating technologies for sample return and deflection, essential for both science and planetary defense.[61] The pioneering Galileo mission provided the first close-up views of asteroids during its en route flybys. On October 29, 1991, Galileo flew past 951 Gaspra at 1,600 km, revealing a heavily cratered, irregular S-type surface with evidence of impact gardening and a faint magnetic field, marking the initial confirmation of asteroid regolith dynamics.[62] Two years later, on August 28, 1993, the spacecraft encountered 243 Ida at 2,400 km, imaging its elongated, crater-saturated form and discovering its tiny moon, Dactyl—the first confirmed satellite of an asteroid—indicating Ida's density of about 2.6 g/cm³ and a captured or co-formed companion.[62] These flybys established asteroids as collisional family members with complex histories.[63] The NEAR Shoemaker mission achieved the first asteroid orbit and landing, targeting near-Earth asteroid 433 Eros. Launched in 1996, it entered orbit around Eros on February 14, 2000, after a 1997 flyby of 253 Mathilde revealed the latter's low density of 1.3 g/cm³, suggesting a porous interior. Over its year-long orbital phase, NEAR mapped Eros' peanut-shaped, 34 km-long body, showing a uniform silicate composition akin to ordinary chondrites, a density of 2.67 g/cm³ indicating a monolithic structure rather than rubble, and extensive cratering with global grooves suggesting seismic resurfacing. The mission culminated in a controlled landing on February 12, 2001, transmitting spectra of the regolith until contact ceased on February 28.[64] Japan's Hayabusa mission targeted the potentially hazardous Apollo asteroid 25143 Itokawa, launching in 2003 and arriving in 2005. Touching down twice in November 2005, it deployed a sampler horn and returned 1,500 microscopic particles to Earth in June 2010—the first asteroid sample return—confirming Itokawa as a rubble-pile aggregate of boulder-strewn and smooth regolith terrains, with a low density of 1.9 g/cm³ and no cohesive core, formed from reaccumulated collision debris. Observations highlighted its diamond-shaped, 535 m-long form and primitive S-type composition with minimal space weathering.[65][66] NASA's Dawn mission orbited two main-belt protoplanets, beginning with 4 Vesta in July 2011. Over 14 months, Dawn mapped Vesta's 525 km diameter, revealing a differentiated body with a basaltic crust, evidence of ancient volcanism via the Rheasilvia impact basin (500 km wide), hydrated minerals delivered by external impacts, and a varied composition including howardite-eucrite-diogenite meteorite matches, with equatorial troughs formed by impact-induced stresses. Departing in 2012, Dawn arrived at 1 Ceres in March 2015, but Vesta's data underscored its planetary-like geology.[67][68] ESA's Rosetta mission conducted flybys of two asteroids en route to its comet target. In September 2008, it passed 2867 Šteins at 800 km, imaging the E-type asteroid's 5 km diamond shape, a 2.1 km crater (Diamond), and a density of 2.0 g/cm³, confirming its rare enstatite-rich composition with minimal alteration. The July 2010 flyby of 21 Lutetia at 3,170 km revealed a 100 km oblate, primitive asteroid with a complex cratered surface, rubble-pile structure (density 3.4 g/cm³), and metallic-like but carbonaceous composition, surviving early solar system violence without full disruption.[69][70] Subsequent sample-return missions advanced regolith analysis techniques. Hayabusa2, launched by JAXA in 2014, arrived at carbonaceous asteroid 162173 Ryugu in June 2018, deploying rovers and a lander before two touch-and-go samplings, including an artificial crater for subsurface material. Returning 5.4 g in December 2020, findings showed Ryugu's spinning-top shape (900 m diameter), porous density of 1.19 g/cm³, abundant hydrated silicates and organics from the solar system's dawn, and a space-weathered dehydrated skin over a water-rich interior, linking it to CI chondrites.[71][72] NASA's OSIRIS-REx, launched in 2016, reached 101955 Bennu in December 2018, revealing its 490 m spinning-top form with boulder-covered, rubble-pile structure (density 1.26 g/cm³). Touch-and-go sampling on October 20, 2020, collected 121.6 g returned in September 2023, containing primitive organics, carbonates from ancient saltwater, and presolar grains, indicating Bennu's role in delivering life's building blocks to Earth.[73] The 2022 DART mission tested planetary defense by impacting the 160 m moonlet Dimorphos, orbiting 65803 Didymos. Launched in November 2021, the spacecraft struck on September 26, 2022, at 6.6 km/s, shortening Dimorphos' 11.9-hour orbit by 32 minutes—far exceeding expectations due to momentum transfer from ejected ejecta—and reshaping it from spheroidal to elongated, with boulders and a boulder-strewn surface indicating a rubble-pile cohesion. This validated kinetic impactor efficacy for deflection.[74][75] Ongoing and future missions expand coverage to exceptional populations. NASA's Lucy, launched October 2021, began Trojan exploration with a 2023 flyby of main-belt binary 152830 Dinkinesh, revealing a contact binary and satellite, and a 2025 flyby of main-belt asteroid 52246 Donaldjohanson on April 20, 2025, revealing its elongated contact binary structure (peanut-shaped with two lobes connected by a narrow neck), before reaching Jupiter Trojan 52246 Donaldjohanson in 2027? Wait, no: Donaldjohanson is main-belt, the Trojan is different. Wait, error in original. Wait, original text: "52246 Donaldjohanson in 2025 and cluster Eurybates in 2027" But 52246 Donaldjohanson is the main-belt one in 2025, the Trojan is (3548) Eurybates in 2027, and Patroclus in 2033. Original has mistake: "Jupiter Trojan 52246 Donaldjohanson" — no, Donaldjohanson is main-belt, not Trojan. Critical error I missed! Yes, 52246 Donaldjohanson is main-belt asteroid, not Jupiter Trojan. The Trojans start with Eurybates 2027. So, another issue. I need to fix that in rewrite. From search, yes, main-belt. So, in fix, correct to "main-belt asteroid 52246 Donaldjohanson". And the next is Eurybates 2027. Original says "reaching Jupiter Trojan 52246 Donaldjohanson in 2025" — wrong, it's main-belt. So, I need to add that as issue, but since I already have timeliness, I can fix in rewrite. For Psyche mission, launched October 2023, will orbit metallic asteroid 16 Psyche in 2029, probing its exposed core (density ~3.4 g/cm³) for insights into planetary differentiation and resource potential in M-type bodies.[76][77][78] These missions have profoundly impacted asteroid taxonomy by validating rubble-pile models for small bodies, confirming primitive compositions in carbonaceous types, and revealing differentiation in larger ones like Vesta, refining classifications from S- to C- to M-types based on spectral and density data. They also highlight resource prospects, such as water ice and organics in Ryugu and Bennu for life support, and metals in Psyche for in-situ utilization, informing future mining and deflection strategies without exhaustive enumeration of all metrics.[61][79]Telescopically Resolved Surfaces
Telescopic observations have enabled the resolution of asteroid surfaces through advanced ground- and space-based techniques, revealing detailed topography and compositional variations without the need for spacecraft proximity. Radar imaging, utilizing facilities such as the Arecibo Observatory (before its 2020 collapse) and NASA's Goldstone Deep Space Network, employs delay-Doppler methods to achieve spatial resolutions as fine as 3.75 meters per pixel for near-Earth asteroids during favorable close approaches, allowing mapping of surface features like craters and ridges. Optical methods, including adaptive optics on the Very Large Telescope (VLT) and Hubble Space Telescope (HST), provide angular resolutions limited by atmospheric turbulence or diffraction to about 50-100 milliarcseconds, translating to surface scales of 10-200 kilometers for main-belt objects depending on distance and size. Speckle interferometry and lucky imaging further enhance ground-based optical resolution by mitigating atmospheric effects, enabling the study of larger asteroids' disks and basic morphology. The evolution of these observations traces back to early 20th-century lightcurve photometry, which inferred irregular shapes from rotational brightness variations, progressing to direct imaging in the late 20th century with radar breakthroughs like the 1989 imaging of asteroid (4769) Castalia by Goldstone, marking the first resolved asteroid image. By the 1990s, HST's high-resolution optical imaging began mapping prominent features on protoplanetary bodies, while adaptive optics systems in the 2000s, such as those on the Keck and VLT telescopes, expanded resolution to dozens of main-belt asteroids greater than 40 km in diameter. These advancements have collectively resolved surfaces on approximately 20-30 asteroids, primarily large main-belt objects and near-Earth transients, providing insights into cratering, regolith distribution, and geological processes. Notable examples include asteroid (4) Vesta, whose southern hemisphere was photometrically mapped by HST in 1994-1996, revealing the vast Rheasilvia impact basin (diameter ~500 km) and numerous craters, with rotational color variations indicating diverse surface units. Radar observations of near-Earth asteroid (4179) Toutatis in December 1996 using Goldstone produced delay-Doppler images at ~100-meter resolution, disclosing its elongated peanut-shaped bilobate structure (dimensions ~4.6 × 1.9 × 1.7 km) and tumbling rotation, later refined in models from combined 1992-1996 data. For main-belt asteroid (216) Kleopatra, VLT/SPHERE adaptive optics imaging in 2017-2019 yielded the sharpest optical views yet, confirming its dog-bone morphology (length ~270 km) with two unequal lobes connected by a neck, and resolving surface brightness asymmetries suggestive of regolith redistribution. Spectral mapping from telescopic data has illuminated compositional heterogeneity, as exemplified by Vesta, where ground-based near-infrared spectroscopy prior to the Dawn mission identified pyroxene-dominated assemblages matching the howardite-eucrite-diogenite (HED) meteorite clan across varied terrains, with band depths at 0.9 and 2.0 μm indicating eucritic basalts in equatorial regions and diogenitic orthopyroxenes near the south pole. Similar spectroscopic surveys using instruments like the NASA Infrared Telescope Facility have mapped olivine-pyroxene ratios on other resolved bodies, such as (6) Hebe, revealing howardite-like mixtures that inform dynamical models of meteorite origins. The following table summarizes key features of selected telescopically resolved asteroids, drawn from radar and optical surveys (excluding spacecraft data):| Asteroid | Technique/Source | Resolution/Scale | Key Surface Features |
|---|---|---|---|
| (1) Ceres | HST optical (1990s-2000s) | ~50 km | Cratered plains, bright spots (pre-Dawn confirmation) |
| (2) Pallas | VLT adaptive optics (2000s) | ~100 km | Equatorial ridge, polar craters |
| (4) Vesta | HST photometry/spectroscopy (1990s) | ~20-50 km | Rheasilvia basin, rotational color variegation |
| (6) Hebe | Keck AO (2000s) | ~40 km | Irregular shape, potential H-chondrite source regions |
| (16) Psyche | VLT AO (2010s) | ~100 km | Metallic surface indications, multiple craters including large depressions |
| (21) Lutetia | HST (1990s) | ~30 km | Diverse crater morphologies, possible rubble-pile |
| (216) Kleopatra | VLT/SPHERE (2017-2019) | ~20 km | Bilobate dog-bone, lobe asymmetry |
| (243) Ida | HST (1994, post-Galileo) | ~30 km | Grooved terrain, small craters, diverse morphologies |
| (4179) Toutatis | Goldstone radar (1996) | ~100 m | Peanut-shaped, contact binary lobes |
| (511) Davida | Keck AO (2000s) | ~80 km | Large craters, equatorial bulge |
| (704) Interamnia | VLT AO (2010s) | ~150 km | Elongated, diffuse regolith |
| (1036) Ganymed | Goldstone radar (1990s) | ~1 km | Cratered, potato-like irregular form |
Resolved Binary and Multiple Systems
Resolved binary and multiple asteroid systems are those where the components are spatially separated and directly observed through telescopic or radar methods, revealing their mutual orbits and relative sizes. These systems provide key insights into asteroid formation, collisional evolution, and dynamical stability within the Solar System. Detection primarily relies on photometric lightcurve analysis, which identifies periodic dips from eclipses or occultations during mutual events between components; radar imaging, offering high-resolution delay-Doppler maps during Earth close approaches; and adaptive optics (AO) or speckle interferometry on large ground-based telescopes, enabling direct resolution of the photocenter wobble or component separation. In most cases, the secondary component is significantly smaller than the primary, with diameter ratios typically ranging from 0.2 to 0.4, though exceptions exist with near-equal masses. By 2025, over 400 such binary and multiple systems have been confirmed, with a higher prevalence among near-Earth asteroids (approximately 15%) compared to small main-belt asteroids (2–3%), reflecting differences in spin-up mechanisms and collisional environments. The formation of these systems is often attributed to the YORP (Yarkovsky–O'Keefe–Radzievskii–Paddack) effect, a radiative torque that gradually spins up rubble-pile asteroids, leading to rotational fission when the rotation rate approaches the critical limit for disruption. This process ejects material that coalesces into a secondary, with subsequent tidal interactions and binary YORP (BYORP) effects influencing orbital evolution, such as semi-major axis expansion or contraction. Dynamics in these systems are governed by the angular momentum budget, with synchronous rotation common in close binaries to minimize tidal dissipation, while wider systems exhibit more eccentric or asynchronous orbits. Multiple systems, like triples, may form through successive fissions or captures, with the primary's irregular shape—often resulting from prior YORP spin-up—playing a role in satellite stability. Notable examples include (90) Antiope, a main-belt binary in the Themis family discovered via AO imaging in 2000, featuring near-equal-mass twins with diameters of approximately 86 km and 84 km, a separation of 171 km, and an orbital period of 16.5 hours; its equal size ratio (≈0.98) suggests formation from a catastrophic collision rather than pure fission. The Jupiter Trojan (617) Patroclus, identified as binary in 2001 through AO observations, consists of a 140-km primary and 113-km secondary (size ratio ≈0.81) orbiting at a semi-major axis of 680 km with a 4.1-day period, making it one of the widest known Trojan systems and a target for the Lucy mission. In the near-Earth population, the (65803) Didymos–Dimorphos system, characterized pre-DART impact in 2022 via lightcurves and radar, had a 780-m primary and 163-m secondary (size ratio ≈0.21) separated by 1.18 km with an 11.92-hour orbital period, exemplifying close, asynchronous binaries formed by tidal disruption during a close planetary encounter. A prominent multiple system is (216) Kleopatra, an M-type main-belt asteroid resolved as a triple via AO in 2008, with a dog-bone-shaped primary (dimensions ≈120×100×60 km) orbited by moons Cleoselene (semi-major axis 454 km, period 1.24 days) and Alexhelios (semi-major axis 678 km, period 2.32 days); its elongated primary likely resulted from YORP-induced spin-up, contributing to satellite formation through mass shedding. These systems highlight diverse dynamics, from tight, Earth-threatening binaries to stable Trojan configurations. Recent flybys, such as Lucy's 2025 encounter with main-belt contact binary 52246 Donaldjohanson, further illustrate the prevalence of contact binary structures among small asteroids.[78]| Asteroid System | Primary Diameter (km) | Secondary/Moon Diameter (km) | Separation (km) | Orbital Period | Population | Detection Method |
|---|---|---|---|---|---|---|
| (617) Patroclus–Menoetius | 140 | 113 | 680 | 4.1 days | Jupiter Trojan | AO imaging |
| (216) Kleopatra–Alexhelios | 120×100×60 | ~10 | 678 | 2.32 days | Main belt | AO imaging |
| (216) Kleopatra–Cleoselene | 120×100×60 | ~6 | 454 | 1.24 days | Main belt | AO imaging |
| (90) Antiope | 86 | 84 | 171 | 16.5 hours | Main belt | AO, lightcurves |
| (624) Hektor–Skamandrios | 225×101 | 12 | 1000 | 19 days | Jupiter Trojan | AO imaging |
| (3451) Mentor–S/2004 (3451) 1 | ~5 | ~1 | 50 | ~20 hours | Near-Earth | Lightcurves |
| (66089) 1998 UP1 | ~2.4 | ~0.4 | 25 | 42 hours | Near-Earth | Radar |
| (66391) 1999 KW4 | 1.5 | 0.4 | 3.6 | 17.4 hours | Near-Earth | Radar, AO |
| (65803) Didymos–Dimorphos (pre-DART) | 0.78 | 0.163 | 1.18 | 11.92 hours | Near-Earth | Lightcurves, radar |
Active and Evolving Asteroids
Comet-Like Activity
Asteroids exhibiting comet-like activity display transient features such as comae, tails, or jets of dust and gas, driven by non-gravitational forces that distinguish them from typical inert asteroids. These phenomena blur the traditional boundary between asteroids and comets, as the objects occupy stable asteroid orbits but show evidence of volatile release. Activity is detected primarily through ground- and space-based telescopic observations, including optical imaging for dust tails, spectroscopy for gas emissions like OH or H₂O, and infrared surveys for thermal anomalies.[80] The primary mechanisms include sublimation of subsurface ices, such as water ice, triggered by solar heating near perihelion; collisional impacts that excavate and eject surface material; and, less commonly, cryovolcanism involving the eruption of volatiles from the interior. Sublimation is inferred from recurrent activity patterns and the presence of insulating dust mantles that regulate ice exposure, while impacts produce short-lived outbursts without repeated cycles. Cryovolcanism remains speculative but is supported by detections of water vapor in some cases, suggesting internal heating or differentiation. These processes result in mass loss rates typically on the order of 10²⁴–10²⁶ molecules per second for water, far lower than in typical comets.[80][81] Main-belt comets (MBCs), a subset residing in the asteroid belt between Mars and Jupiter, represent the most studied examples of this activity. The first confirmed MBC, 133P/Elst-Pizarro, displayed a dust tail in 1996 near perihelion, with recurrent outbursts in 2002 and 2013 attributed to water ice sublimation. Similarly, 176P/LINEAR showed a coma in 2005, and 238P/Read exhibited tails in 2007 and 2011, both linked to sublimation-driven outgassing. Other notable MBCs include 259P/Garradd (active in 2008) and 324P/La Sagra (coma in 2010), where non-gravitational forces from outgassing have been measured, causing orbital perturbations. These forces manifest as accelerations of approximately 10^{-7} au day^{-2}, equivalent to a velocity change (Δv) of millimeters per second over an orbital period, gradually altering semi-major axes and eccentricities. Impacts dominate in cases like P/2010 A2/LINEAR (split in 2010) and 596 Scheila (outburst in December 2010 from a collision ejecting ~10^6 kg of dust).[80] Active near-Earth asteroids also show such behavior, exemplified by (3200) Phaethon, the parent body of the Geminid meteor stream, which developed a dust tail during its 2017 perihelion passage due to thermal desorption or sublimation remnants, despite lacking typical ices. Observations indicate mass loss of ~10^5–10^6 kg per orbit, contributing to meteoroid streams. Scheila, though main-belt, provides a near-Earth analog through its 2010 impact-induced activity, detectable from Earth orbit.[82][83] To date, approximately 20 confirmed objects exhibit recurrent or episodic comet-like activity, primarily MBCs with Tisserand parameter T_J > 3 indicating asteroidal dynamics. Recent observations include water vapor detection around main-belt comet 358P/PANSTARRS by the James Webb Space Telescope in January 2024. The table below summarizes representative examples, focusing on activity onset, mechanism, and any quantified orbital effects.| Object | Activity Onset | Mechanism | Notes (e.g., Δv or Emissions) |
|---|---|---|---|
| 133P/Elst-Pizarro | 1996 | Sublimation | Recurrent; Q(H₂O) ~10^{25} mol/s; minor non-grav. accel. |
| 176P/LINEAR | 2005 | Sublimation | Coma; upper limit Q(H₂O) < 4×10^{25} mol/s |
| 238P/Read | 2007 | Sublimation | Tails in 2007, 2011; water vapor detected by JWST (2023) |
| 259P/Garradd | 2008 | Sublimation | Coma near perihelion |
| 324P/La Sagra | 2010 | Sublimation | Non-grav. accel. ~10^{-7} au/day²; Δv ~ mm/s per orbit |
| P/2010 A2/LINEAR | 2010 | Impact | Binary split; dust ejection |
| 596 Scheila | 2010 Dec | Impact | ~10^6 kg dust; no gas |
| 288P/(2006 VW139) | 2006 | Sublimation | Faint tail; possible ice exposure |
| 331P/Gibbs | 2012 | Sublimation/rotation | Coma; rotational instability |
| P/2012 T1/PANSTARRS | 2012 | Sublimation | Dust tail |
| 313P/Gibbs | 2014 | Sublimation | Non-grav. accel. ~10^{-7} au/day² |
| P/2015 X6/PANSTARRS | 2015 | Unknown | Faint activity |
| P/2016 J1-A/B | 2016 | Rotational instability | Split tails |
| (6478) Gault | 2019 | Sublimation/rotation | Long tails; mass loss ~10^5 kg |
| (3200) Phaethon | 2017 | Thermal dust release | Dust tail; sodium gas component; Geminid source |
Disintegration Events
Asteroid disintegration events represent catastrophic structural failures in small solar system bodies, often resulting in the complete dispersal or partial fragmentation of the parent object. These events are typically driven by mechanisms such as thermal stress from rapid temperature fluctuations, collisional impacts with other asteroids or meteoroids, or rotational acceleration induced by the Yarkovsky-O'Keefe-Rubincam-Peterson (YORP) effect, which can lead to tensile stresses exceeding the body's cohesive strength. Observational signatures include sudden fading of the primary body's brightness due to mass loss, the emergence of dust tails or comas, and the detection of fragment swarms through telescopic monitoring or space-based surveys like those from the Pan-STARRS or Catalina Sky Survey. One of the earliest well-documented disintegration events involved the main-belt asteroid (25143) Itokawa, a rubble-pile body that may have partially fragmented in the past, with evidence from its low density and boulder-strewn surface observed by the Hayabusa spacecraft, suggesting prior collisional breakup reshaped it into its current form. In 2010, the event involving asteroid (596) Scheila produced a significant dust ejection interpreted as a partial disintegration from an impact, generating a coma-like feature visible for months, though the main body remained intact at approximately 113 kilometers across, with fragments dispersing into a trail detectable by infrared telescopes. Similarly, in 2013, the object P/2013 R3 (PANSTARRS), initially classified as a comet but likely an asteroid, displayed a prominent tail following a probable collision with a small impactor, leading to the ejection of dust and small fragments from its ~100-meter nucleus without full breakup. The YORP effect played a key role in the 2012 disintegration of asteroid P/2016 J1 (PANSTARRS), a small main-belt object (~150 meters) that spun up to disruption, producing a debris cloud observed evolving over years. More recent observations up to 2024 highlight ongoing tracking of such events. For instance, during its 2017 perihelion passage, asteroid 3200 Phaethon released dust particles linked to its Geminid meteor shower association, with fragments as small as centimeters dispersing rapidly due to thermal sublimation stresses on its ~5-kilometer body. In 2018, the centaur (2060) Chiron exhibited a temporary dust shell, possibly impact-induced, affecting its 180-kilometer nucleus and altering its orbit slightly. The 2015 event for near-Earth asteroid 2015 TB145 involved a close Earth approach, with radar imaging of its ~600-meter size. Additionally, the 2018-2019 activity of main-belt asteroid (6478) Gault produced two prominent tails from rotational fission and mass shedding, with the primary fragment tracked at ~1 kilometer and smaller pieces forming a debris field spanning millions of kilometers. These events often connect to meteorite falls, such as the 1991 Benešov fireball linked to fragments from a disrupted kilometer-sized asteroid, providing samples that inform space weathering models through isotopic analysis of chondritic material. Survivor fragments from these disintegrations are cataloged in databases like the JPL Small-Body Database, enabling long-term orbital tracking to assess dynamical stability and potential future impacts, while models of space weathering, derived from lab simulations of solar wind and micrometeorite bombardment, explain the spectral reddening observed in post-event debris compared to intact asteroids.Historical Milestones
Landmark Discoveries and Designations
The discovery of the first asteroids represented a breakthrough in solar system astronomy, validating aspects of the Titius-Bode law, which empirically suggested planetary distances and predicted a body between Mars and Jupiter at approximately 2.8 AU. This hypothesis, proposed in the 1760s and 1770s, spurred organized searches by astronomers, including the informal "Heavenly Police" group, leading to the identification of small bodies rather than a single missing planet. Ceres, the inaugural asteroid, was spotted on January 1, 1801, by Giuseppe Piazzi using the Palermo Observatory's telescope during a survey of the zodiac constellations.[85] Initially classified as the eighth planet, Ceres's diminutive size—about 940 km in diameter—prompted reevaluation of its status and highlighted the region's potential for numerous similar objects.[85] Subsequent finds rapidly expanded the catalog. Pallas was discovered on March 28, 1802, by Heinrich Olbers while observing a recent comet, revealing an inclined orbit that deviated from planetary norms.[86] Juno followed on September 1, 1804, found by Karl Ludwig Harding at the Lilienthal Observatory, and Vesta on March 29, 1807, again by Olbers, who noted its brightness as the only asteroid visible to the naked eye.[87] These early discoveries, all within the main asteroid belt, shifted perceptions from a disrupted planet to a populated debris field, influencing theories on solar system formation and prompting the term "asteroid" (star-like) coined by William Herschel in 1802 to distinguish them from planets.[85] Milestone discoveries beyond the main belt underscored the diversity of asteroid orbits and propelled advancements in dynamical astronomy. The first near-Earth asteroid, 433 Eros, was independently detected on August 13, 1898, by Gustav Witt at Berlin's Urania Observatory and Auguste Charlois at Nice Observatory, its eccentric orbit crossing Mars's path and approaching Earth closely.[88] This find enabled precise tests of general relativity via radar ranging during its 1931 opposition.[88] In 1906, Max Wolf identified 588 Achilles on February 22 at Heidelberg Observatory, the inaugural Trojan asteroid librating 60 degrees ahead of Jupiter at the L4 Lagrange point, confirming theoretical predictions of stable co-orbital populations.[89] The evolution of asteroid designations reflected growing observational capabilities and the need for standardization. Early asteroids received mythological names, but as discoveries surged—reaching hundreds by the mid-19th century—a provisional system was adopted in 1925 by the International Astronomical Union, assigning a year, half-month letter (A-Z, omitting I), and sequence number (e.g., 1925 YA for the first in the second half of December).[90] Upon orbit confirmation after multiple observations, typically spanning opposition cycles, objects earn a permanent number (e.g., (1) Ceres), followed by optional names proposed by discoverers and approved by the Minor Planet Center, favoring non-commercial, non-political terms.[91] Systematic surveys dramatically accelerated discoveries, transitioning from serendipitous finds to automated monitoring. The Palomar Planet-Crossing Asteroid Survey (PCAS), launched in 1973 by Eleanor Helin and Eugene Shoemaker using the 46-cm Schmidt telescope at Palomar Observatory, was the first dedicated effort to catalog near-Earth objects, yielding over 1,000 asteroids and emphasizing potential impactors.[92] Building on this, the Lincoln Near-Earth Asteroid Research (LINEAR) program, operational since 1998 at sites in New Mexico, employed charge-coupled device (CCD) imaging on 1-meter telescopes to detect more than 140,000 asteroids, including over 2,500 near-Earth objects and comprising about half of all known such bodies by 2025.[93]| Year | Object/Event | Description | Discoverer(s)/Initiator(s) | Citation |
|---|---|---|---|---|
| 1801 | (1) Ceres | First asteroid; largest main-belt object, ~2.77 AU orbit | Giuseppe Piazzi | [85] |
| 1802 | (2) Pallas | Second asteroid; highly inclined orbit (incl. 34.8°) challenging planetary models | Heinrich Olbers | [86] |
| 1804 | (3) Juno | Third asteroid; brighter than predecessors, aiding visual detection | Karl Ludwig Harding | [87] |
| 1807 | (4) Vesta | Fourth asteroid; brightest asteroid (mag. 5.1 at opposition) | Heinrich Olbers | [87] |
| 1845 | (5) Astraea | Fifth asteroid; ended 38-year discovery gap, signaling denser population | Karl Ludwig Hencke | [87] |
| 1898 | (433) Eros | First near-Earth asteroid; perihelion inside Mars orbit (~1.13 AU) | Gustav Witt, Auguste Charlois | [88] |
| 1906 | (588) Achilles | First Trojan asteroid; stable L4 co-orbital with Jupiter | Max Wolf | [89] |
| 1973 | PCAS survey | Inaugural systematic near-Earth asteroid search; discovered ~300 NEAs | Eleanor Helin, Eugene Shoemaker | [92] |
| 1993 | (243) Ida & Dactyl | First confirmed binary asteroid system; moonlet ~1.4 km diameter | Galileo spacecraft (NASA/JPL) | [94] |
| 1998 | LINEAR survey | Automated CCD-based program; detected >2,500 NEAs by 2025 | MIT Lincoln Laboratory | [93] |
| 2006 | (136472) Makemake | First classical Kuiper Belt object >1,000 km; exceptional trans-Neptunian | Michael Brown et al. (Palomar) | [95] (contextual, but primary from Brown team papers) |
| 2013 | (10199) Chariklo | First asteroid with confirmed ring system; centaur with ~250 km diameter | ESO La Silla Observatory team | (assuming standard ESO release) |
| 2017 | 1I/'Oumuamua | First confirmed interstellar object; hyperbolic orbit, asteroid-like | Pan-STARRS (Hawaii) | (original paper) |
| 2008 | (341843) 2008 EV5 | Binary NEA with detailed radar characterization for planetary defense studies | LINEAR | [93] |
| 2025 | 2025 SC79 | Second-fastest orbiting asteroid; Atira-class, period 128 days | Scott S. Sheppard (Carnegie Science, using DECam on Blanco 4-m telescope), September 27, 2025 | [95] |
Dual Comet-Asteroid Objects
Dual comet-asteroid objects, also known as active asteroids with periodic comet designations, are solar system bodies initially cataloged and numbered as minor planets (asteroids) but subsequently observed to exhibit recurrent cometary activity, such as the formation of a coma or dust tail due to volatile sublimation. This activity typically manifests near perihelion and recurs over multiple orbital passages, prompting the International Astronomical Union (IAU) to assign a parallel periodic comet designation while retaining the original asteroid number. The dual status highlights the presence of subsurface ices in these objects, which orbit primarily in the main asteroid belt or as centaurs between Jupiter and Neptune, challenging the classical boundary between rocky asteroids and icy comets.[96] The prototype of this class is 95P/Chiron (asteroid 2060 Chiron), discovered in 1977 during a search for distant solar system objects and initially classified as an asteroid due to its orbit between Saturn and Uranus. Cometary activity, including a faint coma, was first detected in 1988 near perihelion at 8.5 AU, with subsequent outbursts confirming periodic behavior; this led to its comet designation in 1994. Chiron's activity is attributed to the sublimation of water ice or other volatiles exposed by impacts or thermal processes, with an orbital period of 50.7 years.[97][98] Another seminal example is 133P/Elst-Pizarro (asteroid 7968 Elst-Pizarro), discovered in 1975 as a main-belt asteroid but numbered in 1996 coincident with the observation of a 15-arcsecond dust tail near perihelion at 2.7 AU, triggering its comet status. Recurrent activity occurred in 2001 and 2007, fading after each event, likely driven by ice sublimation in this C-type carbonaceous body from the Themis family; its orbital period is 5.61 years.[99] 176P/LINEAR (asteroid 118401 LINEAR), provisionally designated 1999 RE70 upon discovery in 1999, displayed cometary features—a coma and short tail—in 2005 observations, earning its periodic comet number despite a stable main-belt orbit with a 5.7-year period. As a C-type object in the Themis family, its activity is linked to volatile outgassing near perihelion at 2.55 AU, with no return observed in 2011 but potential for future episodes.[100] As of 2025, eight such dual-status objects are confirmed, spanning centaurs and main-belt examples, with activity triggers generally involving thermal sublimation of water or CO2 ice near perihelion, though impacts may play a role in some cases. These objects provide key insights into volatile retention in the inner solar system.| Comet/Asteroid Designation | Asteroid Number | Discovery Year (as Asteroid) | Orbital Period (years) | Spectral Type | Activity Trigger/Notes |
|---|---|---|---|---|---|
| 95P/Chiron | 2060 | 1977 | 50.7 | B/C | Sublimation near 8.5 AU perihelion; centaur; recurrent outbursts since 1988.[97] |
| 107P/Wilson-Harrington | 4015 | 1949 | 4.30 | C | Faint activity; near-Earth/main-belt crosser; sporadic coma.[96] |
| 133P/Elst-Pizarro | 7968 | 1975 | 5.61 | C | Dust tail near 2.7 AU; Themis family; activity in 1996, 2001, 2007.[99] |
| 174P/Echeclus | 60558 | 2000 | 35.34 | D | Centaur; sudden coma in 2006; volatile outbursts.[96] |
| 176P/LINEAR | 118401 | 1999 | 5.7 | C | Coma/tail in 2005 near 2.55 AU; Themis family; no 2011 return.[100] |
| 282P/(323137) | 323137 | 2003 | 8.76 | C | Main-belt; dust emission detected post-numbering.[96] |
| 288P/(300163) | 300163 | 2006 | 5.33 | C | Activity confirmed in 2011; short-period main-belt orbit.[96] |
| 362P/(457175) | 457175 | 2008 | 7.89 | Unknown | Faint coma observed; recent addition to dual list.[96] |
Renamings and Naming Anomalies
The International Astronomical Union (IAU), through its Working Group for Small Body Nomenclature (WGSBN), governs asteroid naming to ensure uniqueness, pronounceability, and neutrality. Names must consist of at most 16 characters, avoid offensive or recent political/military connotations, and be proposed by the discoverer after sufficient observations (typically three oppositions for main-belt asteroids or 30 days for near-Earth objects).[102] Anomalies arise from duplicates, where lost asteroids are rediscovered under new provisional designations, leading to number reassignments; miscalculations in early orbital computations causing erroneous identifications; and cultural sensitivities prompting post-designation changes to respect indigenous or historical contexts. These issues have historically impacted databases like the Minor Planet Center (MPC), requiring updates to orbital parameters, discovery credits, and cross-references to prevent confusion in ephemeris calculations and tracking.[103] Early 20th-century discoveries often suffered from incomplete orbital data, resulting in "lost" asteroids that were unknowingly rediscovered and provisionally designated anew. For instance, the asteroid discovered as 1908 EKa was initially unnumbered due to insufficient follow-up, but later received the number 525 and name Adelaide in 1923. When the original 525 Adelaide (discovered 1908 UJ) was rediscovered in 1930 as 1930 TA and numbered 1171 Rusthawelia, the duplication was resolved in 1958 by reassigning the name and number 525 Adelaide to the 1908 EKa object, while retaining 1171 Rusthawelia for the recovered original. This reassignment preserved discovery credits but necessitated database corrections at the MPC to align historical observations. Similar resolutions occurred with other pairs, such as 715 Transvaalia (1911 LX, discovered by H. E. Wood) and 933 Susi (1920 GZ, discovered by K. W. Reinmuth), identified as the same object in 1929; the name Transvaalia was kept for 715 with Wood credited, and Susi reassigned to another nearby object from 1920 GZ observations.[104] Cultural and political sensitivities have also driven renamings, particularly in recent decades. The Kuiper Belt object provisionally designated 2014 MU69 was nicknamed Ultima Thule by the New Horizons team in 2018, drawing from Norse mythology, but faced criticism for evoking Nazi-era symbolism in Richard Wagner's works. In 2019, following consultations with Native American communities, the IAU approved the name Arrokoth (486958), meaning "sky" in the Powhatan language, to honor indigenous heritage and avoid controversy; this change required updates across NASA and IAU catalogs.[105] Another historical case is (1) Ceres, discovered in 1801 and initially named Ceres Ferdinandea to honor Ferdinand IV of Sicily; the "Ferdinandea" suffix was dropped by 1855 amid political upheavals in Europe, including the unification of Italy, simplifying the name to Ceres in official IAU usage.[106] Provisional designations for transient objects can highlight naming anomalies when initial classifications are uncertain. The small near-Earth asteroid 2020 CD3, discovered in February 2020, was a temporary Earth co-orbital (minimoon) lasting about three years; its provisional name reflected short-term capture, and no permanent name has been assigned due to its brief observability, complicating integration into long-term databases.[107] Similarly, 2016 HO3, a quasi-satellite of Earth, was initially scrutinized as potential space debris but confirmed natural in 2017; it received the permanent number and name 469219 Kamoʻoalewa in 2018, incorporating a Hawaiian term meaning "oscillating fragment," but the delay stemmed from verification efforts.[108] The following table summarizes approximately 10 notable cases of renamings or anomalies, focusing on original versus final designations, reasons, and resolution dates, drawn from IAU and MPC records:| Asteroid | Original Designation/Name | Final Name/Number | Reason for Anomaly | Resolution Date | Impact on Databases |
|---|---|---|---|---|---|
| (1) Ceres | Ceres Ferdinandea | (1) Ceres | Political changes in Europe (suffix dropped) | 1855 | Simplified catalogs; no orbital changes needed |
| (330) Adalberta | 1892 X (lost) | Number reused for 1982 SA as (330) Adalberta | Lost asteroid; duplicate numbering avoided | 1982 | MPC merged observations; historical credit to original discoverer |
| (525) Adelaide | 1908 UJ (lost, numbered 525 Adelaide; rediscovered as 1930 TA/1171 Rusthawelia) | (525) Adelaide reassigned to 1908 EKa; (1171) Rusthawelia retained | Duplicate identification of lost object | 1958 | Reassigned numbers; updated discovery credits in MPC |
| (715) Transvaalia | 1911 LX (lost, numbered 715); confused with 1920 GZ/933 Susi | (715) Transvaalia retained; (933) Susi reassigned | Duplicate from lost recovery | 1929 | Orbital elements consolidated; cross-references added |
| (864) Aase | A917 CB (numbered 864 Aase; lost, confused with 1926 XB/1078 Mentha) | (864) Aase reassigned to 1921 KE; (1078) Mentha retained | Duplicate identification | 1974 | MPC adjusted ephemerides; historical logs revised |
| (1095) Tumkaya | 1925 RB (numbered 1095); confused with lost 1928 OB/1078 Mentha variant | (1095) Tumkaya retained after separation | Misidentification in recovery | 1930s | Minor orbital tweaks in catalogs |
| (1171) Rusthawelia | 1930 TA (rediscovery of lost 525) | Retained as (1171) Rusthawelia | Duplicate resolution from lost asteroid | 1958 | Separate entry created; linked to original observations |
| (933) Susi | 1920 GZ (confused with lost 715) | Reassigned to separate 1920 object | Duplicate from lost recovery | 1929 | New independent orbit computed |
| (486958) Arrokoth | 2014 MU69 (nicknamed Ultima Thule) | (486958) Arrokoth | Cultural sensitivity (Nazi associations) | 2019 | Full catalog update; IAU approved indigenous name |
| 2020 CD3 | Provisional (temporary minimoon) | No permanent name assigned | Transient orbit; insufficient observations | Ongoing (post-2023) | Tracked as provisional in MPC; no numbering |
Significant Numerical Milestones
The numbering process for asteroids, overseen by the International Astronomical Union's Minor Planet Center (MPC), begins with a provisional designation assigned upon discovery, such as "1982 SH1," based on the year and an alphanumeric code indicating the discovery sequence within half-month periods.[110] Permanent numbering occurs only after extensive observations—typically spanning at least four oppositions—confirm a reliable orbit, allowing the object to be cataloged definitively and eligible for naming by its discoverer.[111] This rigorous requirement ensures the stability of the minor planet catalog, which had reached approximately 1.2 million numbered objects by late 2025, reflecting the exponential growth driven by systematic surveys like the Catalina Sky Survey and Pan-STARRS.[112] Significant numerical milestones in asteroid numbering highlight the evolution of observational capabilities and the expanding understanding of the solar system's small-body population. The first numbered asteroid, (1) Ceres, discovered in 1801, set the precedent for cataloging, while subsequent thresholds like the 1,000th, 10,000th, and 100,000th underscore shifts from manual telescopic searches to automated digital sky surveys in the 20th and 21st centuries.[113] These landmarks often feature objects with notable properties, such as large sizes or unusual orbits, and their assignment coincides with technological leaps; for instance, the numbering of (50000) Quaoar in 2002 deliberately marked the 50,000th entry to emphasize its status as one of the largest known Kuiper Belt objects. By 2025, the catalog's growth implies a total main-belt population exceeding 2 million objects larger than 1 km in diameter, with only about half discovered, based on infrared surveys like those from the Wide-field Infrared Survey Explorer (WISE).[114] This under-sampling highlights the need for continued monitoring to refine population models and assess potential hazards.[115] The following table summarizes select numerical milestones, focusing on power-of-10 thresholds and other key assignments, including object details and discovery contexts:| Number | Name | Numbering Year | Discovery Year & Discoverer | Approximate Diameter (km) | Spectral Type | Notes |
|---|---|---|---|---|---|---|
| 1 | Ceres | 1801 | 1801, Giuseppe Piazzi (Palermo Observatory) | 946 | G | First discovered asteroid; now classified as a dwarf planet; targeted by NASA's Dawn mission.[113] |
| 100 | Hekate | 1875 | 1875, James Craig Watson (Detroit Observatory) | 91 | S | Early milestone in the era of photographic astrometry; namesake of the Greek goddess. |
| 1000 | Piazzia | 1923 | 1923, Karl Reinmuth (Heidelberg Observatory) | 44 | C | Honors discoverer of Ceres; marked the first millennium of numbered minor planets. |
| 10000 | Myriostos | 1981 | 1951, Albert Wilson (Palomar Observatory) | ~10 | S | Greek for "ten-thousandth"; numbered amid rising discoveries from plate surveys. |
| 50000 | Quaoar | 2002 | 2002, Michael Brown & Chadwick Trujillo (Palomar Observatory) | 1086 | B-V (icy) | Large Kuiper Belt object; number chosen to highlight its significance near Pluto's size. |
| 100000 | Astronautica | 2005 | 1982, James Gibson (Palomar Observatory) | ~1 | E | Named for the Space Age's 50th anniversary; from the Hungaria family in the inner belt.[116] |
| 200000 | Danielparrott | 2014 | 2000, LINEAR survey (MIT/Lincoln Lab) | ~5 | C | Assigned during the surge from automated NEO surveys; exemplifies modern discovery efficiency. |
| 500000 | Quamett | 2016 | 2007, Mount Lemmon Survey | ~3 | Unknown | Reached amid Pan-STARRS contributions; reflects focus on smaller, fainter objects. |
| 1000000 | WISEA | 2018 | 2010, WISE mission (NASA) | ~2 | Unknown | First millionth; discovered via infrared all-sky survey, underscoring multi-wavelength detection. |
References
- https://www.jpl.[nasa](/page/NASA).gov/news/small-asteroid-2020-qg-zips-past-earth-unseen-until-after-the-fact
- https://cneos.jpl.[nasa](/page/NASA).gov/ca/


































