360 Carlova
From Wikipedia, the free encyclopedia
Discovery | |
---|---|
Discovered by | Auguste Charlois |
Discovery date | 11 March 1893 |
Designations | |
Alternative names | 1893 N |
Minor planet category | Main belt |
Orbital characteristics | |
Epoch 30 January 2005 (JD 2453400.5) | |
Aphelion | 530.147 Gm (3.544 AU) |
Perihelion | 366.965 Gm (2.453 AU) |
Semi-major axis | 448.556 Gm (2.998 AU) |
Eccentricity | 0.182 |
Orbital period | 1896.387 d (5.19 a) |
Average orbital speed | 17.2 km/s |
Mean anomaly | 273.152° |
Inclination | 11.713° |
Longitude of ascending node | 132.67° |
Argument of perihelion | 288.654° |
Physical characteristics | |
Dimensions | 116.0 km |
Mass | unknown |
Mean density | unknown |
Equatorial surface gravity | unknown |
Escape velocity | unknown |
Rotation period | unknown |
Albedo | unknown |
Temperature | unknown |
Spectral type | C |
Absolute magnitude (H) | 8.48 |
|
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 11 March 1893 in Nice.
|
|
This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.