COMPARE

Side by side

Put up to four minerals or gems next to each other and test them like a gemmologist.

Spinel
Gem Tajikistan

Spinel

MgAl₂O₄

Ruby
Gem Tajikistan

Ruby

Al₂O₃

VERDICT

How to tell them apart

Worked out from the values below; a gem lab would confirm with several tests.

THE TESTS

Gem-testing instruments

Scratch test

Mohs hardness: a mineral scratches anything softer than itself.

Heavy liquid

Density in g/cm³: denser stones sink deeper.

2.02.53.03.54.04.5bromoform 2.89methylene iodide 3.32
  • Spinel 3.6–4.1
  • Ruby 3.98–4.1

Refractometer

Refractive index: how strongly the stone bends light. See light bend through a 3D crystal →

1.401.451.501.551.601.651.701.751.80
  • Spinel 1.719
  • Ruby 1.759–1.772

Polariscope

Between crossed polarisers a doubly refractive stone blinks as it turns; a singly refractive one stays dark. See light bend through a 3D crystal →

SpinelSingle refraction: stays dark
RubyDouble refraction: blinks
0°

Crystal structures

Unit cells side by side. Drag any of them: they all turn together.

SpinelCubic

RubyTrigonal

PROPERTIES

All properties

SpinelRuby
Type Gem Gem
MineralSpinelCorundum
Formula MgAl₂O₄ Al₂O₃
Mineral group Oxides Oxides
Crystal system Cubic Trigonal
Mohs hardness 7.5–8 9
Density 3.6–4.1 g/cm³; composition controls the range 3.98–4.10 g/cm³
Refractive index n ≈ 1.719 for Mg-rich spinel; rises with Fe, Zn, and Cr substitution nω about 1.767–1.772; nε about 1.759–1.763
Optical class Isotropic Uniaxial (−)
Colour Red and pink are classic; also blue, violet and other colours Red to purplish red
Colour cause Red spinel is coloured by chromium, the same trace element that colours ruby and emerald. Chromium is the trace element behind ruby's red, which ranges from orangy red to purplish red; more chromium gives a stronger red. Chromium also makes ruby fluoresce red, which intensifies its colour. Rubies formed in marble, such as those from Myanmar, the Himalayas and northern Vietnam, contain little iron, so their red is especially intense.
Treatments — Ruby can be treated to change its colour, apparent clarity or durability. GIA research has documented low-temperature heating, flux healing of fissures, and filling of fractures with glass.
Look-alikes Spinel was mistaken for ruby for centuries, and many famous historical "rubies" are spinel — among them the Black Prince's Ruby set in the front of Britain's Imperial State Crown and the Timur Ruby, which weighs over 350 carats and carries several Persian inscriptions. The two were separated scientifically only in 1783, when Jean-Baptiste Louis Romé de l'Isle distinguished them by their crystal shapes (GIA reading list). Red spinel is coloured by the same element, chromium, and was mistaken for ruby for centuries (see Spinel). Laboratory-grown ruby, with essentially the same chemical, physical and optical properties, also exists.
Crystal habit Octahedral crystals are classic; also dodecahedral, granular, or massive. Contact twins on {111} define the spinel law. Barrel-shaped, pyramidal, tabular, or prismatic crystals; also granular and massive. Parting and growth features may be prominent.
Cleavage Imperfect parting on {111}; true cleavage is indistinct No true cleavage; common basal and rhombohedral parting
Fracture Conchoidal to uneven or splintery Uneven to conchoidal
Tenacity Brittle Brittle, but compact material is tough
Luster Vitreous Adamantine to vitreous
Streak White White
Transparency Transparent to opaque Transparent to opaque
Fluorescence Usually inert, though some specimens fluoresce; trace elements can produce strong colour. Variable; ruby may fluoresce red under ultraviolet light and some material phosphoresces.
Identification Look for octahedral form, high hardness (7.5–8), lack of strong cleavage, and isotropic optics. Red spinel is singly refractive, unlike doubly refractive ruby. Its hardness of 9 is decisive: it scratches nearly every common mineral. High density and parting help distinguish it; ruby and sapphire are colour varieties of corundum, not separate mineral species.
In Tajikistan Kuh-i-Lal in the Ishkoshim district is the historic source of gem spinel, the "balas ruby" of Badakhshan. Gem ruby is documented from the marble-hosted Snezhnoe deposit in the Kukurt district, Eastern Pamir.
SourceHandbook of Mineralogy — SpinelHandbook of Mineralogy — Corundum