Spodumene

Crystal system · Monoclinic

Spodumene is an inosilicate mineral prized by collectors for its exceptional color range, with known Chinese sources.

About Spodumeneextended article

Crystal Structure
Monoclinic single-chain pyroxene with Li.
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen51.59%
Si Silicon30.18%
Al Aluminum14.50%
Li Lithium3.73%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Spd
→ Spodumene
Li pyroxene
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈspɒdʒəmiːn/
SPOJ-uh-meen
Greek "burnt to ashes"
UV Fluorescence
SW (254 nm)
none
LW (365 nm)
Orange (kunzite)
moderate
Kunzite shows orange LW; pure spodumene inert.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Tenacity
Behavior:
brittle
Under stress:
Prismatic cleavage
Same as kunzite.
Luster
vitreous
Same.
Diaphaneity (Transparency)
transparent
Including kunzite and hiddenite.
Type Locality
Utö Island — Sweden
Described 1800 by d'Andrada
Specific Gravity
3.15–3.21
g/cm³
medium
Lithium pyroxene.
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 · Lepidolite · Feldspar · Quartz
Major Li ore; gemmy variants are kunzite (pink) and hiddenite (green).
Cleavage & Fracture
Cleavage:
perfect 2 directions {110} ~87°
Fracture:
subconchoidal
Perfect prismatic cleavage; brittle.
Market availability: Uncommon
Found at major shows and select dealers. Quality varies by locality.
Collector tier: Solid Display
Reliable mid-tier display species. Easy to find in well-formed examples; broad locality diversity.
Named varieties — color spectrum
Often found withTourmaline · Quartz · Lepidolite · Beryl
Mohs 6.5–7
Vickers (~) 1400 HV
Knoop (~) 1100 HK
Geological setting
Pegmatite
Element composition by mass

Formula: LiAlSi₂O₆ · molar mass: 186.09 g/mol

O 51.59%
Si 30.18%
Al 14.5%
Li 3.73%

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

GroupPyroxene Group
Related members: Augite · Diopside · Jadeite · Hedenbergite · Aegirine · Enstatite
Optical Effects
Pleochroic
Mohs Hardness 6.5–7

Spodumene sits at 6.5–7 on the Mohs scale — harder than glass; scratches steel.

Colors:
Streak
White
Crystal system
Monoclinic
Pronunciation/ˈspɒdjuːmiːn/
Discovery First described 1800 by D'Andrada (Sweden)
SilicatesSilicates (Inosilicates — Pyroxenes)
TL;DR · 1 min read
Spodumene (LiAlSi₂O₆) is the lithium-bearing pyroxene and the principal lithium ore mineral worldwide. Two gem varieties make Spodumene a collector classic: kunzite (pink-violet, Mn-bearing) and hiddenite (emerald-green, Cr-bearing).

Spodumene (LiAlSi₂O₆) is the lithium-bearing pyroxene and the principal lithium ore mineral worldwide. Two gem varieties make Spodumene a collector classic: kunzite (pink-violet, Mn-bearing) and hiddenite (emerald-green, Cr-bearing). Pegmatites at Pala (California), Minas Gerais (Brazil), and Afghanistan supply gem material.

More minerals to explore

About Spodumene

Spodumene belongs to the inosilicate class in the pyroxene group — clinopyroxene and has the chemical formula LiAlSi2O6. 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

Spodumene typically forms large striated prismatic crystals; often enormous in pegmatites; cleavable masses. Its color range is broad, including colorless, white, gray, green (hiddenite), pink/purple (kunzite), and yellow. The luster is vitreous to pearly, the streak is white, and specimens range from transparent (gem varieties) to translucent/opaque. The cleavage is perfect on {110} at nearly 90° (pyroxene cleavage). The fracture is uneven to subconchoidal, which aids identification.

Collector context

How it forms

The geological setting for Spodumene is typically granitic pegmatites, especially li-cs-ta (lct) type; the defining li mineral in li-rich pegmatites. It is commonly found in association with lepidolite, tourmaline (elbaite), beryl, columbite, quartz.

Classic Chinese localities

Spodumene is widely represented across Chinese provinces, including Hunan, Yunnan, Sichuan, Hubei.

Why collectors care

Spodumene 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 Spodumene 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 Spodumene 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.