| Lightcurve-base 3D-model of 168 Sibylla. | |
| Discovery [1] | |
|---|---|
| Discovered by | J. C. Watson |
| Discovery site | Ann Arbor |
| Discovery date | 28 September 1876 |
| Designations | |
| (168) Sibylla | |
| Pronunciation | /sɪˈbɪlə/ [2] |
Named after | Sibyls |
| A876 SA; 1911 HF; 1949 MO | |
| main-belt | |
| Adjectives | Sibyllian /sɪˈbɪliən/ |
| Orbital characteristics [3] [4] | |
| Epoch 31 July 2016 (JD 2457600.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 136.01 yr (49676 d) |
| Aphelion | 3.6215 AU (541.77 Gm) |
| Perihelion | 3.1417 AU (469.99 Gm) |
| 3.3816 AU (505.88 Gm) | |
| Eccentricity | 0.070943 |
| 6.22 yr (2271.4 d) | |
Average orbital speed | 16.19 km/s |
| 171.517° | |
| 0° 9m 30.564s / day | |
| Inclination | 4.6617° |
| 205.959° | |
| 173.920° | |
| Physical characteristics | |
| Dimensions | 148.39±4.0 km [3] 149.06 ± 4.29 km [5] |
| Mass | (3.92 ± 1.80) × 1018 kg [5] |
Mean density | 2.26 ± 1.05 g/cm3 [5] |
| 47.009 h (1.9587 d) | |
| 23.82 hours [6] | |
| 0.0535±0.003 | |
| C | |
| 7.94 | |
168 Sibylla is a large main-belt asteroid, discovered by Canadian-American astronomer J. C. Watson on September 28, 1876. It was most likely named for the Sibyls, referring to the Ancient Greek female oracles. [7] Based upon its spectrum this object is classified as a C-type asteroid, which indicates it is very dark and composed of primitive carbonaceous materials. 168 Sibylla is a Cybele asteroid, orbiting beyond most of the main-belt asteroids.
Photometric observations of this asteroid made at the Torino Observatory in Italy during 1990–1991 were used to determine a synodic rotation period of 23.82 ± 0.004 hours. [6] The shape of this slowly rotating object appears to resemble an oblate spheroid. [8]