
mineral
Aquamarine
Beryl (Be3Al2Si6O18 with iron impurities)
AI-generated identification · may be incorrectHardness: 7.5-8.0 (Mohs scale), Color: Pale blue to greenish-blue, Luster: Vitreous (glassy), Crystal Structure: Hexagonal, Cleavage: Imperfect/Indistinct, Specific Gravity: 2.66-2.80
- Hardness
- 7
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Physical properties
Hardness: 7.5-8.0 (Mohs scale), Color: Pale blue to greenish-blue, Luster: Vitreous (glassy), Crystal Structure: Hexagonal, Cleavage: Imperfect/Indistinct, Specific Gravity: 2.66-2.80
Formation & geological history
Formed in pegmatites and metamorphic rocks through hydrothermal processes involving beryllium-rich fluids during the cooling of granitic magma.
Uses & applications
Primarily used as a gemstone in high-end jewelry (rings, necklaces, earrings). It is also a minor source of beryllium for industrial alloys.
Geological facts
The name comes from the Latin 'aqua marina', meaning 'water of the sea'. It is the birthstone for March and was historically believed by sailors to protect them at sea.
Field identification & locations
Identify by its characteristic pale blue color, lack of inclusion (compared to emerald), and high hardness which resists scratching. Commonly found in Brazil, Pakistan, and Madagascar.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary