
mineral
Moonstone
Orthoclase (KAlSi3O8) with inclusions of Albite (NaAlSi3O8)
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: Colorless to white, tan, or gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Adularescence: Blue or white glow.
- Hardness
- 6-6
- Color
- Colorless to white, tan, or gray
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Colorless to white, tan, or gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Adularescence: Blue or white glow.
Formation & geological history
Formed from molten rock deep in the earth; as it cools, the intermixed minerals (orthoclase and albite) separate into alternating layers, causing light to scatter. Commonly found in pegmatites and alpine veins.
Uses & applications
Used primarily as a gemstone in jewelry, decorative ornaments, and by crystal collectors for its aesthetic and metaphysical associations.
Geological facts
Ancient Romans believed moonstone was formed from frozen rays of the moon. It is the state gem of Florida to commemorate the moon landing, even though it is not found there.
Field identification & locations
Identify by its unique schiller effect (adularescence) that moves as the stone is tilted. Look for thin, alternating mineral layers. Commonly found in Sri Lanka, India, and Myanmar.
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Epidote
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Granite (Phaneritic intrusive igneous rock)
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