COMPARE

Side by side

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

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
  • Sapphire 3.98–4.1
  • Diamond 3.52

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
  • Sapphire 1.759–1.772
  • DiamondOTL 2.417

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 →

SapphireDouble refraction: blinks
DiamondSingle refraction: stays dark
0°

Crystal structures

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

SapphireTrigonal

DiamondCubic

PROPERTIES

All properties

SapphireDiamond
Type Gem Gem
MineralCorundumDiamond
Formula Al₂O₃ C
Mineral group Oxides Native elements
Crystal system Trigonal Cubic
Mohs hardness 9 10
Density 3.98–4.10 g/cm³ 3.52 g/cm³
Refractive index nω about 1.767–1.772; nε about 1.759–1.763 n 2.417
Optical class Uniaxial (−) Isotropic
Colour Blue and every non-red gem colour Colourless and fancy colours
Colour cause Traces of iron and titanium — only a few hundredths of a percent — turn corundum blue; more iron gives a darker blue. Chromium produces pink sapphire. Sapphire also occurs in violet, green, yellow, orange, purple, grey, black and brown. —
Look-alikes Colourless sapphire was once a popular diamond imitation. Laboratory-grown sapphire is durable enough to be used for supermarket-scanner and spacecraft windows. Colourless sapphire was once a popular diamond imitation (see Sapphire).
Crystal habit Barrel-shaped, pyramidal, tabular, or prismatic crystals; also granular and massive. Parting and growth features may be prominent. Most commonly octahedral, dodecahedral or cubic crystals; faces may show triangular growth or dissolution features.
Cleavage No true cleavage; common basal and rhombohedral parting Perfect on {111}
Fracture Uneven to conchoidal Conchoidal
Tenacity Brittle, but compact material is tough Brittle despite exceptional hardness
Luster Adamantine to vitreous Adamantine
Streak White White
Transparency Transparent to opaque Transparent to opaque
Fluorescence Variable; ruby may fluoresce red under ultraviolet light and some material phosphoresces. Fluorescence varies; blue is common, but response and strength are not diagnostic by themselves.
Identification 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. Mohs hardness 10, adamantine luster, perfect octahedral cleavage and very high thermal conductivity are characteristic; reliable identification requires gemological testing.
In Tajikistan Sapphire is documented together with ruby at the Snezhnoe deposit in the Kukurt district, Eastern Pamir. —
SourceHandbook of Mineralogy — CorundumHandbook of Mineralogy — Diamond