
mineral
Beryl (Variety: Aquamarine/Green Beryl)
Beryllium Aluminum Silicate (Be3Al2Si6O18)
AI-generated identification · may be incorrectHardness: 7.5–8 on Mohs scale; Color: Pale blue to sea-green (due to trace iron); Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: Imperfect; Specific gravity: 2.63–2.90.
- Hardness
- 7
- Color
- Pale blue to sea-green (due to trace iron)
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7.5–8 on Mohs scale; Color: Pale blue to sea-green (due to trace iron); Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: Imperfect; Specific gravity: 2.63–2.90.
Formation & geological history
Usually found in granitic pegmatites or hydrothermal veins. Formed during the late stages of magmatic crystallization when beryllium is concentrated. Common in Precambrian and Paleozoic terrains.
Uses & applications
Primary source of beryllium for alloys in aerospace and telecommunications; significant use as a gemstone in high-end jewelry; prized by mineral collectors in its raw form.
Geological facts
The name comes from Latin 'aqua marina' (water of the sea). Ancient sailors believed it could calm waves and protect them at sea. It is the official birthstone for March.
Field identification & locations
Identify in the field by its distinct hexagonal crystal habit, lack of reaction to acid, and hardness. Common locations include Brazil, Pakistan, Madagascar, and the Ural Mountains in Russia.
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