How to identify Ruby
Corundum (Al₂O₃) variety Ruby
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Open the appTo correctly identify Ruby (Corundum (Al₂O₃) variety 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
Color
Overall color and any zoning or banding
Ranges from pinkish-red to deep, vivid 'pigeon's blood' red. The color is typically unevenly distributed, often concentrated in patches or streaks.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to adamantine.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically smooth to the touch, with a dense, compact feel.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Hexagonal system, commonly found as tabular, prismatic, or bipyramidal crystals. Often twinned.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
No true cleavage, but exhibits parting along basal planes and rhombohedral planes due to lamellar twinning.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in metamorphic rocks (marbles, gneisses, schists), igneous rocks (basalts, syenites), and secondary alluvial deposits derived from these primary sources.
Key Facts
- Hardness
- 9 on the Mohs scale
- Specific Gravity
- 3.97 - 4.05
- Crystal System
- Hexagonal (trigonal)
- Color
- Red (due to chromium impurities)
- Luster
- Vitreous to adamantine
- Transparency
- Transparent to opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- None (exhibits parting)
- Composition
- Aluminum oxide (Al₂O₃) with trace chromium (Cr)
Physical characteristics
- Crystal Habit: Typically prismatic, tabular, or bipyramidal crystals; also granular, massive, or in lamellar aggregates. Often twinned.
- Cleavage Type: No true cleavage; exhibits parting along basal planes {0001} and rhombohedral planes {1011} due to lamellar twinning.
- Fracture Type: Conchoidal to uneven, brittle.
- Tenacity: Brittle
- Luster Type: Vitreous to adamantine
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