326 Tamara
Appearance
Discovery | |
---|---|
Discovered by | Johann Palisa |
Discovery date | 19 March 1892 |
Designations | |
(326) Tamara | |
Named after | Tamar |
Main belt | |
Orbital characteristics[1] | |
Epoch 31 July 2016 (JD 2457600.5) | |
Uncertainty parameter 0 | |
Observation arc | 122.57 yr (44770 d) |
Aphelion | 2.75738 AU (412.498 Gm) |
Perihelion | 1.87764 AU (280.891 Gm) |
2.31751 AU (346.695 Gm) | |
Eccentricity | 0.18980 |
3.53 yr (1288.6 d) | |
Average orbital speed | 19.56 km/s |
26.2160° | |
0° 16m 45.714s / day | |
Inclination | 23.7294° |
32.2069° | |
238.542° | |
Earth MOID | 0.94523 AU (141.404 Gm) |
Jupiter MOID | 2.43855 AU (364.802 Gm) |
TJupiter | 3.445 |
Physical characteristics | |
Dimensions | 93.00±1.7 km |
Mass | unknown |
Mean density | unknown |
Equatorial surface gravity | unknown |
Equatorial escape velocity | unknown |
14.445 h (0.6019 d) | |
0.0368±0.001 | |
Temperature | unknown |
C | |
9.36 | |
326 Tamara is a large Main belt asteroid. It is classified as a C-type asteroid and is probably composed of carbonaceous material.
It was discovered by Johann Palisa on 19 March 1892 in Vienna.
References
- ^ "326 Tamara". JPL Small-Body Database. NASA/Jet Propulsion Laboratory. Retrieved 11 May 2016.
External links