Rock Identifier
Lepidolite on Quartz (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2 (Lepidolite) / SiO2 (Quartz)) — mineral
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
Identified More mineral
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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.