
mineral
Aquamarine
Beryl (Be3Al2Si6O18 with iron impurities)
AI-generated identification · may be incorrectHardness: 7.5-8 on the Mohs scale. Color: Pale blue to light green. Luster: Vitreous (glass-like). Crystal structure: Hexagonal. Cleavage: Indistinct. Specific gravity: 2.67-2.74.
- Hardness
- 7
- Color
- Pale blue to light green
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7.5-8 on the Mohs scale. Color: Pale blue to light green. Luster: Vitreous (glass-like). Crystal structure: Hexagonal. Cleavage: Indistinct. Specific gravity: 2.67-2.74.
Formation & geological history
Formed in pegmatites, which are igneous rocks that result from the cooling of magma. Also found in metamorphic rocks like schist. Dating varies by location but often associated with Mesozoic to Cenozoic geological events.
Uses & applications
Primarily used as a gemstone in jewelry (rings, earrings, necklaces). In industry, beryl is a source of beryllium, used in aerospace and electronics.
Geological facts
Aquamarine is the birthstone for March. Its name is derived from the Latin 'aqua marina', meaning 'water of the sea'. The largest gem-quality crystal ever found weighed 243 pounds.
Field identification & locations
Identify by its distinct hexagonal crystal shape (in raw form) and its pale blue color. Commonly found in Brazil, Pakistan, and Madagascar. Collectors look for clarity and intensity of blue color.
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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