Rock Identifier
Lepidolite in Quartz (or Lepidolite Ore) (Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2) in Quartz (SiO2)) — igneous
igneous

Lepidolite in Quartz (or Lepidolite Ore)

Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2) in Quartz (SiO2)

Hardness: 2.5-3 (Lepidolite) to 7 (Quartz); Color: Purple, lilac, pinkish-grey; Luster: Pearly to vitreous; Crystal Structure: Monoclinic (Mica); Cleavage: Perfect basal.

Hardness
2
Color
Purple, lilac, pinkish-grey
Luster
Pearly to vitreous
Identified More igneous

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Physical properties

Hardness: 2.5-3 (Lepidolite) to 7 (Quartz); Color: Purple, lilac, pinkish-grey; Luster: Pearly to vitreous; Crystal Structure: Monoclinic (Mica); Cleavage: Perfect basal.

Formation & geological history

Formed in granitic pegmatites during the final stages of magmatic crystallization. Higher concentrations of Lithium are required for its formation, often found in late-stage hydrothermal veins.

Uses & applications

Major source of lithium for batteries, glass making, and ceramics. Also used as a decorative stone, in lapidary work, and for metaphysical/collector purposes.

Geological facts

Lepidolite is the most common lithium-bearing mineral. It is often referred to as the 'peace stone' in New Age circles because it contains lithium, which is used medically to stabilize moods.

Field identification & locations

Identify by its distinctive lilac/purple color and micaceous 'glittery' flakes when broken. Commonly found in Brazil, Africa (Zimbabwe), and the USA (California and Maine).