
igneous/mineral
Lepidolite in Quartz (Lithium-bearing Ore)
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2) and Quartz (SiO2)
Hardness: 2.5-3 (Lepidolite) to 7 (Quartz); Color: Lilac, lavender, or pink inclusions in a white or translucent matrix; Luster: Vitreous to pearly; Crystal structure: Monoclinic (Mica) and Hexagonal (Quartz); Specific gravity: ~2.8.
- Hardness
- 2
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5-3 (Lepidolite) to 7 (Quartz); Color: Lilac, lavender, or pink inclusions in a white or translucent matrix; Luster: Vitreous to pearly; Crystal structure: Monoclinic (Mica) and Hexagonal (Quartz); Specific gravity: ~2.8.
Formation & geological history
Formed in granitic pegmatites during the final stages of magma crystallization where lithium is concentrated. Often associated with other minerals like tourmaline and spodumene. Ages vary globally from Proterozoic to Cenozoic.
Uses & applications
Primary source of lithium used in rechargeable batteries, glass, and ceramics. Also used as a decorative stone in jewelry (cabochons) and for metaphysical/collecting purposes.
Geological facts
Lepidolite is known as the 'peace stone' in folklore and is a major source of the rare alkali metal Rubidium. It is one of the few minerals that frequently contains significant levels of lithium.
Field identification & locations
Identify by its distinct lilac-to-purple color and micaceous sheen within a harder host rock. Commonly found in Brazil, Madagascar, and the US (Maine/California). Field collectors should look for platy, shiny flakes that can be scratched with a penny.
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Other igneous/mineral specimens
Lepidolite
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2)
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Lepidolite
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2)
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Chlorite (Small Flakes/Sand)
Chlorite Group (Magnesium Iron Aluminum Silicate Hydroxide - (Mg,Fe)3(Si,Al)4O10(OH)2·(Mg,Fe)3(OH)6)
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Garnet (Pyrope or Almandine)
Silicate (X3Y2Si3O12)
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Lepidolite
Lepidolite [K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2]
Mineral
Peridot (Olivine)
Magnesium Iron Silicate (Mg, Fe)2SiO4
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