Discovery[1] | |
---|---|
Discovered by | T. Kobayashi |
Discovery site | Ōizumi Obs. |
Discovery date | 2 December 1996 |
Designations | |
(11133) Kumotori | |
Named after | Mount Kumotori (Japanese mountain)[2] |
1996 XY | |
main-belt · (outer)[3] background[4] | |
Orbital characteristics[1] | |
Epoch 23 March 2018 (JD 2458200.5) | |
Uncertainty parameter 0 | |
Observation arc | 28.27 yr (10,324 d) |
Aphelion | 2.9313 AU |
Perihelion | 2.6210 AU |
2.7762 AU | |
Eccentricity | 0.0559 |
4.63 yr (1,690 d) | |
54.098° | |
0° 12m 47.16s / day | |
Inclination | 10.689° |
83.096° | |
158.34° | |
Physical characteristics | |
8.96 km (calculated)[3] | |
4.634±0.0005 h[5] | |
0.057 (assumed)[3] | |
L[6] · C (assumed)[3] | |
13.517±0.003 (R)[5] 13.6[1] · 13.97[3] 14.10±0.46[6] | |
11133 Kumotori (provisional designation 1996 XY) is a background asteroid from the central regions of the asteroid belt, approximately 9 kilometers (6 miles) in diameter. It was discovered on 2 December 1996, by Japanese amateur astronomer Takao Kobayashi at his Ōizumi Observatory. The asteroid was named after Mount Kumotori near Tokyo.[2] It has a rotation period of 4.6 hours.[3]
jpldata
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was invoked but never defined (see the help page).AstDys-object
was invoked but never defined (see the help page).Waszczak-2015
was invoked but never defined (see the help page).Veres-2015
was invoked but never defined (see the help page).