
mineral
Lepidolite on Quartz
K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2 (Lepidolite) / SiO2 (Quartz)
Hardness: 2.5-3.5 (Lepidolite) and 7 (Quartz). Color: Pale lilac, pink, or purple flakes on a white/clear matrix. Luster: Pearly to vitreous. Crystal structure: Monoclinic (sheets) and Trigonal. Cleavage: Perfect micaceous cleavage.
- Hardness
- 2
- Color
- Pale lilac, pink, or purple flakes on a white/clear matrix
- Luster
- Pearly to vitreous
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Physical properties
Hardness: 2.5-3.5 (Lepidolite) and 7 (Quartz). Color: Pale lilac, pink, or purple flakes on a white/clear matrix. Luster: Pearly to vitreous. Crystal structure: Monoclinic (sheets) and Trigonal. Cleavage: Perfect micaceous cleavage.
Formation & geological history
Formed in granitic pegmatites during the late stages of magmatic crystallization. It is a lithium-rich mica that occurs where rare elements are concentrated by hydrothermal fluids.
Uses & applications
A major source of lithium used in batteries, glass-making, and ceramics. Also popular for metaphysical collecting and occasionally used as an ornamental stone.
Geological facts
Lepidolite is one of the major source minerals for the rare alkali metals rubidium and caesium. It was originally named 'lilalite' because of its lavender color before being renamed from the Greek 'lepidos' for scale.
Field identification & locations
Identified by its lilac-to-pink color and micaceous, flaky 'books' of crystals that can be peeled with a fingernail. Commonly found in Brazil, Russia, California, and Zimbabwe.
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