
mineral
Moonstone
Orthoclase Feldspar (KAlSi3O8)
AI-generated identification · may be incorrectHardness: 6.0-6.5 on Mohs scale; Color: Colorless to white, gray, or peach with blue/white adularescence; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
- Hardness
- 6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6.0-6.5 on Mohs scale; Color: Colorless to white, gray, or peach with blue/white adularescence; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
Formation & geological history
Formed in igneous and metamorphic rocks from cooling magma or hydrothermal activity. Its unique glow comes from the intergrowth of two types of feldspar (orthoclase and albite) that separate into thin, alternating layers as the mineral cools.
Uses & applications
Primary use is in jewelry as gemstones (cabs or faceted). Also a popular mineral for metaphysical collecting and historically used as an amulet.
Geological facts
Ancient Romans believed moonstone was formed from frozen drops of moonlight. It is the Florida State Gemstone (honoring the Apollo moon landings) and is known for 'adularescence'—an optical phenomenon that causes a shimmering light to move across the stone.
Field identification & locations
Identify by its distinctive milky blue or white sheen when rotated under light. Commonly found in Sri Lanka, India, Myanmar, Madagascar, and parts of the USA (like New Mexico). To test in the field, look for the 'schiller' effect and scratch resistance (it will scratch glass but be scratched by quartz).
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