
Mineral
Lepidolite
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2)
Hardness: 2.5–3.5 on Mohs scale; Color: Pink, purplish-pink, lilac, or violet-grey; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (micaceous sheets); Specific gravity: 2.8–2.9.
- Hardness
- 2
- Color
- Pink, purplish-pink, lilac, or violet-grey
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5–3.5 on Mohs scale; Color: Pink, purplish-pink, lilac, or violet-grey; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (micaceous sheets); Specific gravity: 2.8–2.9.
Formation & geological history
Formed primarily in lithium-bearing granitic pegmatites. It is an igneous secondary mineral that often occurs with other lithium minerals like spodumene or tourmaline. It can represent late-stage crystallization in magma chambers.
Uses & applications
Major ore of lithium used in batteries and electronics; used in high-temp glass and ceramics; widely carved into spheres, towers, and jewelry for the metaphysical/collector market.
Geological facts
Lepidolite is the most common lithium-bearing mineral. It was first called 'lilalite' (from the Hindu word for lilac) before being renamed from the Greek word 'lepidos' for scale, referring to its scaly, micaceous appearance.
Field identification & locations
Identify by its distinctive lilac/purple color and pearly luster. In the field, look for 'books' of mica-like sheets or granular masses. Common locations include Brazil, Madagascar, Canada (Manitoba), and the USA (Maine, California).
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