Types of Iridescent Gemstones & Minerals

Types of Iridescent Gemstones & Minerals
Types of Iridescent Gemstones & Minerals

Iridescence is the play of color, or a series of colors, produced by interference or diffraction (or both), either when light is reflected from thin films (inclusions), twinning planes or from the unique structure of precious opal.

There are several types of iridescence that have their own particular causes:

  • Labradorescence
  • Adularescence (or Schiller)
  • Aventurescence
  • Opalescence 

Labradorescence Types of Iridescent Gemstones & Minerals
Polished labradorite


Labradorescence is the effect seen in Labradorite (a Feldspar) and Spectrolite (a Labradorite found in Finland). It is caused by interference on the boundaries of lamellar twin planes, which are usual in Feldspars. Many Labradorites are carved to exploit this unique type of sheen.

Adularescence Types of Iridescent Gemstones & Minerals
Unpolished moonstone. Photo: Crystalarium


This type of sheen is exhibited in Moonstone (another Feldspar), caused by reflection on Moonstone's lamellar twinning planes. The effect is a blue color floating just below the surface of the stone. Adularescence is also known as Schiller.

Rainbow pyrite Types of Iridescent Gemstones & Minerals
Rainbow pyrite, a variety of mineral pyrite. The iridescence is caused by tarnishing by oxidation and molybdenum traces in the mineral. Photo: Ryan lay


Aventurescence is named after Aventurine Feldspar, which is also known as Sunstone. This type of iridescence is due to the play of color caused by reflection on tiny, thin inclusions of goethite and hematite (or both). This gives the stone a golden or reddish-brown color and specular reflections.

Opalescence Types of Iridescent Gemstones & Minerals
Stunning Australian opal! Photo: Able Ground


The causes of play of color in Opal were long uncertain until the invention of the electron microscope. This enabled scientists to see the unique structure of Opal at high magnification, and to discover that Opal is made up of small spheres of silica.

In Opal, both interference and diffraction play a role in the play of color. Interference occurs when part of the light gets reflected from the surface of a silica sphere while another part gets refracted inside the sphere, being reflected again. Diffraction in Opal is the result of light hitting a gap between the spheres and then being split up into its spectral components.

In precious Opal, larger silica spheres of about 350 ┬Ám (micro meters) in diameter give off red flashes with changes in viewing angles. The smaller spheres result in green, blue or purple flashes which cannot increase in wavelength to give a red flash. Therefore, the sizes of the 'gaps', or 'voids', determine which color is seen.

An ammolite gemstone is a fossil ammonite.
Ammolite is a rare iridescent gemstone formed from the fossilized shell of Ammonite.
  Photo: Lou (@themineralcollective)

See also: 
How Do Asterism Minerals Form?
Why Fluorite Comes in Different Colors? With Examples
How Do Opalised Fossils Form?
What Is Cat's Eye Effect Observed in Some Minerals?
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