Gemstone Windows and Dark Patches: What to Look for in a Cut Gem

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AI-generated educational illustration. Conceptual only; not a photograph of an actual specimen or location. A coloured gem may have a pale, see-through centre or areas that look almost black. Both affect its appearance, but they do not have the same cause. What is a window? A window is an area where light passes through the gem instead of being returned towards the viewer. You may see the background through it, especially near the centre. Cutting angles and the material's refractive index—how it bends light—help determine whether this happens. There is no single ideal depth for every gemstone. Why dark patches need a closer look Darkness can have several causes. The material may absorb a lot of light. Some facets may reflect dark surroundings or the observer. Extinction is another cause, involving light that is not returned to the viewer after internal reflection. For that reason, calling every black patch “extinction” can be misleading. A simple viewing routine Look at the gem fac...

The polariscope (polarization)

 Basic

A polariscope is a gem identification tool that employs polarised light. There are two polarised filters on the instrument, one on top and one on the bottom. Both the polarizer and the analyzer have vibrational planes of their own. The field between them stays black when the polarizer's vibrational plane is at right angles to the analyzer's vibrational direction. The "crossed position" is the name for this pose. Gems can be examined in this position to see if they are: isotropic anomalously double refractive (ADR) anisotropic anisotropic aggregate

Operation of the polariscope and possible observations

Turn on the light source and set the gemstone on the rotating platform immediately above the polarizer with the polarizer and analyzer crossed (this platform might not always be present, in which case you use your tweezers). You'll get four options if you look at the gemstone via the analyser while gently spinning it. 1. The stone appears dark throughout a 360° rotation. The stone is isotropic (singly refractive). 2. The stone will show anomalous double refraction (ADR). It is isotropic (singly refractive). 3. Throughout a 360° rotation the stone blinks 4 times, light and dark. The stone is anisotropic (double refractive). 4. The stone will appear light all the time. The stone is a microcrystalline or cryptocrystalline aggregate (like, for instance, chalcedony).


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