
mineral
Ruby (Raw/Rough)
Corundum (Al2O3 with Chromium trace)
Hardness: 9 on Mohs scale; Color: Pinkish-red to deep violet-red; Luster: Adamantine to vitreous; Crystal structure: Trigonal/Hexagonal; Cleavage: None (parting sometimes present); Specific gravity: 3.97–4.05
- Hardness
- 9 on Mohs scale
- Color
- Pinkish-red to deep violet-red
- Luster
- Adamantine to vitreous
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Physical properties
Hardness: 9 on Mohs scale; Color: Pinkish-red to deep violet-red; Luster: Adamantine to vitreous; Crystal structure: Trigonal/Hexagonal; Cleavage: None (parting sometimes present); Specific gravity: 3.97–4.05
Formation & geological history
Formed through contact metamorphism or in igneous rocks like basalt. Found in marble-hosted environments or gravel-rich alluvial deposits. Rubies range in age from hundreds of millions to billions of years old depending on the source deposit.
Uses & applications
Primarily used in high-end jewelry and as a gemstone for collectors. Industrial grade corundum is used for abrasives, lasers, and watch bearings.
Geological facts
The red color is caused specifically by the presence of chromium. Without chromium, the mineral is simply called sapphire. It is the second hardest natural substance on Earth after diamond.
Field identification & locations
Identify in the field by its extreme hardness (scratching anything but diamond), its dense weight, and its fluorescent glow under UV light. Commonly found in Myanmar, Sri Lanka, Thailand, and Mozambique.
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