
mineral
Pink 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, lilac, or purple; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal.
- Hardness
- 2
- Color
- Pink, lilac, or purple
- Luster
- Pearly to vitreous
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Physical properties
Hardness: 2.5-3.5 on Mohs scale; Color: Pink, lilac, or purple; Luster: Pearly to vitreous; Crystal Structure: Monoclinic; Cleavage: Perfect basal.
Formation & geological history
Forms in granitic pegmatites, often associated with other lithium-bearing minerals like tourmaline and spodumene through igneous crystallization.
Uses & applications
A major source of lithium used in batteries and glass making; also used for decorative carvings, palm stones, and jewelry.
Geological facts
Lepidolite is known as the 'Stone of Transition' in metaphysical circles and was originally discovered in the 18th century. It is the most common lithium-bearing mineral.
Field identification & locations
Identify by its characteristic micaceous structure (scaling/flaking), soft hardness, and distinctive lilac to pink hue. Often found in Minas Gerais, Brazil and California, USA.
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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