
mineral
Moonstone
Orthoclase (Potassium aluminum silicate - KAlSi3O8)
AI-generated identification · may be incorrectHardness: 6-6.5 (Mohs scale); Color: White, cream, or blue-ish with a pearly or opalescent sheen (adularescence); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
- Hardness
- 6-6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 (Mohs scale); Color: White, cream, or blue-ish with a pearly or opalescent sheen (adularescence); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
Formation & geological history
Formed through the cooling and slow separation of two different types of feldspar (orthoclase and albite) within igneous rocks like pegmatites. This internal layering causes light to scatter, creating the stone's characteristic glow.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons, rings, earrings) and as a popular specimen for crystal healing and mineral collectors.
Geological facts
Ancient Romans believed moonstones were formed from frozen moonbeams. It is the Florida State Gemstone (commemorating the Apollo moon landings) despite not being naturally occurring in the state.
Field identification & locations
Identify by its 'adularescence' (a glowing interior shine when tilted). It is commonly found in Sri Lanka, India, Myanmar, and Madagascar. In the field, look for a perthitic texture and the characteristic pearly sheen on cleavage planes.
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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