360 Carlova
| Discovery A | |
|---|---|
| Discoverer | Auguste Charlois |
| Discovery Date | March 11, 1893 |
| Alternate Designations | 1893 N B |
| Category | Main belt |
| Orbital Elements C Epoch 30 January, 2005 (JD 2453400.5) | |
| Eccentricity (e) | 0.182 |
| Semi-Major Axis (a) | 448.556 Gm (2.998 AU) |
| Perihelion (q) | 366.965 Gm (2.453 AU) |
| Aphelion (Q) | 530.147 Gm (3.544 AU) |
| Orbital Period (P) | 1896.387 d (5.19 a) |
| Mean Orbital Speed | 17.2 km/s |
| Inclination (i) | 11.713° |
| Longitude of the Ascending Node (Ω) | 132.67° |
| Argument of Perihelion (ω) | 288.654° |
| Mean Anomaly (M) | 273.152° |
| Physical Characteristics | |
| Dimensions | 116.0 km |
| Mass | unknown |
| Density | unknown |
| Surface Gravity | unknown |
| Escape Velocity | unknown |
| Rotation Period | unknown |
| Spectral Class | C |
| Absolute Magnitude | 8.48 |
| Albedo | unknown |
| Mean Surface Temperature | unknown |
360 Carlova is a very large Main belt asteroid. It is classified as a C-type asteroid and is probably composed of privitive carbonates.
It was discovered by Auguste Charlois on March 11, 1893 in Nice.
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