Onyx is a form of chalcedony consisting of alternating light and dark parallel bands. The material typically shows a waxy to dull luster and a solid to slightly translucent appearance, with colors ranging from cream to black or deep brown in the darker bands. It often occurs as banded stalactitic or massive forms that can be polished to reveal crisp belt-like stripes. Brazilian material is among the most widely collected and admired, with classic banding patterns that form eye-catching scenes when cut as slabs or carved into cabochons.

Formula
SiO2
Rarity
Common
Stability
Stable
Collector interest
High Interest
Classification notes
Silicate mineral; Quartz group (SiO2)

Key characteristics

Crystal system
trigonal
Mohs hardness
6.5–7
Specific gravity
2.55–2.7
Luster
vitreous, waxy, dull
Transparency
translucent, opaque
Color
black, white, gray, brown, red, orange
Streak
white
Cleavage
none
Fracture
conchoidal, subconchoidal, uneven
Crystal habit
massive, granular
  • Gem mineral
  • Classic / historic

Where Onyx is found

Top localities

  1. Minas Gerais1 specimen

About Onyx

Collectors value onyx for its historical use in decorative carvings and its versatile aesthetic in display pieces. The striking contrast of bands makes each specimen unique, and care for onyx involves standard mineral handling plus gentle polishing to preserve the delicate banding. While onyx can occur in a range of environments, it is the banded chalcedony varieties that attract attention in cabinet displays and with craftspeople who favor bold, graphic patterns.