Asteroids, or small rocky bodies of the Solar System, exhibit an impressive diversity of sizes. Although most are small fragments a few meters in size, some reach several hundred kilometers in diameter. This classification is primarily based on measurements from space missions and telescopic observations combined with modeling of their shapes. List of the largest asteroids classified by average diameter:
Ceres, the largest asteroid and also a dwarf planet, constitutes about 25% of the total mass of the main asteroid belt. Its spherical shape and internal differentiation suggest early thermal evolution, possibly driven by radioactive elements. It has a crust rich in salts and hydrated clays and may even harbor a subsurface ocean.
Vesta is one of the few asteroids to have been explored up close, notably by the Dawn probe. With a diameter of 525 km, Vesta has a basaltic surface, evidence of a volcanic past. It is also the likely parent body of the HED (howardites, eucrites, and diogenites) meteorites found on Earth.
Vesta is the second-largest asteroid and the brightest visible from Earth. Its surface features complex geological characteristics, including a massive impact crater near its south pole. The Dawn mission revealed that Vesta has a differentiated structure with an iron core, similar to terrestrial planets.
Pallas, similar in size to Vesta, has a highly inclined orbit relative to the ecliptic plane. Its visible spectrum indicates a surface rich in hydrated silicates. Less studied than Ceres and Vesta, it may have undergone partial differentiation.
Hygiea, the fourth-largest, has a nearly spherical shape despite a relatively low density suggesting a porous or water-rich composition. In 2019, images from the VLT (Very Large Telescope) helped determine its dimensions and overall shape.
Hygiea is the main member of the Hygiea asteroid family and could be reclassified as a dwarf planet due to its spherical shape. It is the darkest of the four large asteroids, with a surface likely composed of primitive carbonaceous materials dating back to the formation of the Solar System.
Interamnia, the fifth-largest, is an F-type asteroid, belonging to a dark and primitive class. Its observation is difficult due to its low albedo and distance. It remains one of the most massive objects over 300 km in diameter in the belt.
The study of asteroids, particularly the large ones, provides valuable clues about the conditions that prevailed during the formation of the Solar System 4.6 billion years ago. These celestial bodies are considered "fossils" of the primordial Solar System, preserving in their chemical composition and structure invaluable information about planetary formation processes.
Rank | Name | Average diameter (km) | Dimensions (km) | Type | Discovery year |
---|---|---|---|---|---|
1 | Ceres | 940 | 964×964×892 | C (dwarf planet) | 1801 |
2 | Vesta | 525 | 573×557×446 | V | 1807 |
3 | Pallas | 512 | 550×516×476 | B | 1802 |
4 | Hygiea | 430 | 450×430×424 | C | 1849 |
5 | Interamnia | 326 | 350×304×290 | F | 1910 |
6 | Europa | 315 | 360×315×240 | C | 1858 |
7 | Davida | 289 | 357×294×231 | C | 1903 |
8 | Sylvia | 286 | 385×265×230 | X | 1866 |
9 | Hektor | 250 | 403×200 | D | 1907 |
10 | Euphrosyne | 248 | 268×248×240 | C | 1854 |
11 | Juno | 240 | 290×240×190 | S | 1804 |
12 | Psyche | 226 | 240×185×145 | M | 1852 |
13 | Cybele | 222 | 240×230×190 | X | 1861 |
14 | Thisbe | 218 | 225×205×190 | B | 1852 |
15 | Camilla | 215 | 250×220×190 | C | 1868 |
16 | Herculina | 212 | 230×200×180 | S | 1872 |
17 | Doris | 210 | 225×210×190 | C | 1857 |
18 | Iris | 200 | 240×200×160 | S | 1847 |
19 | Patientia | 198 | 210×195×180 | C | 1899 |
20 | Amphitrite | 195 | 210×190×175 | S | 1854 |
21 | Lutetia | 190 | 132×101×76 | M | 1852 |
22 | Bamberga | 185 | 230×190×130 | C | 1892 |
23 | Egeria | 180 | 195×175×160 | G | 1850 |
24 | Elektra | 178 | 215×155×150 | G | 1873 |
25 | Eunomia | 175 | 190×170×150 | S | 1851 |
26 | Fortuna | 172 | 180×170×150 | G | 1852 |
27 | Juno | 170 | 190×160×140 | S | 1804 |
28 | Metis | 168 | 180×160×140 | S | 1848 |
29 | Nemausa | 165 | 175×160×140 | C | 1858 |
30 | Bellona | 160 | 170×155×140 | S | 1854 |
Type | Classification | Composition | Albedo | Location | Example |
---|---|---|---|---|---|
C | Carbonaceous | Silicates, clays, organic compounds | 0.03-0.10 (very dark) | Outer belt | Hygiea |
S | Silicaceous | Silicate minerals + nickel-iron | 0.10-0.22 | Inner belt | Iris |
M | Metallic | Nickel-iron cores | 0.10-0.18 | Mid-belt | Psyche |
V | Vestoid | Basaltic lava | 0.30-0.40 | Inner belt | Vesta |
B | Bright Carbonaceous | Primitive carbon compounds | 0.04-0.08 | Outer belt | Pallas |
F | Dark Carbonaceous | Hydrated minerals | 0.03-0.07 | Mid-belt | Interamnia |
G | Carbonaceous (phyllosilicates) | Clay minerals | 0.05-0.09 | Mid-belt | Ceres |
D | Organic-rich | Complex organics + ice | 0.02-0.05 | Jupiter Trojans | Hektor |
X | Metallic/Silicate mix | Variable composition | 0.05-0.35 | Various | Sylvia |
P | Primitive organic | Organic compounds + silicates | 0.02-0.06 | Outer belt | Bamberga |