
mineral
Moonstone
Orthoclase (KAlSi3O8) or Albite (NaAlSi3O8)
Hardness: 6-6.5 on Mohs scale; Color: Milky white to translucent with a blue or white internal sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
- Hardness
- 6-6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Milky white to translucent with a blue or white internal sheen; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in two directions; Specific gravity: 2.56-2.59
Formation & geological history
Formed in plutonic igneous rocks (pegmatites) through the cooling of magma. As it cools, the intergrowth of orthoclase and albite separates into stacked layers, creating its signature optical effect.
Uses & applications
Primary use is in the jewelry industry as a semi-precious gemstone. It is also used by collectors and in metaphysical practices.
Geological facts
The visual phenomenon seen in moonstone is called 'adularescence,' caused by light scattering between microscopic layers of different feldspars. It is the Florida State Gemstone (commemorating the Moon landing) and is associated with June birthdays.
Field identification & locations
Identify by its characteristic billowy light effect (schiller) when rotated. Found commonly in Sri Lanka, India, Myanmar, and Madagascar. In the field, look for a pearly luster and a distinct 'stair-step' cleavage pattern characteristic of feldspars.
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