
mineral
Moonstone
Orthoclase (Potassium Aluminum Silicate), Formula: (K,Na)AlSi3O8
Hardness: 6.0-6.5 on Mohs scale; Color: Colorless to white with a blue or white schiller; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect at two directions; Specific Gravity: 2.56-2.59
- Hardness
- 6
- Color
- Colorless to white with a blue or white schiller
- 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 schiller; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect at two directions; Specific Gravity: 2.56-2.59
Formation & geological history
Formed from molten rock (magma) that cools slowly, allowing two different types of feldspar to intergrow. As the rock cools, the minerals separate into alternating layers. It is primarily found in pegmatite veins and metamorphic rocks.
Uses & applications
Predominantly used as a gemstone in jewelry (rings, pendants, and earrings) and as a lapidary material for collectors.
Geological facts
The visual effect seen in moonstone is called adularescence, caused by light scattering between microscopic layers of orthoclase and albite. It has been used in jewelry for centuries, particularly by the Romans and during the Art Nouveau period.
Field identification & locations
Identify in the field by its distinct 'glow' or shimmer when rotated under light. Commonly found in Sri Lanka, India, Myanmar, and Madagascar. Collectors look for high transparency and a strong blue 'flash'.
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