Sapphire Inclusions
Explore sapphire inclusions in Hyperion, the Lotus Gemology inclusion database. Hyperion contains photomicrographs of inclusions and internal features in natural sapphire, documented with information on geographic origin, treatment, lighting conditions, field of view, photographer and published references.
This color-change sapphire from Madagascar contained many zircon crystals that showed clear evidence of heat treatment, including cloudiness.
Natural Color-Change Sapphire •
Madagascar •
Enhancements:
Heat (H) •
Lighting Conditions:
Fiber Optic: Oblique
Photographer:
E. Billie Hughes •
Image Number:
A-001-3514-2
This color-change sapphire from Madagascar contained many zircon crystals that showed clear evidence of heat treatment, including cloudiness and glassy discoid fractures around them.
Natural Color-Change Sapphire •
Madagascar •
Enhancements:
Heat (H) •
Lighting Conditions:
Diffuse Light Field (Transmitted Light)
Photographer:
E. Billie Hughes •
Image Number:
A-001-3514-1
A complex structure of tiny exsolved particles and milky texture clouds outline the shape of this crystal at an earlier stage in its growth. This stone is from Queensland’s Lava Plains mines. The black crystal in the center is probably columbite (a.k.a. niobite).
Natural Sapphire •
Australia •
Enhancements:
None Detected (None) •
Lighting Conditions:
Dark Field + Oblique Fiber Optic
Photographer:
E. Billie Hughes •
Image Number:
A-001-3513-4
Sutherland, F.L., Coenraads, R.R. et al. (2015) Corundum (sapphire) and zircon relationships, Lava Plains gem fields, NE Australia: Integrated mineralogy, geochemistry, age determination, genesis and geographical typing. Mineralogical Magazine, Vol. 79, No. 3, pp. 545–581; not seen.
Note that the fingerprint (a partially healed fracture) in this stone has hexagonal zones. This indicates that the fingerprint formed parallel to the basal pinacoid.
Natural Sapphire •
Australia •
Enhancements:
None Detected (None) •
Lighting Conditions:
Fiber Optic: Oblique
Photographer:
E. Billie Hughes •
Image Number:
A-001-3513-3
Sutherland, F.L., Coenraads, R.R. et al. (2015) Corundum (sapphire) and zircon relationships, Lava Plains gem fields, NE Australia: Integrated mineralogy, geochemistry, age determination, genesis and geographical typing. Mineralogical Magazine, Vol. 79, No. 3, pp. 545–581; not seen.
A complex structure of tiny exsolved particles and milky texture clouds outline the shape of this crystal at an earlier stage in its growth. This stone is from Queensland’s Lava Plains mines.
Natural Sapphire •
Australia •
Enhancements:
None Detected (None) •
Lighting Conditions:
Fiber Optic: Oblique
Photographer:
Richard W. Hughes •
Image Number:
A-001-3513-2
Sutherland, F.L., Coenraads, R.R. et al. (2015) Corundum (sapphire) and zircon relationships, Lava Plains gem fields, NE Australia: Integrated mineralogy, geochemistry, age determination, genesis and geographical typing. Mineralogical Magazine, Vol. 79, No. 3, pp. 545–581; not seen.
A delightful sight. This pinkish purple sapphire from Serendib features a lovely iridescent fingerprint, its structure mimicing the underlying atomic pattern of its host.
Natural Sapphire •
Sri Lanka (Ceylon) •
Enhancements:
None Detected (None) •
Lighting Conditions:
Fiber Optic: Oblique
Photographer:
E. Billie Hughes •
Image Number:
A-001-3509-1
Roedder, E. (1962) Ancient fluids in crystals. Scientific American, Vol. 207, pp. 38–47; RWHL*.
Hughes, R.W. (1997) Ruby & Sapphire. Boulder, CO, RWH Publishing, 512 pp.; RWHL*.
Tiny black dendrites inhabit the sticky blue world of this sapphire from Madagascar, growing amidst the small pockets of undigested fluid in a fingerprint.
Natural Sapphire •
Madagascar •
Enhancements:
None Detected (None) •
Lighting Conditions:
Fiber Optic: Oblique
Photographer:
Wimon Manorotkul •
Image Number:
A-001-3480-1
Exsolved rutile silk lights up the interior of this natural blue sapphire from Sri Lanka. It is these inclusions that give rise to the stars in cabochon-cut stones.
Natural Sapphire •
Sri Lanka (Ceylon) •
Enhancements:
None Detected (None) •
Lighting Conditions:
Fiber Optic: Oblique
Photographer:
Richard W. Hughes •
Image Number:
A-001-3478-1
The clear, undamaged, euhedral form of this crystal, suspended in its sapphire host, provides evidence that the stone is unheated.
Natural Sapphire •
Sri Lanka (Ceylon) •
Enhancements:
None Detected (None) •
Lighting Conditions:
Dark Field
Photographer:
E. Billie Hughes •
Image Number:
A-001-3468-1
Hughes, R.W. (1997) Ruby & Sapphire. Boulder, CO, RWH Publishing, 512 pp.; RWHL*.
Polysynthetic twinning is secondary twinning, forming after the host crystal grew. When the stone is placed between crossed polars, the dazzling colors of these polysynthetic twin planes can be easily seen.
Natural Sapphire •
Madagascar •
Enhancements:
None Detected (None) •
Lighting Conditions:
Diffuse Light Field + Crossed Polars
Photographer:
E. Billie Hughes •
Image Number:
A-001-3471-1
Hughes, R.W. (1997) Ruby & Sapphire. Boulder, CO, RWH Publishing, 512 pp.; RWHL*.
Like Mother Nature’s snow globe, Sri Lankan sapphire often has negative crystals containing other inclusions. In this example we can see small diaspore needles and black graphite flakes inside the cavities.
Natural Sapphire •
Sri Lanka (Ceylon) •
Enhancements:
None Detected (None) •
Lighting Conditions:
Dark Field + Oblique Fiber Optic
Photographer:
E. Billie Hughes •
Image Number:
A-001-3462-4
Roedder, E. (1962) Ancient fluids in crystals. Scientific American, Vol. 207, pp. 38–47; RWHL*.
Hughes, R.W. (1997) Ruby & Sapphire. Boulder, CO, RWH Publishing, 512 pp.; RWHL*.
When a rutile-silk containing sapphire is heated, titanium from the rutile dissolves into the surrounding sapphire. Once in solid solution, the titanium reacts with iron, creating a blue color. The result is tiny blue halos surrounding the remnants of the rutile silk, a process dubbed “inkspot internal diffusion” by John Koivula. This partially dissolved silk with blue color concentrations is a clear sign that the sapphire was heated.
Natural Sapphire •
Sri Lanka (Ceylon) •
Enhancements:
Heat (H) •
Lighting Conditions:
Diffuse Light Field (Transmitted Light)
Photographer:
E. Billie Hughes •
Image Number:
A-001-3417-1
Koivula, J.I. (1987) Internal diffusion. Journal of Gemmology, Vol. 20, No. 7/8, pp. 474–477; RWHL*.
Hughes, R.W. (1997) Ruby & Sapphire. Boulder, CO, RWH Publishing, 512 pp.; RWHL*.
Search the Complete Hyperion Database
Sapphire inclusions may include mineral crystals, rutile silk, healed fissures, fluid inclusions, negative crystals, color zoning and other features formed during or after crystal growth. Such features are important to gemologists because they can provide evidence useful in identifying sapphire, understanding its geological history, recognizing treatment and, in some cases, determining geographic origin.
Sapphire Inclusion Photomicrographs
The Hyperion sapphire gallery includes microscopic features found in sapphires from major deposits around the world. Each entry is accompanied by descriptive information and, where available, references to the gemological literature.
What Inclusions Can Reveal About Sapphire
Inclusions are an important part of sapphire identification. Their form, composition, orientation and alteration can help gemologists distinguish natural sapphire from synthetic material, recognize evidence of heat treatment, and study the geological environment in which the sapphire formed.
Hyperion combines inclusion photomicrography with supporting gemological information so that individual features can be compared with documented examples from known sapphire deposits.
About Hyperion
Hyperion is the Lotus Gemology searchable inclusion database. It allows users to browse gemstone inclusions by gem type, geographic origin, treatment and keyword.
