
mineral
Aquamarine
Beryl (Be3Al2Si6O18 with iron impurities)
Hardness: 7.5-8.0 on Mohs scale; Color: Pale blue to light green; Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: Imperfect/Poor; Specific gravity: 2.63 - 2.80
- Hardness
- 7
- Color
- Pale blue to light green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7.5-8.0 on Mohs scale; Color: Pale blue to light green; Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: Imperfect/Poor; Specific gravity: 2.63 - 2.80
Formation & geological history
Formed in granitic pegmatites or hydrothermal veins where beryllium is present. Most specimens date from several hundred million years old, crystallizing from cooling magma-enriched fluids.
Uses & applications
Primarily used as a gemstone in jewelry (rings, necklaces, earrings). It is also a minor source of beryllium for industrial alloys, though most beryl of this quality is reserved for collectors or lapidary use.
Geological facts
Aquamarine is the birthstone for March. Its name is derived from the Latin 'aqua marina', meaning 'sea water'. Unlike emeralds, aquamarines often grow in very large, clean crystals.
Field identification & locations
Identify in the field by its hexagonal crystal habit (if present), its hardness (will scratch glass), and its distinctive watery-blue hue. Commonly found in Brazil, Pakistan, and Madagascar. Collectors look for high clarity and deep 'Santa Maria' blue saturation.
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