Lightcurve-base 3D-model of Carlova on the top with an image of the asteroid on the bottom. | |
| Discovery | |
|---|---|
| Discovered by | Auguste Charlois |
| Discovery date | 11 March 1893 |
| Designations | |
| 1893 N | |
| Main belt | |
| Adjectives | Carlovian |
| Orbital characteristics | |
| Epoch 31 July 2016 (JD 2457600.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 111.79 yr (40832 d) |
| Aphelion | 3.53698 AU (529.125 Gm) |
| Perihelion | 2.46807 AU (369.218 Gm) |
| 3.00253 AU (449.172 Gm) | |
| Eccentricity | 0.17800 |
| 5.20 yr (1900.3 d) | |
| 350.473° | |
| 0° 11m 21.988s / day | |
| Inclination | 11.6967° |
| 132.551° | |
| 287.862° | |
| Physical characteristics | |
| 135±3 km | |
| Mass | (1.96±0.37)×1018 kg |
Mean density | 1.52±0.31 g/cm3 |
| 6.189594 h (0.2578998 d) | |
| 0.043±0.006 | |
| C | |
| 8.49 | |
360 Carlova is a very large main-belt asteroid. It is classified as a C-type asteroid and is probably composed of carbonaceous material. Dust activity due to sublimation has been detected on this asteroid, suggesting the presence of water ice in its interior.
The asteroid has a convex, roughly ellipsoid shape. The sidereal rotation period is 6.1873 hours with an axis of rotation along the ecliptic coordinates (l, b) = (95°±3°, 40°±1°). It was discovered by Auguste Charlois on 11 March 1893 in Nice.