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C-type asteroids are carbonaceous asteroids. They are the most common variety forming around 75% of known asteroids, and an even higher percentage in the outer part of the belt beyond 2.7 AU, which is dominated by this asteroid type.

Contents 1 Characteristics 2 C-group asteroids 2.1 C-group (Tholen) 2.2 C-group (SMASS) 3 References

This type of asteroid has very similar spectra to carbonaceous chondrite meteorites (types CI and CM), whose chemical composition is approximately the same as the Sun and the primitive solar nebula, except that they do not contain hydrogen, helium and other volatiles. Hydrated (water-containing) minerals are present.

C-type asteroids are extremely dark with albedos typically in the 0.03 to 0.10 range. Their spectra contain moderately strong ultraviolet absorption at wavelengths below about 0.4 μm to 0.5 μm, while at longer wavelengths they are largely featureless but slightly reddish. The so-called "water" absorption feature around 3 μm, which can be an indication of water content in minerals is also present.

The largest unequivocally C-type asteroid is 10 Hygiea, although the SMASS classification places the largest asteroid 1 Ceres, here as well, because that scheme lacks a G-type.

See also asteroid spectral types.

In the Tholen classification, the C-type is grouped along with three less numerous types into a wider C-group of carbonaceous asteroids which contains:

• B-type
• C-type
• F-type
• G-type

In the SMASS classification, the wider C-group contains the types

• B-type corresponding to the Tholen B and F-types
• a core C-type for asteroids having the most "typical" spectra in the group
• Cg and Cgh types corresponding to the Tholen G-type
• Ch type with an absorption feature around 0.7μm
• Cb type corresponding to transition objects between the SMASS C and B types.

• S. J. Bus and R. P. Binzel Phase II of the Small Main-belt Asteroid Spectroscopy Survey: A feature-based taxonomy, Icarus, Vol. 158, pp. 146 (2002).