
mineral
Lepidolite
K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2 (Lithium-bearing mica)
Hardness: 2.5–3 on Mohs scale; Color: Pink, lilac, or purple; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific Gravity: 2.8–2.9
- Hardness
- 2
- Color
- Pink, lilac, or purple
- Luster
- Pearly to vitreous
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Physical properties
Hardness: 2.5–3 on Mohs scale; Color: Pink, lilac, or purple; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific Gravity: 2.8–2.9
Formation & geological history
Formed in Lithium-bearing granitic pegmatites. It is associated with other lithium minerals like spodumene and tourmaline. Typically late-stage magmatic crystallization.
Uses & applications
Major ore of lithium used in batteries and glass production; also used as an ornamental stone in jewelry, carvings, and as a popular metaphysical/collector mineral.
Geological facts
Lepidolite is the most common lithium-bearing mineral. It often contains traces of rubidium and cesium, making it scientifically useful for radiometric dating of rocks.
Field identification & locations
Identify in the field by its distinctive lilac color, micaceous 'scaly' appearance, and low hardness (can be scratched by a fingernail). Found in Brazil, Canada, Madagascar, and the USA (California/Maine).
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