An asteroid is a solid object, smaller than a planet, which in our Solar System orbits the Sun. Most asteroids are believed to be remnants of the protoplanetary disc or fragments of larger asteroids. The vast majority of asteroids are within the main asteroid belt between Mars and Jupiter. Studying the sizes, shapes, orbits, and distribution of asteroids, as well as their composition and age through meteorites which came from asteroids, gives us precious information on the early evolution of our solar system. They are precious gifts to humanity so that we can understand our solar system, learn how to avoid their collision with the Earth, and utilize them.
Asteroids in the solar system
Hundreds of thousands of asteroids have been discovered within the solar system, and the rate of discovery has been increasing. Each asteroid discovered is given a tentative name, then after at least three sightings and orbit determination, it is given a number, then a permanent name.
Current estimates put the total number of asteroids above 1 kilometer in diameter in the solar system to be between 1.1 and 1.9 million. The largest asteroid in the inner solar system is 1 Ceres, with a diameter of about 900 kilometers. Two other large inner solar system belt asteroids are 2 Pallas and 4 Vesta; both have diameters of about 500 kilometers. Vesta is the only main belt asteroid that is sometimes visible to the naked eye (in some very rare occasions, a near-Earth asteroid may be visible without technical aid).
The mass of all the asteroids of the Main Belt is estimated to be about 3.0-3.6x1021 kg, or about 4 percent of the mass of our moon. Of this, 1 Ceres comprises 950x1018 kg, some 32 percent of the total. Adding in the next three most massive asteroids, 4 Vesta (9 percent), 2 Pallas (7 percent), and 10 Hygiea (3 percent), bring this figure up to 51 percent; while the three after that, 511 Davida (1.2 percent), 704 Interamnia (1.0 percent), and 3 Juno (0.9 percent), only add another 3 percent to the total mass. The number of asteroids then increases exponentially as their individual masses decrease.
Asteroids around other stars than our Sun would be called extrasolar asteroids. Because asteroids are much smaller than planets, detection of them is currently difficult. The distinction between planets and asteroids is not very clear. Large asteroids such as Ceres and Vesta could possibly be classified as planets, because they have not been destroyed since the formation of the solar system.
Asteroids are commonly classified into groups based on the characteristics of their orbits and details of the spectrum of sunlight they reflect.
Orbit groups and families
Many asteroids have been placed in groups and families based on their orbital characteristics. It is customary to name a group of asteroids after the first member of that group to be discovered. Groups are relatively loose dynamical associations, whereas families are much "tighter" and are thought to be products of the catastrophic break-up of a large parent asteroid sometime in the past.
In 1975, an asteroid taxonomic system—based on color, albedo, and spectral shape—was developed by Clark R. Chapman, David Morrison, and Ben Zellner. These properties are thought to correspond to the composition of the asteroid's surface material. Originally, they classified only three types of asteroids:
- C-type asteroids - carbonaceous, 75 percent of known asteroids
- S-type asteroids - silicaceous, 17 percent of known asteroids
- M-type asteroids - metallic, most of the remaining asteroids
This list has since been expanded to include a number of other asteroid types. The number of types continues to grow as more asteroids are studied. Notably, in 1984, David Tholen developed the 15-class taxonomy, which became very popular.
Note that the proportion of known asteroids falling into the various spectral types does not necessarily reflect the proportion of all asteroids of that type; some types are easier to detect than others, biasing the totals.
Compositions of asteroids and meteorite parent bodies
Originally, spectral designations were based on inferences of an asteroid's composition, thus giving insight on which asteroids are likely parent bodies of meteorites. Yet, the correspondence between spectral class and composition is not always very good, and various classifications are in use. This has led to significant confusion. While asteroids of different spectral classifications are likely to be composed of different materials, there are no assurances that asteroids within the same taxonomic class are composed of similar materials. The situation may be made worse by the possibility of space weathering, as observed in lunar soils. Space weathering is believed to be at the root of a long-standing controversy that ordinary chondrites, which are the most abundant meteorites, do not seem abundant in the main asteroid belt.
Recently, higher-quality telescopic observations, spacecraft explorations, and additional laboratory studies of meteorites have been conducted, leading to greater understanding of space weathering and other effects. These are expected to improve spectral classification and our ability to analyze asteroid composition remotely, thus linking meteorites with their parent body asteroids.
Historical discovery methods
Asteroid discovery methods have drastically improved over the past two centuries.
In the last years of the eighteenth century, Baron Franz Xaver von Zach organized a group of 24 astronomers to search the sky for the "missing planet" predicted at about 2.8 AU from the Sun by the Titius-Bode law, partly as a consequence of the discovery, by Sir William Herschel in 1781, of the planet Uranus at the distance "predicted" by the law. This task required that hand-drawn sky charts be prepared for all stars in the zodiacal band down to an agreed-upon limit of faintness. On subsequent nights, the sky would be charted again and any moving object would, hopefully, be spotted. The expected motion of the missing planet was about 30 seconds of arc per hour, readily discernable by observers.
Ironically, the first asteroid, 1 Ceres, was not discovered by a member of the group, but rather by accident in 1801 by Giuseppe Piazzi director, at the time, of the observatory of Palermo, in Sicily. He discovered a new star-like object in Taurus and followed the displacement of this object during several nights. His colleague, Carl Friedrich Gauss, used these observations to determine the exact distance from this unknown object to the Earth. Gauss' calculations placed the object between the planets Mars and Jupiter. Piazzi named it after Ceres, the Roman goddess of agriculture.
Three other asteroids (2 Pallas, 3 Juno, 4 Vesta) were discovered over the next few years, with Vesta found in 1807. After eight more years of fruitless searches, most astronomers assumed that there were no more and abandoned any further searches.
However, Karl Ludwig Hencke persisted, and began searching for more asteroids in 1830. Fifteen years later, he found 5 Astraea, the first new asteroid in 38 years. He also found 6 Hebe less than two years later. After this, other astronomers joined in the search and at least one new asteroid was discovered every year after that (except the wartime year 1945). Notable asteroid hunters of this early era were J. R. Hind, Annibale de Gasparis, Robert Luther, H. M. S. Goldschmidt, Jean Chacornac, James Ferguson, Norman Robert Pogson, E. W. Tempel, J. C. Watson, C. H. F. Peters, A. Borrelly, J. Palisa, Paul Henry and Prosper Henry and Auguste Charlois.
In 1891, however, Max Wolf pioneered the use of astrophotography to detect asteroids, which appeared as short streaks on long-exposure photographic plates. This drastically increased the rate of detection compared with previous visual methods: Wolf alone discovered 248 asteroids, beginning with 323 Brucia, whereas only slightly more than 300 had been discovered up to that point. Still, a century later, only a few thousand asteroids were identified, numbered and named. It was known that there were many more, but most astronomers did not bother with them, calling them "vermin of the skies.”
Modern discovery methods
Until 1998, asteroids were discovered by a four-step process. First, a region of the sky was photographed by a wide-field telescope. Pairs of photographs were taken, typically one hour apart. Multiple pairs could be taken over a series of days. Second, the two films of the same region were viewed under a stereoscope. Any body in orbit around the Sun would move slightly between the pair of films. Under the stereoscope, the image of the body would appear to float slightly above the background of stars. Third, once a moving body was identified, its location would be measured precisely using a digitizing microscope. The location would be measured relative to known star locations.
These first three steps do not constitute asteroid discovery: the observer has only found an apparition, which gets a provisional designation, made up of the year of discovery, a code of two letters representing the week of discovery, and of a number so more than the one discovered one took place in this week (e.g., 1998 FJ74).
The final step of discovery is to send the locations and time of observations to Brian Marsden of the Minor Planet Center. Dr. Marsden has computer programs that compute whether an apparition ties together previous apparitions into a single orbit. If so, the object gets a number. The observer of the first apparition with a calculated orbit is declared the discoverer, and he gets the honor of naming the asteroid (subject to the approval of the International Astronomical Union) once it is numbered.
Latest technology: Detecting hazardous asteroids
There is increasing interest in identifying asteroids whose orbits cross Earth's orbit, and that could, given enough time, collide with Earth (see Earth-crosser asteroids). The three most important groups of near-Earth asteroids are the Apollos, Amors, and the Atens. Various asteroid deflection strategies have been proposed.
The near-Earth asteroid 433 Eros had been discovered as long ago as 1898, and the 1930s brought a flurry of similar objects. In order of discovery, these were: 1221 Amor, 1862 Apollo, 2101 Adonis, and finally 69230 Hermes, which approached within 0.005 AU of the Earth in 1937. Astronomers began to realize the possibilities of Earth impact.
Two events in later decades increased the level of alarm: the increasing acceptance of Walter Alvarez' theory of dinosaur extinction being due to an impact event, and the 1994 observation of Comet Shoemaker-Levy 9 crashing into Jupiter. The U.S. military also declassified the information that its military satellites, built to detect nuclear explosions, had detected hundreds of upper-atmosphere impacts by objects ranging from one to ten meters across.
All of these considerations helped spur the launch of highly efficient automated systems that consist of Charge-Coupled Device (CCD) cameras and computers directly connected to telescopes. Since 1998, a large majority of the asteroids have been discovered by such automated systems. A list of teams using such automated systems includes:
- The Lincoln Near-Earth Asteroid Research (LINEAR) team
- The Near-Earth Asteroid Tracking (NEAT) team
- The Lowell Observatory Near-Earth-Object Search (LONEOS) team
- The Catalina Sky Survey (CSS)
- The Campo Imperatore Near-Earth Objects Survey (CINEOS) team
- The Japanese Spaceguard Association
- The Asiago-DLR Asteroid Survey (ADAS)
The LINEAR system alone has discovered 62,283 asteroids as of December 14, 2005. Between all of the automated systems, 3,868 near-Earth asteroids have been discovered including over six hundred more than one kilometer in diameter.
The naming format
Newly discovered asteroids are given a provisional designation consisting of the year of discovery and an alphanumeric code, such as 2001 FH. When its orbit is confirmed, it is given a number, and later may also be given a name (e.g., 1 Ceres). The formal naming convention uses parentheses around the number (e.g., (433) Eros), however, dropping the parentheses is quite common. Informally, especially when a name is repeated in running text, it is common to drop the number altogether, or to drop it after the first mention.
The Minor Planet Circular (MPC) of October 19, 2005, was a historical one, as it saw the highest numbered asteroid jump from 99947 to 118161, causing a small "Y2K"-like crisis for various automated data services—up until then, only five digits were allowed in most data formats for the asteroid number. This has been addressed in some data fields by having the leftmost digit, the ten-thousands place, use the alphabet as a digit extension. A=10, B=11,…, Z=35, a=36,…, z=61. The highest number 120437 thus is cross-referenced as C0437 on some lists. Also, the fictional asteroid of The Little Prince, B612, now could be connected with the real (110612) 2001 TA142 which is listed as (B0612) 2001 TA142 in the compacted lists —although it is already present as 46610 Bésixdouze (B612 in hexadecimal translates to 46610 in decimal notation).
Unnamed asteroids that have been given a number keep their provisional designation, such as (29075) 1950 DA.
As modern discovery techniques have discovered vast numbers of new asteroids, they are increasingly being left unnamed. The first asteroid to be left unnamed was (3360) 1981 VA. On rare occasions, an asteroid's provisional designation may become used as a name in itself: the still unnamed (15760) 1992 QB₁ gave its name to a group of asteroids which became known as cubewanos.
Sources for names
The first few asteroids were named after figures from Greco-Roman mythology, but as such names started to run out, others were used—famous people, literary characters, the names of the discoverer's wives, children, and even television characters.
The first asteroid to be given a non-mythological name was 20 Massalia, named after the city of Marseilles. For some time only female (or feminized) names were used; Alexander von Humboldt was the first man to have an asteroid named after him, but his name was feminized to 54 Alexandra. This unspoken tradition lasted until 334 Chicago was named; even then, oddly feminized names show up in the list for years afterward.
As the number of asteroids began to run into the hundreds, and eventually the thousands, discoverers began to give them increasingly frivolous names. The first hints of this were 482 Petrina and 483 Seppina, named after the discoverer's pet dogs. However, there was little controversy about this until 1971, upon the naming of 2309 Mr. Spock (which was not even named after the Star Trek character, but after the discoverer's cat who supposedly bore a resemblance to him). Although the IAU subsequently banned pet names as sources, eccentric asteroid names are still being proposed and accepted, such as 6042 Cheshirecat, 9007 James Bond, or 26858 Misterrogers.
Special naming rules
Asteroid naming is not always a free-for-all: there are some types of asteroid for which rules have developed about the sources of names. For instance, Centaurs (asteroids orbiting between Saturn and Neptune) are all named after mythological centaurs; Trojans, after heroes from the Trojan War; and trans-Neptunian objects, after underworld spirits.
The first few asteroids discovered were assigned symbols like the ones traditionally used to designate Earth, the Moon, the Sun and planets. The symbols quickly became ungainly, hard to draw and recognise. By the end of 1851 there were 15 known asteroids, each (except one) with its own symbol. The first four's main variants are shown here:
Johann Franz Encke made a major change in the Berliner Astronomisches Jahrbuch (BAJ, "Berlin Astronomical Yearbook") for 1854. He introduced encircled numbers instead of symbols, although his numbering began with Astraea, the first four asteroids continuing to be denoted by their traditional symbols. This symbolic innovation was adopted very quickly by the astronomical community. The following year (1855), Astraea's number was bumped up to 5, but Ceres through Vesta would be listed by their numbers only in the 1867 edition. A few more asteroids (28 Bellona, 35 Leukothea, and 37 Fides) would be given symbols as well as using the numbering scheme.
The circle would become a pair of parentheses, and the parentheses sometimes omitted altogether over the next few decades.
Until the age of space travel, asteroids were merely pinpricks of light in even the largest telescopes and their shapes and terrain remained a mystery.
The first close-up photographs of asteroid-like objects were taken in 1971 when the Mariner 9 probe imaged Phobos and Deimos, the two small moons of Mars, which are probably captured asteroids. These images revealed the irregular, potato-like shapes of most asteroids, as did subsequent images from the Voyager probes of the small moons of the gas giants.
The first true asteroid to be photographed in close-up was 951 Gaspra in 1991, followed in 1993 by 243 Ida and its moon Dactyl, all of which were imaged by the Galileo probe en route to Jupiter.
The first dedicated asteroid probe was NEAR Shoemaker, which photographed 253 Mathilde in 1997, before entering into orbit around 433 Eros, finally landing on its surface in 2001.
Other asteroids briefly visited by spacecraft en route to other destinations include 9969 Braille (by Deep Space 1 in 1999), and 5535 Annefrank (by Stardust in 2002).
In September 2005, the Japanese Hayabusa probe started studying 25143 Itokawa in detail and will return samples of its surface to earth in 2010. Following that, the next asteroid encounters will involve the European Rosetta probe (launched in 2004), which will study 2867 Šteins and 21 Lutetia in 2008 and 2010.
NASA is planning to launch the Dawn Mission in 2007, which will orbit both 1 Ceres and 4 Vesta in 2011-2015.
It has been suggested that asteroids might be used in the future as a source of materials that may be rare or exhausted on earth (asteroid mining).
- Near-Earth object
- Minor planet
- Asteroid belt
- Known Asteroid Impacts & Their Effects
- Alphabetical list of minor planet names
- Alphabetical and numerical lists of minor planet names
- Near Earth Objects Dynamic Site
- Asteroids Dynamic Site
- Asteroid naming statistics
- Near Earth Asteroid Tracking (NEAT)
- Everything you wanted to know about comets and asteroids
- Spaceguard UK
- When Did the Asteroids Become Minor Planets?
- Large amount of information on asteroid groups collected by Gérard Faure
- Asteroid Simulator with Moon and Earth
- NASA Planetary Data System Small Bodies Node
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