
mineral
Lepidolite
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2)
Hardness: 2.5–3 on the Mohs scale; Color: Pink, purplish-gray, or lavender; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (micaceous sheets/flakes); Specific gravity: 2.8–2.9.
- Hardness
- 2
- Color
- Pink, purplish-gray, or lavender
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5–3 on the Mohs scale; Color: Pink, purplish-gray, or lavender; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (micaceous sheets/flakes); Specific gravity: 2.8–2.9.
Formation & geological history
Formed in late-stage crystallization of lithium-bearing granite pegmatites. It is often found associated with other lithium minerals like tourmaline and spodumene. Geological age varies by deposit location, ranging from Precambrian to Cenozoic.
Uses & applications
Primary source of lithium for glass making and metallurgy; also used in the production of ornamental carvings, bead jewelry, and as a metaphysical collector's stone.
Geological facts
Lepidolite is the most common lithium-bearing mineral. It was first described in the late 18th century and was originally named 'lilalite' before being renamed to lepidolite, after the Greek word 'lepidos' for scale, referring to its scaly appearance.
Field identification & locations
Identify in the field by its distinct lilac-purple color, low hardness (can be scratched by a copper coin), and its tendency to flake off in glittery scales or clusters. Common locations include Brazil, Russia (Ural Mountains), Madagascar, and the United States (California/Maine).
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