Lepidolite

Crystal system · Monoclinic

Lepidolite is a silicate mineral prized by collectors for its exceptional color range.

About Lepidoliteextended article

Crystal Structure
Li-mica.
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen40.99%
Si Silicon28.78%
K Potassium10.02%
F Fluorine9.74%
Al Aluminum6.91%
Li Lithium3.56%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Lpd
→ Lepidolite
Li-mica
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/lɪˈpɪdəlaɪt/
lih-PID-uh-lite
Greek lepis (scale)
Tenacity
Behavior:
elastic
Under stress:
Springs back
Same.
Luster
pearly
Lavender-pink sheets.
Diaphaneity (Transparency)
translucent
Pinkish-violet lithium mica.
Type Locality
Rožná — Czech Republic
Described 1792 by Klaproth
Magnetism
Category:
diamagnetic
Test result:
Slight repulsion possible
Li-rich mica — diamagnetic baseline.
Test with rare-earth magnet (N42 or N52 neodymium). Suspend specimen on thread for sensitive paramagnetic detection. Diamagnetic minerals are weakly repelled (visible only with strong magnets like bismuth).
Specific Gravity
2.80–2.90
g/cm³
light
Li-rich mica.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Geological Setting
Environment:
pegmatite
Host rock:
lithium-rich pegmatite
Companions:
Tourmaline · Spodumene · Feldspar · Beryl
Diagnostic mineral of lithium-rich pegmatite environments.
Cleavage & Fracture
Cleavage:
perfect 1 direction {001} — basal
Fracture:
uneven
Pinkish-lavender sheets.
Collector tier: Solid Display
Reliable mid-tier display species. Easy to find in well-formed examples; broad locality diversity.
Often found withTourmaline · Spodumene · Quartz · Cleavelandite
Mohs 2.5–4
Vickers (~) 170 HV
Knoop (~) 185 HK
Geological setting
Pegmatite
Element composition by mass

Formula: K(Li,Al)₃(Si,Al)₄O₁₀(F,OH)₂ · molar mass: 396.11 g/mol

O 44.43%
Al 23.84%
Si 14.18%
K 9.87%
F 4.8%
Li 2.63%
H 0.25%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

GroupMica Group
Related members: Muscovite · Biotite · Phlogopite
Mohs Hardness 2.5–4

Lepidolite sits at 2.5–4 on the Mohs scale — can be scratched by a steel knife.

Colors:
Streak
White
Crystal system
Monoclinic
SilicatesSilicates (Phyllosilicates — Micas)
TL;DR · 1 min read
Lepidolite (K(Li,Al)₃(Si,Al)₄O₁₀(F,OH)₂) is the lithium-bearing mica, distinctive for its lavender to pink color and book-like aggregates of glittering scales. It is a major lithium ore mineral and the most-collected lithium mica.

Lepidolite (K(Li,Al)₃(Si,Al)₄O₁₀(F,OH)₂) is the lithium-bearing mica, distinctive for its lavender to pink color and book-like aggregates of glittering scales. It is a major lithium ore mineral and the most-collected lithium mica. Pegmatites at Coronel Murta (Brazil), Pala (California), and Madagascar produce iconic specimens, often paired with rubellite tourmaline.

More minerals to explore

Other Members of the Mica Group

云母族

About Lepidolite

Lepidolite is a silicate mineral in the mica group (trilithionite-polylithionite series) and has the chemical formula K(Li,Al)3(Al,Si)4O10(F,OH)2. It crystallizes in the monoclinic system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.

Identification & care

Specimens usually show tabular pseudohexagonal crystals; scaly, platy, fine-grained masses; coarse books; typically in dense lepidolite aggregates. Its color range is broad, including lilac, pale purple, rose-pink, colorless, pale yellowish, and pale gray. The luster is vitreous, pearly, the streak is white, and specimens are typically transparent, translucent. The cleavage is perfect/basal on {001} — classic mica cleavage. The fracture is uneven (mica-like flexible flakes), which aids identification.

Collector context

How it forms

Lepidolite forms in granitic pegmatites — specifically lithium-rich pegmatites (lct type); often associated with other lithium minerals like tourmaline (elbaite), kunzite, and morganite. It is commonly found in association with elbaite (tourmaline), kunzite (spodumene), morganite (beryl), topaz, quartz, feldspar, columbite-tantalite.

Why collectors care

Lepidolite is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.

What affects value

Value in Lepidolite is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.

Naming history

The name Lepidolite has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.