An Introduction to Gemstone Inclusions

Magnification opens the door to a fascinating dimension in gemology — the inner world of gemstone inclusions. You’ll see marvels that can rival the beauty and intrigue of the gem itself. On a practical level, identifying inclusions may help you identify the gem species.
Reading time: 3 min 17 sec
Gemstone Inclusions - Apatite in Spinel
This rounded apatite crystal displays interference colors between crossed polars in a Burmese spinel. “Natural Spinel, Tanzania; Mahenge.” Photo by E. Billie Hughes. © Lotus Gemology. Used with permission.

Gemstone inclusions can also reveal how a gem was formed and whether it’s a natural or synthetic stone. Some gems have specific inclusions that their lookalikes lack. Some inclusions only occur in a single gemstone species or even in a single mine!

What are Gemstone Inclusions?

Simply put, an inclusion is any material that is trapped inside of another mineral while that mineral forms. For example, crystals, liquid or gas bubbles, or even fractures caused by radioactive material in the host material may comprise gemstone inclusions. Since researchers constantly discover new inclusions and varieties, a listing of inclusions can never be complete.

Gemstone Inclusions - Petroleum in Quartz
This quartz stone has petroleum inclusions. Photo by Luciana Barbosa. Licensed under CC By-SA 3.0

Viewing Gemstone Inclusions

Inclusions are instrumental in identifying many gemstone species. Nevertheless, viewing inclusions can be difficult. To study them, gemologists often use a microscope, preferably one with dark-field illumination. While a magnification of 30-60X (the range of most stereoscopic microscopes) may resolve many inclusions, some of the tinier ones require magnification of 200X or more.

Knowing how to use your microscope and various lighting techniques are essential skills for identifying inclusions. However, getting tiny details into sharp focus often proves quite challenging, if not impossible, in some cases. Sometimes, student gemologists can easily jump to conclusions about what they see through magnification.

Gemstone Inclusions - Diamond Inclusions
These drawings illustrate types of diamond inclusions.

Learning How to Distinguish Gemstone Inclusions

Discretion is essential. For example, can you make out the inclusion in the garnet pictured below? It’s difficult to tell if the ends are terminated or if they’re bubbles. As it turns out, they’re terminated. This means the inclusion is a crystal. Crystal inclusions indicate a natural garnet, while bubbles would indicate a cheap synthetic. Thus, identifying this inclusion correctly would be critical.

Gemstone Inclusions - Crystal in Garnet
Crystals or bubbles?

If you can’t see an inclusion clearly enough to distinguish its features, don’t base an identification on it. If you’re in doubt, look at all the available clues. A standard gemstone identification procedure should yield enough information to make a proper identification.

Learning to locate inclusions and distinguish their varieties takes practice. Pictures and descriptions serve only as guides. Gemology students should examine as many gemstones as possible. Use your loupe first and then your microscope. Keep practicing until you’re an expert at finding and identifying inclusions.

gemstone inclusions - peridot with ludwigite
Peridots can be identified by the presence of a “lily pad” type of inclusion. However, this peridot from Pakistan also contains needle-like crystals of ludwigite, a very rare mineral. This crystal weighs 34 grams and measures 5.3 x 2.1 x 1.4 cm. © Rob Lavinsky, Used with permission.

More Resources for Identifying Gemstone Inclusions

Do you want to learn more about inclusions? The International Gem Society (IGS) has a four-part series of Members Only Premium articles on gemstone inclusions. These articles document the primary inclusion varieties commonly used for gemstone identification.

Gemstone Inclusions - Dolomite and Rutile in Quartz
For more stunning photographs of gemstone inclusions like this one, see our article on gemstone photomicrography. “Dolomite in Quartz with rutile, Minas Gerais, Brazil.” Photo by Danny J. Sanchez. Field of view = 5.2mm • Depth of field = 2.25mm.

About the author
Joel E. Arem, Ph.D., FGA
Dr. Joel E. Arem has more than 60 years of experience in the world of gems and minerals. After obtaining his Ph.D. in Mineralogy from Harvard University, he has published numerous books that are still among the most widely used references and guidebooks on crystals, gems and minerals in the world. Co-founder and President of numerous organizations, Dr. Arem has enjoyed a lifelong career in mineralogy and gemology. He has been a Smithsonian scientist and Curator, a consultant to many well-known companies and institutions, and a prolific author and speaker. Although his main activities have been as a gem cutter and dealer, his focus has always been education.
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About the author
Donald Clark, CSM IMG
Donald Clark, CSM founded the International Gem Society in 1998. Donald started in the gem and jewelry industry in 1976. He received his formal gemology training from the Gemological Institute of America (GIA) and the American Society of Gemcutters (ASG). The letters "CSM" after his name stood for Certified Supreme Master Gemcutter, a designation of Wykoff's ASG which has often been referred to as the doctorate of gem cutting. The American Society of Gemcutters only had 54 people reach this level. Along with dozens of articles for leading trade magazines, Donald authored the book "Modern Faceting, the Easy Way."
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