
mineral
Moonstone
Feldspar (Orthoclase with Albite), (K,Na)AlSi3O8
AI-generated identification · may be incorrectHardness: 6-6.5 Mohs scale; Color: Colorless to white with blue or white schiller (adularescence); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect at two planes; 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: Colorless to white with blue or white schiller (adularescence); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect at two planes; Specific gravity: 2.56-2.59
Formation & geological history
Formed in plutonic igneous rocks (pegmatites) through the intergrowth of orthoclase and albite. As the cooling magma solidifies, the two minerals separate into thin, alternating layers, which causes the scattering of light known as adularescence.
Uses & applications
Primarily used in jewelry (cabochons, beads, rings) and as a collector's gemstone. Historically used in talismans and decorative arts.
Geological facts
The unique glow is called adularescence, named after Mt. Adular in Switzerland, a famous source. It is the state gem of Florida in honor of the moon landings, despite not being found there.
Field identification & locations
Identify by its characteristic blue or white 'shimmer' that moves across the surface when tilted. Commonly found in Sri Lanka, India, Myanmar, and Madagascar. Collectors look for high transparency and strong blue flashes.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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