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How to identify Ruby

Corundum (Al₂O₃) var. Ruby

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To correctly identify Ruby (Corundum (Al₂O₃) var. Ruby), 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

    Ranges from pinkish-red to deep, vivid 'pigeon's blood' red. The color is due to chromium impurities.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to adamantine.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Typically smooth on crystal faces, conchoidal fracture surfaces.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Hexagonal prisms, tabular crystals, bipyramidal forms. Often found as irregular grains in alluvial deposits.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, but exhibits parting along basal planes and rhombohedral planes due to twinning.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Metamorphic rocks (marble, gneiss, schist), igneous rocks (basalt, syenite, pegmatites), and secondary alluvial deposits.

Key Facts

Hardness
9 (Mohs scale)
Specific Gravity
3.97 - 4.05 g/cm³
Crystal System
Trigonal
Color
Red (due to Cr³⁺ impurities)
Luster
Vitreous to adamantine
Transparency
Transparent to opaque
Fracture
Conchoidal to uneven
Cleavage
None (exhibits parting)
Composition
Aluminum oxide (Al₂O₃) with trace chromium

Physical characteristics

  • Crystal Habit: Hexagonal prisms, tabular, bipyramidal; also granular, massive, or in alluvial pebbles.
  • Cleavage Type: None, but exhibits parting along {0001} (basal) and {1011} (rhombohedral) planes due to lamellar twinning.
  • Fracture Type: Conchoidal to uneven.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to adamantine.

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