
mineral
Moonstone
Orthoclase (Potassium aluminum silicate - KAlSi3O8)
Hardness: 6.0-6.5 (Mohs), Color: Colorless to white with a blue or white adularescence (sheen), Luster: Vitreous to pearly, Crystal Structure: Monoclinic, Cleavage: Two directions at 90 degrees, Specific Gravity: 2.56-2.59
- Hardness
- 6
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Physical properties
Hardness: 6.0-6.5 (Mohs), Color: Colorless to white with a blue or white adularescence (sheen), Luster: Vitreous to pearly, Crystal Structure: Monoclinic, Cleavage: Two directions at 90 degrees, Specific Gravity: 2.56-2.59
Formation & geological history
Formed in igneous and metamorphic rocks. The characteristic 'glow' (adularescence) is caused by the intergrowth of two types of feldspar (orthoclase and albite) that separate as the mineral cools, causing light to scatter.
Uses & applications
Primarily used as a gemstone in jewelry (rings, pendants, earrings) and for crystal healing/collecting. High-quality specimens with strong blue sheen are highly sought after by lapidaries.
Geological facts
Ancient Romans believed moonstone was formed from frozen beams of moonlight. It is the Florida State Gemstone (commemorating the Moon landings) even though it is not naturally found there.
Field identification & locations
Identify by its distinctive 'billowy' light that moves across the surface as the stone is turned. It is commonly found in Sri Lanka, India, Madagascar, and Myanmar. In the field, look for feldspar-rich pegmatites.
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