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The Largest Asteroids
# Name Year of Discovery Orbit’s Semimajor Axis (AU) Diameter (km) Compositional Class
1 Ceres 1801 2.77 940 C (carbonaceous)
2 Pallas 1802 2.77 540 C (carbonaceous)
3 Juno 1804 2.67 265 S (stony)
4 Vesta 1807 2.36 510 basaltic
10 Hygiea 1849 3.14 410 C (carbonaceous)
16 Psyche 1852 2.92 265 M (metallic)
31 Euphrosyne 1854 3.15 250 C (carbonaceous)
52 Europa 1858 3.10 280 C (carbonaceous)
65 Cybele 1861 3.43 280 C (carbonaceous)
87 Sylvia 1866 3.48 275 C (carbonaceous)
451 Patientia 1899 3.06 260 C (carbonaceous)
511 Davida 1903 3.16 310 C (carbonaceous)
704 Interamnia 1910 3.06 310 C (carbonaceous)

The asteroids all revolve about the Sun in the same direction as the planets, and most of their orbits lie near the plane in which Earth and other planets circle. The majority of asteroids are in the asteroid belt    , the region between Mars and Jupiter that contains all asteroids with orbital periods between 3.3 to 6 years ( [link] ). Although more than 75% of the known asteroids are in the belt, they are not closely spaced (as they are sometimes depicted in science fiction movies). The volume of the belt is actually very large, and the typical spacing between objects (down to 1 kilometer in size) is several million kilometers. (This was fortunate for spacecraft like Galileo, Cassini, Rosetta , and New Horizons, which needed to travel through the asteroid belt without a collision.)

Asteroids in the solar system.

Asteroids in the Solar System. All known asteroids as of 2006 are plotted in this diagram of the Solar System. At center is the Sun, with the orbits of the inner planets drawn as blue circles. At the outer edge of the diagram the orbit of Jupiter is drawn as a blue circle. The vast majority of asteroids lie between the orbits of Mars and Jupiter, and are plotted here as thousands of white dots. Also plotted are the three “families” of asteroids whose orbits are largely determined by the influence of Jupiter. They are the “Greeks”, located at lower right, the “Trojans” at far left and the “Hildas” at upper right, inside the orbit of Jupiter.
This computer-generated diagram shows the positions of the asteroids known in 2006. If the asteroid sizes were drawn to scale, none of the dots representing an asteroid would be visible. Here, the asteroid dots are too big and give a false impression of how crowded the asteroid belt would look if you were in it. Note that in addition to those in the asteroid belt, there are also asteroids in the inner solar system and some along Jupiter’s orbit (such as the Trojans and Greeks groups), controlled by the giant planet’s gravity.

Still, over the long history of our solar system, there have been a good number of collisions among the asteroids themselves. In 1918, the Japanese astronomer Kiyotsugu Hirayama found that some asteroids fall into families , groups with similar orbital characteristics. He hypothesized that each family may have resulted from the breakup of a larger body or, more likely, from the collision of two asteroids. Slight differences in the speeds with which the various fragments left the collision scene account for the small spread in orbits now observed for the different asteroids in a given family. Several dozen such families exist, and observations have shown that individual members of most families have similar compositions, as we would expect if they were fragments of a common parent.

Practice Key Terms 2

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Source:  OpenStax, Astronomy. OpenStax CNX. Apr 12, 2017 Download for free at http://cnx.org/content/col11992/1.13
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