326 Tamara
| Discovery | |
|---|---|
| Discovered by | Johann Palisa |
| Discovery date | 19 March 1892 |
| Designations | |
|
Named after
|
Tamar |
| Main belt | |
| Orbital characteristics | |
| 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) |
| Jupiter Tisserand parameter | 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 March 19, 1892 in Vienna.
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