
mineral
Moonstone
Orthoclase Feldspar (composed of alternate layers of orthoclase and albite), (K,Na)AlSi3O8
Hardness: 6.0-6.5 on Mohs scale; Color: Colorless to white/bluish with a milky 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/bluish with a milky sheen
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6.0-6.5 on Mohs scale; Color: Colorless to white/bluish with a milky sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
Formation & geological history
Formed from molten rock (magma) that cools slowly. As it cools, the intergrowth of orthoclase and albite separate into stacked layers, which causes the light to scatter, creating the 'adularescence' effect. It is typically found in pegmatites and metamorphic rocks worldwide.
Uses & applications
Primarily used as a gemstone in jewelry (rings, pendants, earrings). It is also highly valued by mineral collectors for specimens showing strong blue or rainbow schiller.
Geological facts
The shimmering light effect is called adularescence, named after Mt. Adular in Switzerland, a famous source for the stone. It was once believed by the Romans to be formed from frozen beams of moonlight.
Field identification & locations
Identify in the field by its distinct pearly luster and floating blue or white light as the stone is turned (adularescence). It is commonly found in Sri Lanka, India, Myanmar, and Madagascar. For collectors, look for high transparency and a strong blue sheen.
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