Spinel

Crystal system · Isometric

Spinel is an oxide mineral valued for its hardness and gem potential, with several world-class Chinese localities.

About Spinelextended article

Crystal Structure
Cubic close-packed O²⁻; Mg in tetrahedral, Al in octahedral.
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen44.98%
Al Aluminum37.93%
Mg Magnesium17.08%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Spl
→ Spinel
Mg-Al oxide
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/spɪˈnɛl/
spih-NELL
two syllables (Latin spinella)
Lapidary & Faceting Recommendations
Recommended cut:
cushion
Also seen:
oval, round brilliant, pear
Typical yield:
35% of rough
Isotropic — no pleochroism concerns. Singly refractive gives diamond-like brilliance.
Birthstone & Anniversary Gift Reference
August (zodiac)zodiac: Leo / Virgo
UV Fluorescence
SW (254 nm)
none
LW (365 nm)
Red
strong
Cr-bearing red/pink spinel fluoresces strongly LW red.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Famous specimens of this species
Black Prince's Ruby — ~170 ct
Actually a red spinel, not a ruby. Set in the Imperial State Crown above Cullinan II.
Origin: Badakhshan, Afghanistan. Now at: British Crown Jewels. Recorded before 1367.
Timur Ruby — 352.5 ct
Another famous "ruby" that is actually red spinel. Bears Persian inscriptions of past owners.
Origin: Badakhshan, Afghanistan. Now at: British Crown Jewels. Recorded pre-1612.
Tenacity
Behavior:
brittle
Under stress:
Shatters under blow
No cleavage; brittle fracture.
Luster
vitreous
Glass-like brightness.
Color Cause (Chromophore)
Chromophore:
Cr³⁺ / Fe³⁺
Mechanism:
idiochromatic
Color produced:
red / blue / pink
Red spinel: Cr (similar mechanism to ruby). Blue/black: Fe.
Diaphaneity (Transparency)
transparent
Highest-quality spinel rivals corundum in transparency.
Type Locality
Lake Manyara — Tanzania
Described 1546 by Latin "spinella"
Specific Gravity
3.58–3.61
g/cm³
medium
Lighter than corundum — important separation tool.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Synthetics & Imitations
Lab-grown methods
Verneuil flame fusion 1908 · Verneuil
Common in jewelry as birthstone simulant.
Flux growth 1965 · Chatham
Less common — rare to find as gem-grade flux spinel.
Common imitations
Glass
Color matches; lower RI, bubbles.
Synthetic corundum
Verneuil synthetic ruby/sapphire often sold as "spinel" colors.
Geological Setting
Environment:
metamorphic
Host rock:
marble, serpentinite
Companions:
Corundum · Mica · Forsterite
Mogok (Burma) red/pink spinel from contact-metamorphic marbles. Tajik and Vietnamese pink spinel similar.
Treatments & Enhancements
(generally untreated)stable· detection: n/a
Spinel is one of the few important gems that is essentially never treated. Marketed as "natural untreated".
As a buyer: request written disclosure of treatments and confirm whether the price reflects treated or untreated material.
Characteristic Inclusions
Octahedral crystalssolid★ diagnostic
Smaller spinel octahedra arranged in trails or "fingerprints" — Burmese diagnostic.
Apatite needlessolid
Hexagonal apatite prisms common in pink/red spinel.
Diagnostic inclusions are characteristic enough to help identify origin or species under 10× loupe.
Twinning Laws
Spinel lawcontact
Twin plane {111} — flattened triangular crystals. Eponymous twin law for the cubic system.
Formation eraHigh-T metamorphic + magmatic; Burmese spinels Cenozoic uplift.
Cleavage & Fracture
Cleavage:
none — (parting on {111})
Fracture:
conchoidal
Parting can mimic cleavage in heavily twinned material.
Market availability: Uncommon
Found at major shows and select dealers. Quality varies by locality.
Collector tier: Cabinet Classic
World-class display species — sought after for cabinet collections, well-documented localities, frequent show-piece pieces.
Often found withOlivine · Corundum · Magnetite · Chondrodite
Mohs 7.5–8
Vickers (~) 1650 HV
Knoop (~) 1340 HK
Nickel–Strunz 4.BB.05
Dana 07.02.01.01
Geological setting
Placer
Element composition by mass

Formula: MgAl₂O₄ · molar mass: 142.27 g/mol

O 44.98%
Al 37.93%
Mg 17.08%

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

GroupSpinel Group
Related members: Magnetite · Chromite · Gahnite
Mohs Hardness 7.5–8

Spinel sits at 7.5–8 on the Mohs scale — very hard; only diamond or corundum scratches it.

Colors:
Streak
White
Crystal system
Isometric (Cubic)
Type localitySri Lanka (Ceylon)
Discovery First described 1779 by Jean-Baptiste Romé de l'Isle
Oxides & HydroxidesOxides
TL;DR · 1 min read
Spinel (MgAl₂O₄) is the parent species of the spinel oxide group and a cherished gem mineral for centuries. Famous historical "rubies" turned out to be red spinels — including the "Black Prince's Ruby" in the British Crown Jewels and Russia's "Tamerlane Ruby.

Spinel (MgAl₂O₄) is the parent species of the spinel oxide group and a cherished gem mineral for centuries. Famous historical “rubies” turned out to be red spinels — including the “Black Prince’s Ruby” in the British Crown Jewels and Russia’s “Tamerlane Ruby.” Modern gem spinels come from Mogok (Myanmar) and Mahenge (Tanzania), with bright red, pink, and cobalt-blue varieties.

More minerals to explore

About Spinel

Spinel is an oxide mineral in the spinel group and has the chemical formula MgAl2O4. It crystallizes in the isometric 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

Spinel typically forms octahedral crystals (classic habit), sometimes twinned (spinel twins/macles); massive, granular. Its color range is broad, including colorless, white, red (ruby spinel), pink, orange, blue, green, purple, brown, black, and virtually every color possible. The luster is vitreous, the streak is white, and specimens range from transparent to opaque. The cleavage is imperfect on {111}. The fracture is conchoidal, uneven, which aids identification.

Collector context

How it forms

Spinel forms in mafic/ultramafic igneous rocks and their metamorphic derivatives; marble and calc-silicate skarns; alluvial gem gravels. It is commonly found in association with corundum (ruby/sapphire), pyrope garnet, diopside, calcite, dolomite, phlogopite.

Classic Chinese localities

Documented Chinese occurrences are recorded at Shangbao Mine, Xianghualing Sn-polymetallic ore field and Yaogangxian W-Sn ore field, among others.

Why collectors care

Spinel occupies a rare position: it matters equally to specimen collectors and to the gem trade. Crisp natural crystals with saturated color and good clarity command premium pricing and are among the highest-prestige targets in any systematic collection.

What affects value

Value in Spinel is assessed, in typical order of weight, against: (1) locality provenance; (2) crystal size; (3) transparency and internal clarity; (4) color intensity and saturation; (5) crystal form and termination sharpness; (6) matrix and associated-species aesthetics; (7) gem-cutting potential. Verified locality documentation and cutting potential further elevate collector demand.

Naming history

The name Spinel 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.