The Dichroscope

Using the dichroscope to observe pleochroism in coloured gemstones, distinguishing dichroic from trichroic materials.

equipment/dichroscope pleochroism colour identification

Introduction

The dichroscope reveals pleochroism by showing two polarised images side by side.
It's essential for identifying coloured anisotropic gems and can help distinguish
natural from synthetic materials.

Pleochroism—the property of showing different colours in different crystallographic
directions—is diagnostic for many coloured gemstones.

Types of Dichroscope

Two main types are available:

Calcite Dichroscope

Uses a calcite rhomb (Iceland spar) to split the image:

  • More accurate: Clear separation of colours
  • Traditional choice: Preferred by professionals
  • Higher cost: More expensive than polaroid type
  • Fragile: Calcite can cleave if dropped

Polaroid Dichroscope

Uses polarising film to create two windows:

  • More affordable: Lower cost option
  • Durable: Less fragile than calcite
  • Good for field use: Compact and rugged
  • Slightly less clear: Colours may be slightly muted

Usage Technique

Proper technique is essential for accurate results:

Basic Procedure

  1. View the gem through the dichroscope with strong transmitted light
  2. Rotate the dichroscope (not the gem) while observing
  3. Look for colour differences between the two images
  4. Rotate the gem to find the direction of maximum colour difference
  5. Record both colours seen

Tips for Best Results

  • Use a strong, white light source
  • View through the body of the stone, not the surface
  • Check multiple directions (rotate the gem 90°)
  • Compare colours side by side in the two windows
  • Work with good eye relief (don't press against eyepiece)

Interpreting Results

Observation Interpretation Example Gems
Two identical colours Isotropic or viewing down optic axis Spinel, garnet, glass
Two different colours (dichroism) Uniaxial gem (trigonal, tetragonal, hexagonal) Ruby, sapphire, tourmaline
Three colours visible (trichroism) Biaxial gem (orthorhombic, monoclinic, triclinic) Tanzanite, alexandrite, iolite
No colour visible Colourless or very pale stone Colourless topaz, pale beryl

Pleochroism Strength

Pleochroism varies from very weak to very strong:

Strength Scale

  • None: Isotropic materials (no pleochroism)
  • Weak: Slight colour variation, difficult to see
  • Distinct: Clear difference but moderate
  • Strong: Obvious colour difference
  • Very strong: Dramatic colour change between directions

Factors Affecting Visibility

  • Colour saturation: Pale stones show less pleochroism
  • Viewing direction: Maximum difference perpendicular to optic axis
  • Light quality: Strong, white light shows colours best
  • Stone size: Larger stones show colours more clearly

Diagnostic Pleochroism

Characteristic Pleochroism by Gemstone
Gemstone Strength Colours
Ruby Strong Purple-red / orange-red
Blue sapphire Strong Violet-blue / greenish-blue
Emerald Distinct Blue-green / yellow-green
Tanzanite Strong (trichroic) Blue / purple / brown
Tourmaline Strong Variable, often dark / light of same hue
Alexandrite Strong (trichroic) Green / orange / purple-red
Kunzite Strong Pink / colourless
Iolite Very strong (trichroic) Violet / blue / pale yellow
Peridot Weak Yellow-green / green
Aquamarine Weak Colourless / pale blue
Andalusite Strong (trichroic) Yellow-green / brown / red
Hiddenite Distinct Yellow-green / blue-green
Zircon (blue) Weak Blue / colourless

Dichroism vs Trichroism

Understanding the distinction:

Dichroic Gems (Uniaxial)

Uniaxial crystals have two principal optical directions and show
two pleochroic colours. These belong to:

Trichroic Gems (Biaxial)

Biaxial crystals have three principal optical directions and can
show three distinct pleochroic colours. These belong to:

To see all three colours, rotate the gem to view along different axes.

Practical Applications

Common Mistakes

Avoid these errors when using the dichroscope:

  • Rotating the gem instead of the dichroscope initially
  • Using reflected light instead of transmitted light
  • Not checking multiple directions in the stone
  • Confusing colour zoning with pleochroism
  • Testing opaque or heavily included stones (no light transmission)