10199 Chariklo
Diagram of Chariklo and its rings as seen during a stellar occultation on 3 June 2013. This diagram was constructed by plotting the respective time and location of the observatories that recorded the occultation. | |
| Discovery | |
|---|---|
| Discovered by | Spacewatch |
| Discovery site | Kitt Peak Obs. |
| Discovery date | 15 February 1997 |
| Designations | |
| (10199) Chariklo | |
| Pronunciation | /ˈkærəkloʊ/ |
Named after | Χαρικλώ Khariklō (Ancient Greek nymph) |
| 1997 CU26 | |
| centaur · distant | |
| Adjectives | Charikloan, Charikloian /kærəˈkloʊ(i)ən/ |
| Symbol | |
| Orbital characteristics | |
| Epoch 5 May 2025 (JD 2460800.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 36+ yr |
| Earliest precovery date | 5 November 1988 |
| Aphelion | 18.420 AU |
| Perihelion | 13.077 AU |
| 15.748 AU | |
| Eccentricity | 0.1696 |
| 62.50 yr (22,827 days) | |
| 123.744° | |
| 0° 0m 56.774s / day | |
| Inclination | 23.425° |
| 300.470° | |
| |
| 241.323° | |
| Saturn MOID | 4.710 AU |
| Uranus MOID | 3.186 AU |
| Physical characteristics | |
| Dimensions | (287.6+2.8 −3.0) × (270.4+2.8 −5.6) × (198.2+10.8 −5.4) km |
| 249.6+6.0 −4.6 km | |
| Mass | (5.9–6.9)×1018 kg |
Mean density | 0.73–0.85 g/cm3 |
| 7.004±0.036 h | |
North pole right ascension | 151.03°±0.14° (C1R ring) |
North pole declination | +41.81°±0.07° (C1R ring) |
| 0.037±0.001 | |
| |
| ~19 | |
| 6.8–7.3 | |
10199 Chariklo /ˈkærəkloʊ/ is a ringed asteroid or centaur in the outer Solar System. It is the largest known centaur, with a diameter of about 250 km (160 mi). It orbits the Sun between Saturn and Uranus with an orbital period of 62.5 years. It was discovered on 15 February 1997 by the University of Arizona's Spacewatch project at Kitt Peak National Observatory. Chariklo has a dark, reddish surface composed of water ice, silicate minerals, amorphous carbon, and various complex organic compounds (also known as tholins).
Chariklo's ring system consists of two narrow rings of icy particles in orbit around the object. The rings of Chariklo were discovered in 2013, when astronomers observed Chariklo occulting or passing in front of a star. Chariklo was the first minor planet discovered to have rings, and as of 2025, it is one of the four minor planets known to have rings (the three others being 2060 Chiron, Haumea, and Quaoar). It is unknown what keeps Chariklo's rings stable, as it has been predicted that they should decay within a few million years. Astronomers have hypothesized that Chariklo's rings might be maintained by the gravitational influence of yet-undiscovered shepherd moons orbiting Chariklo. The origin of Chariklo's rings is uncertain, with various possible explanations including ejection of surface material via outgassing or tidal disruption of a moon around Chariklo.