mineral
Morganite (Pink Beryl)
Beryllium aluminum silicate Be3Al2(SiO3)6
AI-generated identification · may be incorrectHardness: 7.5 - 8.0 on Mohs scale; Color: Pink, peach, or salmon; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: Indistinct; Specific Gravity: 2.71 - 2.90
- Hardness
- 7
- Color
- Pink, peach, or salmon
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7.5 - 8.0 on Mohs scale; Color: Pink, peach, or salmon; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: Indistinct; Specific Gravity: 2.71 - 2.90
Formation & geological history
Formed in granitic pegmatites through the crystallization of magma enriched with beryllium. Mostly found in deposits and pockets within metamorphic or igneous host rocks.
Uses & applications
Primarily used as a gemstone in high-end jewelry (rings, necklaces, earrings) and as a highly sought-after mineral specimen for collectors.
Geological facts
Morganite was named after the financier J.P. Morgan in 1910 by George F. Kunz. It is the rare pink-to-orange variety of beryl, making it a cousin to emerald and aquamarine.
Field identification & locations
Identify by its hexagonal crystal habit, lack of reaction to acid, and high hardness. Commonly found in Madagascar, Brazil, and Afghanistan. Collectors look for strong saturation and clarity.
