
mineral
Moonstone
Orthoclase Feldspar (containing Albite lamellae), (KAlSi3O8)
Hardness: 6.0-6.5 on Mohs scale; Color: Colorless to white with a blue or white adularescent sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.56-2.59.
- Hardness
- 6
- Color
- Colorless to white with a blue or white adularescent sheen
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6.0-6.5 on Mohs scale; Color: Colorless to white with a blue or white adularescent sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.56-2.59.
Formation & geological history
Formed in igneous or metamorphic environments through the cooling of magma or the metamorphism of rocks. Its unique shimmer (adularescence) is caused by the alternating layers of orthoclase and albite that scatter light.
Uses & applications
Primarily used in jewelry (cabochons, rings, and pendants), as a birthstone for June, and highly valued by mineral collectors for its optical effects.
Geological facts
Ancient Romans believed moonstones were formed from frozen rays of moonlight. It is the state gem of Florida to commemorate the moon landing, despite not being found there naturally.
Field identification & locations
Identify in the field by its distinct 'shimmer' that appears to move across the surface as the stone is tilted. Found commonly in Sri Lanka, India, Madagascar, and Myanmar. Use a hardness test to distinguish it from plastic or glass imitations.
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