asteroidide

Asteroidide is a term used in speculative and theoretical discussions to describe a hypothetical class of small Solar System bodies that blend characteristics of asteroids and comets. The name combines asteroid with the suffix -ide, a convention sometimes used in mineral and chemical nomenclature. In current astronomical practice, asteroidide is not an officially recognized category, and there is no consensus on a formal definition or criteria.

In proposed conceptions, asteroidides are envisioned as objects that occupy regions from the main asteroid belt to the outer Solar System and exhibit a mix of rocky and volatile-rich properties. They are often described as having sizes ranging from tens of meters up to a few kilometers, with interiors that may contain ices or hydrated minerals. When subjected to solar heating, some asteroidides are imagined to show transient activity, such as brief outgassing or coma formation, blurring the line between typical asteroids and comets.

Dynamic and spectral characteristics in speculative discussions frequently include orbits that are more varied than those of conventional asteroids, including eccentricities and inclinations that allow occasional outgassing events. Their spectral signatures are described as intermediate between silicate-dominated asteroids and cometary surfaces, reflecting a mixed mineralogy.

Observational status remains uncertain, as no confirmed asteroidide has been identified in real surveys. Any candidate would require careful analysis to distinguish from activated asteroids, comets, or other known classes, and would likely lead to reclassification within established catalogs.

In literature and science fiction, asteroidides frequently serve as a device to explore the continuum between rocky asteroids and volatile-rich bodies, highlighting questions about formation, evolution, and the diversity of small bodies in the Solar System. See also: asteroid, comet, centaur, damocloid.