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— CH. 1 · INTRODUCTION —

Asteroid family

~5 min read · Ch. 1 of 7
7 sections
  • Asteroid families are populations of space rocks that share nearly identical orbital fingerprints, and they carry a secret: most of them are the wreckage of ancient collisions. Between roughly a third and a third and a half of all asteroids in the main belt belong to one of these families. That is a staggering proportion of the belt's population bound together by a shared violent past. The questions that follow are worth sitting with. How old are these families? What does their composition tell us about the bodies that created them? And what happens to a family as time slowly pulls it apart?

  • Kiyotsugu Hirayama, a Japanese astronomer who lived from 1874 to 1943, was the first person to look at asteroid orbits and see families where others saw only chaos. In 1918 he published his findings, identifying the Koronis, Eos, and Themis families as distinct groupings. He later added the Flora and Maria families to his list. In his honor, asteroid families are sometimes called Hirayama families, a term that applies especially to those five prominent groupings he himself found. His key insight was to analyze proper orbital elements rather than the ordinary osculating elements, which fluctuate on timescales of tens of thousands of years and can obscure the underlying relationships. Proper elements, by contrast, remain nearly constant for at least tens of millions of years, making real family membership visible across vast stretches of time.

  • In many or most cases, when two asteroids collided, the parent body was completely shattered. Some families, however, came from something less catastrophic: a large cratering event that gouged out material without destroying the parent body. The Vesta, Pallas, Hygiea, and Massalia families all formed this way. Cratering families have a recognizable signature: one large surviving body surrounded by a swarm of much smaller fragments. Composition tells the story plainly. Because all the fragments share the same origin, they match each other chemically. The Vesta family is a notable exception, because Vesta was a differentiated body, meaning it had separated into layers, and the collision exposed material from different depths with different compositions. Some families, like Flora, have a complex internal structure that researchers cannot fully explain yet, possibly because several separate collisions occurred in the same region at different times.

  • Asteroid families are not permanent. Their estimated lifetimes run on the order of a billion years, which is significantly shorter than the age of the Solar System, so few if any families alive today are true relics of the earliest era. Two processes erode them. Jupiter and other large bodies slowly perturb the orbits of family members, spreading them apart over time. Collisions between asteroids grind members down into smaller and smaller pieces. Once a fragment becomes small enough, a subtle force called the Yarkovsky effect takes hold: radiation pressure from sunlight nudges tiny rocks toward orbital resonances with Jupiter, and once there, they are ejected from the belt relatively quickly. Age estimates for individual families range from hundreds of millions of years down to less than several million years, as is the case for the compact Karin family. Old families betray their age by having few small members left, because those smaller bodies have been lost fastest.

  • Some families have grown so old that virtually all their members have dispersed, leaving only a handful of the original large fragments. A suggested example is the 9 Metis and 113 Amalthea pair, two asteroids that may be the last survivors of a family that has otherwise vanished. Iron meteorites found on Earth offer a different kind of evidence for how many families once existed. Chemical ratios in iron meteorites point to at least 50 to 100 parent bodies large enough to have been differentiated, bodies that were subsequently shattered to expose their metallic cores and produce the meteorites we now collect. That is a count of lost families written in the rocks themselves.

  • Modern computer searches have identified more than a hundred asteroid families using two main techniques. The hierarchical clustering method looks for groupings where members are nearest neighbors in orbital element space. Wavelet analysis maps the density of asteroids across orbital space and hunts for peaks. A 2015 study identified 122 notable families containing roughly 100,000 member asteroids, drawn from a catalog of nearly 400,000 numbered minor planets. The data from that study is available at the Small Bodies Data Ferret website. Family boundaries are inherently fuzzy: at their edges, families blend gradually into the background asteroid population, which means member counts are always approximate. Even in the dense center of a family, a few interlopers from the background population sneak in. The asteroid 1 Ceres, the largest body in the belt, turns out to be one such interloper: it sits inside what was once called the Ceres family, now renamed the Gefion family, despite having no genetic connection to the other members.

  • Not every grouping deserves the title "family," and astronomers have developed a careful vocabulary to describe the range. The word cluster describes a small, tightly bound family like the Karin cluster. Clumps are groupings with few members that still stand clearly apart from the background, such as the Juno clump. Clans are more ambiguous: they merge gradually into the surrounding asteroid density and may have complex internal structures that make it hard to tell whether they are one large group or several overlapping unrelated ones. The Flora family has been called a clan for exactly this reason. Tribes are even less certain, either because they have too few members or because the orbital parameters carry large uncertainties. The most rigorously established groupings are called nominal families or clusters, and it is these that carry the most scientific weight. The Eos family, with over 16,000 members, and the Nysa family, with over 19,000, stand among the largest reliably identified groupings in the belt.

Common questions

What is an asteroid family and how does it form?

An asteroid family is a population of asteroids sharing similar proper orbital elements, including semi-major axis, eccentricity, and orbital inclination. Members are thought to be fragments produced by past collisions between larger asteroids, either from complete shattering of a parent body or from a large cratering event that ejected material without destroying the parent.

Who first identified asteroid families?

Japanese astronomer Kiyotsugu Hirayama (1874-1943) first identified several prominent asteroid families in 1918. He recognized the Koronis, Eos, and Themis families initially, then later added Flora and Maria. In his honor, asteroid families are sometimes called Hirayama families.

What percentage of main belt asteroids belong to asteroid families?

About 33% to 35% of asteroids in the main belt are family members. A 2015 study identified 122 notable families containing approximately 100,000 member asteroids from a catalog of nearly 400,000 numbered minor planets.

How long do asteroid families last?

Asteroid families are thought to have lifetimes on the order of a billion years, significantly shorter than the age of the Solar System. Age estimates for individual families range from hundreds of millions of years down to less than several million years, as in the case of the compact Karin family.

What is the difference between an asteroid family and an asteroid clan or clump?

A nominal asteroid family is a rigorously identified grouping with distinct boundaries in orbital element space. A clan, such as the Flora family, merges gradually into the background population and may consist of overlapping unrelated groups. A clump has relatively few members but is clearly distinct from the background, while tribes are groupings too statistically uncertain to be confidently classified.

What is the Yarkovsky effect and how does it affect asteroid families?

The Yarkovsky effect is a subtle force from sunlight that nudges small asteroids toward orbital resonances with Jupiter over time. Once small family members reach these resonances, they are relatively rapidly ejected from the asteroid belt, contributing to the gradual decay of asteroid families over millions to billions of years.

All sources

13 references cited across the entry

  1. 1journalA collisional family of icy objects in the Kuiper beltMichael E. Brown et al. — March 2007
  2. 3journalThe Hansa Family: A New High-Inclination Asteroid FamilyC. W. Hergenrother et al. — September 1996
  3. 4bookAsteroids IVD. Nesvorný et al. — December 2014
  4. 5journalAsteroid Family Identification Using the Hierarchical Clustering Method and WISE/NEOWISE Physical PropertiesJoseph R. Masiero et al. — June 2013
  5. 6journalAsteroid Dynamical FamiliesV. Zappalà et al. — 1997
  6. 7journalThe Trojan asteroid belt: Proper elements, stability, chaos and familiesMilani, Andrea — October 1993
  7. 8journalAsteroid families classification: Exploiting very large datasetsAndrea Milani et al. — September 2014
  8. 9journalAutomated Classification of Asteroids into Families at WorkZoran Knezevic et al. — July 2014
  9. 10journalTaxonomy of asteroid families among the Jupiter Trojans: comparison between spectroscopic data and the Sloan Digital Sky Survey colorsF. Roig et al. — June 2008
  10. 11journalA multidomain approach to asteroid families' identificationV. Carruba et al. — August 2013
  11. 12webHirayama familyDavid Darling
  12. 13journalGroups of asteroids probably of common originHirayama — October 1918