360 Carlova
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| Discovery A | |
|---|---|
| Discoverer | Auguste Charlois |
| Discovery date | March 11, 1893 |
| Alternate designations B |
1893 N |
| Category | Main belt |
| Orbital elements C | |
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| 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 D | |
| 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 (geometric) | 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 carbonaceous material.
It was discovered by Auguste Charlois on March 11, 1893 in Nice.
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