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How to identify Onyx

Banded Chalcedony (SiO2)

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To correctly identify Onyx (Banded Chalcedony (SiO2)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.

Step-by-step identification

  1. 1

    Color

    Overall color and any zoning or banding

    Typically black and white, or brown and white bands. Can also be solid black (often commercially called 'black onyx' but scientifically solid black chalcedony). Other colors like red, green, or blue can occur due to impurities or artificial dyeing.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Waxy to vitreous (glassy) when polished; dull to waxy on unpolished surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth, microcrystalline, conchoidal fracture surfaces. Feels cool to the touch.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline, meaning individual crystals are too small to be seen without high magnification. Forms in botryoidal, mammillary, or stalactitic masses, often filling cavities.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in the cavities of volcanic rocks (e.g., amygdules in basalt, geodes), hydrothermal veins, and sometimes in sedimentary deposits where silica-rich waters have permeated and deposited chalcedony.

Key Facts

Hardness
6.5-7 on the Mohs scale
Specific Gravity
2.58-2.64 g/cm³
Crystal System
Trigonal (cryptocrystalline aggregates)
Color
Black, white, brown, red, green; often banded
Luster
Waxy to vitreous
Transparency
Translucent to opaque
Fracture
Conchoidal
Cleavage
None
Composition
Silicon dioxide (SiO2)

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregates, typically massive, botryoidal, mammillary, or stalactitic, filling cavities. Individual crystals are microscopic.
  • Cleavage Type: None
  • Fracture Type: Conchoidal, producing smooth, shell-like breaks.
  • Tenacity: Brittle
  • Luster Type: Waxy to vitreous

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