
mineral
Ruby (Corundum)
Aluminum Oxide (Al2O3) with Chromium traces
AI-generated identification · may be incorrectHardness: 9.0 (Mohs scale), Color: Vivid red to pinkish-red, Luster: Vitreous to sub-adamantine, Crystal structure: Trigonal/Hexagonal, Cleavage: None (has parting), Specific Gravity: 3.97-4.05
- Hardness
- 9
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Physical properties
Hardness: 9.0 (Mohs scale), Color: Vivid red to pinkish-red, Luster: Vitreous to sub-adamantine, Crystal structure: Trigonal/Hexagonal, Cleavage: None (has parting), Specific Gravity: 3.97-4.05
Formation & geological history
Formed in metamorphic rocks (marble or schist) or igneous rocks (basalt) where aluminum-rich fluids crystallized under high heat and pressure, often millions of years ago.
Uses & applications
Primarily used in high-end jewelry (one of the four precious stones), watchmaking (pivot bearings), and industrial lasers.
Geological facts
Ruby is the red variety of the mineral corundum; sapphire is any other color of corundum. The most valuable rubies exhibit a 'pigeon blood' red color and a natural fluorescence.
Field identification & locations
Identify in the field by its extreme hardness (scratches almost anything except diamond) and hexagonal crystal habit. Common locations include Myanmar (Burma), Mozambique, Thailand, and Sri Lanka.
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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