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Overview of the crystal systems and their optical properties

Structure Structure type
Crystal axes
Angles
Symmetry
(of highest
crystal class)
Optic
character
Refractive
index (RI)
Optic sign Pleochroism Gem
examples
Amorphous No order

No axes

No symmetry Isotropic

Singly refractive

1 RI

n

None None Glass

Amber

Cubic Isometric: 1 axis length

a1 = a2 = a3
All at 90°

13 planes

9 axes
Center

Isotropic

Singly refractive

1 RI

n

None None

Diamond
Spinel
Garnet

Tetragonal Dimetric: 2 axis lengths

a1 = a2 ≠ c
All at 90°

5 planes

5 axes
Center

Anisotropic

Doubly refractive
Uniaxial

2 RIs

nω and nε

+ = nε > nω

– = nε < nω

May be dichroic Zircon
Hexagonal Dimetric: 2 axis lengths

a1 = a2 = a3 ≠ c
a axes at 60°;
c axis at 90° to their plane

7 planes

7 axes
Center

Anisotropic

Doubly refractive
Uniaxial

2 RIs

nω and nε

+ = nε > nω

– = nε < nω

 

May be dichroic Beryl

Apatite

Trigonal Dimetric: 2 axis lengths

a1 = a2 = a3 ≠ c
a axes at 60°;
c axis at 90° to their plane

3 planes

4 axes
Center

Anisotropic

Doubly refractive
Uniaxial

2 RIs

nω and nε

+ = nε > nω

– = nε < nω

 

May be dichroic Corundum

Quartz
Tourmaline

Orthorhombic Trimetric: 3 axis lengths

a ≠ b ≠ c
All at 90°

3 planes

3 axes
Center

Anisotropic

Doubly refractive
Biaxial

3 RIs

nα, nβ, nγ

+ = nβ closer to nα

– = nβ closer to nγ

± = nβ midway to nα & nγ
May be trichroic Topaz

Zoisite
Olivine (peridot)

Monoclinic Trimetric: 3 axis lengths

a ≠ b ≠ c
2 axes at 90°; 1 oblique

1 axis

1 plane
Center

Anisotropic

Doubly refractive
Biaxial

3 RIs

nα, nβ, nγ

+ = nβ closer to nα

– = nβ closer to nγ
± = nβ midway to nα & nγ

May be trichroic Orthoclase

Spodumene

Triclinic Trimetric: 3 axis lengths

a ≠ b ≠ c
all axes oblique

No planes

No axes
Center

Anisotropic

Doubly refractive
Biaxial

3 RIs

nα, nβ, nγ

+ = nβ closer to nα

– = nβ closer to nγ
± = nβ midway to nα & nγ

May be trichroic Axinite

Labradorite

Optic character/sign with the Refractometer

Optic character/curve variations: Uniaxial or biaxial

  1. Two constant curves = Uniaxial
  2. Two variable curves = Biaxial
  3. One constant/one variable, which meet but do not cross = Uniaxial
  4. One constant/one variable which don't meet
  5. Check the polaroid angle of the constant curve
    • Biaxial = polaroid angle of constant curve = 90°
    • Uniaxial = polaroid angle of constant curve ≠ 90°

RI readings of corundum

RI readings for different faces on corundum. Corundum is uniaxial negative.
Illustration © Richard W. Hughes

Optic sign

Uniaxial stones

  1. High RI curve varies = (+)
  2. Low RI curve varies = (-)
  3. Both curves constant: At 0° polaroid angle, only the o-ray is seen
    • a. If low curve is seen = (+)
    • b. If high curve is seen = (-)

Biaxial stones

  1. If nβ is closer to nα, the gem is (+)
  2. If nβ is closer to nγ, the gem is (-)
  3. If nβ is halfway between nα and nγ, the gem is (±)
  4. If two possible betas exist, false beta will have a polaroid angle equal to 90°. True beta will have a polaroid angle unequal to 90°.

Polaroid angle

Symbols

Uniaxial crystals

Biaxial crystals

This page is http://www.ruby-sapphire.com/crystal_optics.htm
Page updated 11 March, 2010

 

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