
mineral
Lepidolite
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2)
Hardness: 2.5-3.5 on Mohs scale; Color: Pink, lilac, rose-red to violet-gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal cleavage; Specific gravity: 2.8-2.9
- Hardness
- 2
- Color
- Pink, lilac, rose-red to violet-gray
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5-3.5 on Mohs scale; Color: Pink, lilac, rose-red to violet-gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal cleavage; Specific gravity: 2.8-2.9
Formation & geological history
Formed in granitic pegmatites containing lithium. It is often associated with other lithium minerals like spodumene and tourmaline. It occurs in late-stage crystallization of highly fractionated magma.
Uses & applications
Primary source of lithium used in batteries, glass, and ceramics. It is also used as a gemstone, for ornamental carvings, and by mineral collectors for its unique color.
Geological facts
Lepidolite was first discovered in the 18th century and is named after the Greek word 'lepidos', meaning scale, referring to its scaly or micaceous texture. It contains high amounts of the rare alkali metals rubidium and cesium.
Field identification & locations
Identify by its distinctive lilac/pink color and micaceous (flakey) habit. Commonly found in Brazil, Russia (Ural Mountains), USA (California, Maine), and Zimbabwe. Collectors should look for its pearly sheen and ease of scratching with a copper penny.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Biotite Schist
Biotite-rich Schist [K(Mg,Fe)3AlSi3O10(F,OH)2]
metamorphic