
mineral
Aquamarine
Beryl (Be3Al2Si6O18)
AI-generated identification · may be incorrectHardness: 7.5-8.0 on Mohs scale; Color: Pale blue to light green; Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: Indistinct; Specific Gravity: 2.66-2.80.
- 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: Indistinct; Specific Gravity: 2.66-2.80.
Formation & geological history
Formed primarily in pegmatites through hydrothermal processes where beryllium-rich fluids cool and crystallize over millions of years, often in the late stages of magmatic evolution.
Uses & applications
Primarily used as a gemstone in high-end jewelry and for mineral specimen collecting due to its clarity and calming color.
Geological facts
The largest gem-quality aquamarine ever found was the Dom Pedro, which weighed approximately 110 kilograms in its rough state. It is the birthstone for March and is named from the Latin 'aqua marina' meaning sea water.
Field identification & locations
Identify by its characteristic pale blue-to-teal color, high hardness (will scratch glass), and hexagonal crystal habit. Found commonly in Brazil, Pakistan, and Madagascar. Look for it in coarse-grained granite regions.
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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