
mineral
Lepidolite
Lepidolite (K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2)
AI-generated identification · may be incorrectHardness: 2.5-3.5 on Mohs scale; Color: Pink, purplish, lavender-gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal cleavage; Specific gravity: 2.8-2.9
- Hardness
- 2
- Color
- Pink, purplish, lavender-gray
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5-3.5 on Mohs scale; Color: Pink, purplish, lavender-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 where lithium is present. It is often found associated with other lithium minerals like tourmaline and spodumene.
Uses & applications
Major source of lithium used in batteries and glass making; commonly used as a gemstone for beads and decorative carvings; popular 'calming' stone in metaphysical circles.
Geological facts
Lepidolite is one of the primary minerals containing rubidium. It was first described in the 18th century and is notable for its 'sparkly' appearance due to its mica-like structure.
Field identification & locations
Identify by its characteristic lavender color and mica-like layered structure that flakes easily. Found in lithium-rich pegmatites in Brazil, Canada, and Africa.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary