326 Tamara
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Discovery A | |
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Discoverer | Johann Palisa |
Discovery date | March 19, 1892 |
Alternate designations B |
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Category | Main belt |
Orbital elements C | |
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Eccentricity (e) | 0.191 |
Semi-major axis (a) | 346.755 Gm (2.318 AU) |
Perihelion (q) | 280.598 Gm (1.876 AU) |
Aphelion (Q) | 412.911 Gm (2.76 AU) |
Orbital period (P) | 1288.948 d (3.53 a) |
Mean orbital speed | 19.56 km/s |
Inclination (i) | 23.723° |
Longitude of the ascending node (Ω) |
32.335° |
Argument of perihelion (ω) |
238.429° |
Mean anomaly (M) | 292.783° |
Physical characteristics D | |
Dimensions | 93.0 km |
Mass | unknown |
Density | unknown |
Surface gravity | unknown |
Escape velocity | unknown |
Rotation period | unknown |
Spectral class | C |
Absolute magnitude | 9.36 |
Albedo (geometric) | unknown |
Mean surface temperature |
unknown |
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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Vulcanoids | Near-Earth asteroids | Main belt | Jupiter Trojans | Centaurs | Damocloids | Comets | Trans-Neptunians (Kuiper belt · Scattered disc · Oort cloud) |
For other objects and regions, see: asteroid groups and families, binary asteroids, asteroid moons and the Solar system For a complete listing, see: List of asteroids. See also Pronunciation of asteroid names and Meanings of asteroid names. |