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Main-belt asteroid From Wikipedia, the free encyclopedia
336 Lacadiera is a large Main belt asteroid.[1] It is classified as a D-type asteroid and is probably composed of organic rich silicates, carbon and anhydrous silicates. The asteroid was discovered by Auguste Charlois on 19 September 1892 in Nice.
Discovery | |
---|---|
Discovered by | Auguste Charlois |
Discovery date | 19 September 1892 |
Designations | |
(336) Lacadiera | |
Pronunciation | Occitan: [lakaˈdjeɾɔ] |
Named after | La Cadiera |
1892 D | |
Main belt | |
Orbital characteristics[1] | |
Epoch 31 July 2016 (JD 2457600.5) | |
Uncertainty parameter 0 | |
Observation arc | 123.57 yr (45133 d) |
Aphelion | 2.4661 AU (368.92 Gm) |
Perihelion | 2.0373 AU (304.78 Gm) |
2.2517 AU (336.85 Gm) | |
Eccentricity | 0.095224 |
3.38 yr (1234.2 d) | |
324.173° | |
0° 17m 30.12s / day | |
Inclination | 5.6530° |
235.044° | |
2023-Sep-03 | |
31.129° | |
Physical characteristics | |
Dimensions | 69.31±2.4 km |
13.70 h (0.571 d) | |
0.0459±0.003 | |
D | |
9.76 | |
In 2000, the asteroid was detected by radar from the Arecibo Observatory at a distance of 1.21 AU. The resulting data yielded an effective diameter of 69 ± 9 km.[2]
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