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Encyclopedia > Eunomia asteroid

The Eunomia family is a group of several hundred asteroids that share similar orbital and spectral properties. It is believed to be a result of the collision and breakdown of a larger parent body. The group is named after its largest and first-found member, 15 Eunomia.


Eunomia asteroids are S-type asteroids, so they are quite bright in color and their composition is likely a mixture of nickel-iron with silicates similar to 243 Ida or 951 Gaspra. A few C-type or other asteroids lie within the group, but they are most likely interlopers and not related to other Eunomia asteroids.


The Eunomia family is located between 3:1 and 8:3 resonances with Jupiter.


Orbital elements for the Eunomia family:


The Minor Planets
Vulcanoids | Main belt | Groups and Families | Near-Earth objects | Jupiter Trojans
Centaurs | Trans-Neptunians | Damocloids | Comets | Kuiper Belt | Oort Cloud
(For other objects and regions, see: Binary asteroids, Asteroid moons and the Solar system)
(For a complete listing, see: List of asteroids)

  Results from FactBites:
 
15 Eunomia - Wikipedia, the free encyclopedia (829 words)
It is the largest of the stony (S-type) asteroids, and somewhere between the 8th to 12th largest Main Belt asteroid overall (uncertainty in diameters causes uncertainty in its ranking).
The range of compositions of the remaining Eunomia family members, formed by a collision of the common parent body, is large enough to encompass all the surface variations on Eunomia itself.
An older explanation of the compositional differences, that Eunomia is a mantle fragment of a far larger parent body (with a bit of crust on one end, and a bit of core on the other) appears to be ruled out by studies of the mass distribution of the entire Eunomia family of asteroids.
asteroid (1793 words)
Most asteroids move in orbits that are somewhat more inclined and eccentric than those of the major planets (with the exception of Pluto) – the orbit of an average main-belt asteroid being inclined at about 10° to the plane of the ecliptic with an eccentricity of about 0.15.
Following its discovery, an asteroid is given a preliminary designation that consists of the year of discovery, an upper case letter to indicate the half-month in that year (A=Jan 1-15, B=Jan 16-31,..., Y=Dec 16-31, the letter “I” being omitted), and a second upper case letter in sequence.
The distribution of the various classes throughout the asteroid belt is highly structured, suggesting that many asteroids formed at or near their present distances from the Sun and are representative of the composition of the solar nebula (not including hydrogen and helium) at these locations.
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