4 Vesta
| |||||
|---|---|---|---|---|---|
| Discovery | |||||
| Who | Heinrich Wilhelm Olbers | ||||
| When | March 29, 1807 | ||||
| Alternate Designation(s) | |||||
| Orbital Characteristics | |||||
| Category | Main belt (Vesta family) | ||||
| Semi-Major Axis | 353.323 Gm (2.362 AU) | ||||
| Perihelion | 321.956 Gm (2.152 AU) | ||||
| Aphelion | 384.689 Gm (2.571 AU) | ||||
| Eccentricity | 0.089 | ||||
| Revolution Period | 1325.768 d (3.63 yr) | ||||
| Inclination | 7.133° | ||||
| Mean Orbital Speed | 19.38 km/s | ||||
| Physical Characteristics | |||||
| Dimensions | 468.3 km | ||||
| Mass | 2.701×1020 kg | ||||
| Density | 5.0 g/cm³ | ||||
| Surface Gravity | 0.30 m/s² | ||||
| Escape Velocity | 0.39 km/s | ||||
| Rotation Period | 0.2226 d | ||||
| Spectral Class | V-type asteroid | ||||
| Absolute Magnitude | 3.20 | ||||
| Albedo | 0.423 | ||||
| Mean Surface Temperature | ~223 K | ||||
It was discovered by the German astronomer Heinrich Wilhelm Olbers on March 29, 1807. He allowed the prominent mathematician Carl Friedrich Gauss to name the asteroid after the Roman virgin goddess of home and hearth, Vesta.
After the discovery of Vesta in 1807, no other asteroids were discovered for 38 years; the next was 5 Astraea.
In the earliest times of the Solar system, Vesta was hot enough for its interior to melt. This resulted in differentiation of the asteroid. It is likely to have a layered structure: a metallic iron-nickel core and an overlying olivine mantle. The surface is basaltic rock from ancient lava flows, obviously some kind of short-lived volcanic activity was present. This makes Vesta unlike any other asteroid and in a sense it is more like the terrestrial planets, which underwent similar geological processes.
However, it was not only of its kind; there were originally probably dozens of similar large planetesimals, but all the other bodies were shattered into families of smaller asteroids during the chaotic early times. Metallic iron-nickel asteroids are thought to originate from the cores of such bodies, with stony ones coming from their crusts and mantles.
Not even Vesta has survived intact. In 1996 the Hubble Space Telescope (see image below) detected a huge crater on Vesta, 430 kilometres across and perhaps a billion years old. It is thought that this crater may be the source of the small V-type asteroids (or Vestoids) observed today.
in May 1996 from 177 Gm'']]In 2001 one such asteroid, 1929 Kollaa, was not only determined to be a piece from Vesta, but also the exact location of its formation was traced to deep in the crust.
The Yarkovsky effect along with perturbing planets and asteroids causes scattering among the Vesta family. Some of the asteroids like 9969 Braille have become Near-Earth asteroids. Smaller fragments have even rained down as meteoritess. Vesta is thought to be the source of the HED meteorites.
Our knowledge about Vesta is expected to increase tremendously when the Dawn probe enters an orbit around the asteroid in 2010.
References
External links
The Minor Planets
Vulcanoids | Main belt | | Near-Earth objects | Jupiter Trojans
Centaurs | Trans-Neptunians | Damocloids | Comets | Kuiper Belt | Oort Cloud
(For other objects and regions, see: , Asteroid moons and the Solar system)
(For a complete listing, see: List of asteroids)