758 Mancunia

758 Mancunia is a minor planet orbiting the Sun. It was discovered in 1912 from Johannesburg by H. E. Wood, a Mancunian. This object is orbiting at a distance of 3.19 AU with a period of 5.70 years and an eccentricity (ovalness) of 0.15. The orbital plane is inclined at an angle of 5.61° to the plane of the ecliptic.

758 Mancunia
Discovery
Discovered byH. E. Wood
Discovery siteJohannesburg
Discovery date18 May 1912
Designations
MPC designation
(758) Mancunia
Pronunciation/mænˈkjuːniə/
Alternative designations
1912 PE
Orbital characteristics
Epoch 31 July 2016 (JD 2457600.5)
Uncertainty parameter 0
Observation arc101.39 yr (37034 d)
Aphelion3.6704 AU (549.08 Gm)
Perihelion2.7081 AU (405.13 Gm)
Semi-major axis
3.1893 AU (477.11 Gm)
Eccentricity0.15086
Orbital period (sidereal)
5.70 yr (2080.3 d)
Mean anomaly
260.973°
Mean motion
0° 10m 22.98s / day
Inclination5.6102°
Longitude of ascending node
106.200°
314.999°
Earth MOID1.72323 AU (257.792 Gm)
Jupiter MOID1.66575 AU (249.193 Gm)
TJupiter3.172
Physical characteristics
Mean radius
42.74±3.35 km
43.54 ± 0.655 km
Mass(9.31 ± 0.80) × 1017 kg
Mean density
2.69 ± 0.26 g/cm3
Synodic rotation period
12.7253 h (0.53022 d)
0.1317±0.023
8.16

    Observation of this asteroid in 1996 suggested a rotation period of 6.902 hours. However, radar observations from Arecibo indicated this may be in error. Independent photometry measurements made during December 2006 were combined to determine an estimated period nearly double that of the original, or 12.7253±0.0006 h with a brightness variation amplitude of 0.26±0.02 in magnitude. A high radar albedo indicates this object is most likely metallic. Dips in the radar echo suggests there are large concavities on both sides. It is classified as an X-type asteroid in the Tholen taxonomy and spans a girth of 85±7 km.

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