
mineral
Moonstone (Orthoclase Feldspar)
Orthoclase (KAlSi3O8) with Albite (NaAlSi3O8)
Hardness: 6-6.5 (Mohs scale), Color: Creamy white to pale tan, Luster: Vitreous to pearly, Crystal structure: Monoclinic, Cleavage: Two directions at nearly 90 degrees, Specific gravity: 2.56-2.59
- Hardness
- 6-6
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Physical properties
Hardness: 6-6.5 (Mohs scale), Color: Creamy white to pale tan, Luster: Vitreous to pearly, Crystal structure: Monoclinic, Cleavage: Two directions at nearly 90 degrees, Specific gravity: 2.56-2.59
Formation & geological history
Formed in igneous and metamorphic environments, specifically pegmatites and granites. The characteristic 'glow' or adularescence occurs as the cooling mineral separates into alternating layers of orthoclase and albite, which scatter light.
Uses & applications
Primarily used as a gemstone in jewelry (rings, pendants, earrings) and as a stone for metaphysical collecting and spiritual practices.
Geological facts
Ancient Romans believed moonstone was formed from frozen rays of the moon. It is the Florida State Gemstone (commemorating the Apollo moon landings) even though it is not naturally found there.
Field identification & locations
Identify by its 'schiller' effect or adularescence (a ghostly internal sheen). In the field, look for crystalline faces and its distinct right-angle cleavage. Common in Sri Lanka, India, Myanmar, and Madagascar.
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