
mineral
Alexandrite
Chrysoberyl (BeAl2O4)
AI-generated identification · may be incorrectHardness: 8.5 Mohs scale; Color: Green/Blue-green in daylight, Red/Purplish-red in incandescent light (pleochroism); Luster: Vitreous; Crystal Structure: Orthorhombic; Cleavage: Distinct in one direction.
- Hardness
- 8
- Luster
- Vitreous
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Physical properties
Hardness: 8.5 Mohs scale; Color: Green/Blue-green in daylight, Red/Purplish-red in incandescent light (pleochroism); Luster: Vitreous; Crystal Structure: Orthorhombic; Cleavage: Distinct in one direction.
Formation & geological history
Formed in granitic pegmatites and mica schists where beryllium is present and silica is deficient, allowing chromium to substitute for aluminum. Most specimens are from the Phanerozoic eon.
Uses & applications
Primarily used as a rare and precious gemstone in high-end jewelry and as a prized specimen for mineral collectors.
Geological facts
First discovered in the Ural Mountains of Russia in 1830 and named after Tsar Alexander II. It is often described as 'emerald by day, ruby by night.'
Field identification & locations
Identified by its extreme hardness and dramatic color-change effect (Alexandrite effect). Found in Russia, Brazil, Sri Lanka, and East Africa. Use a penlight and daylight to check for color shifts.
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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