Rock Identifier
Synthetic opal cabochon/bead (Opal-like hydrated amorphous silica; likely lab-created polymer–silica opal or Gilson synthetic opal (SiO₂·nH₂O)) — gemstone
gemstone

Synthetic opal cabochon/bead

Opal-like hydrated amorphous silica; likely lab-created polymer–silica opal or Gilson synthetic opal (SiO₂·nH₂O)

AI-generated identification · may be incorrect

Vivid blue-green body color with patchy play-of-color and a smooth polished surface; opal is amorphous, non-cleaving, Mohs hardness 5.5–6.5, vitreous-to-resinous luster, and specific gravity about 1.98–2.20. The unusually uniform cylindrical form and intense pattern strongly suggest synthetic rather than natural opal.

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Physical properties

Vivid blue-green body color with patchy play-of-color and a smooth polished surface; opal is amorphous, non-cleaving, Mohs hardness 5.5–6.5, vitreous-to-resinous luster, and specific gravity about 1.98–2.20. The unusually uniform cylindrical form and intense pattern strongly suggest synthetic rather than natural opal.

Formation & geological history

Natural opal forms when silica-rich groundwater deposits hydrated silica in cavities and fractures, commonly in volcanic rocks, over millions of years. Synthetic opal is manufactured by arranging silica spheres and binding them into a stable gem material.

Uses & applications

Used in jewelry, beads, cabochons, and decorative objects; synthetic material is generally inexpensive and durable enough for occasional wear.

Geological facts

Play-of-color results from diffraction of light by regularly spaced microscopic silica structures. Natural blue-green opal can occur in Australia, Ethiopia, Mexico, and Nevada, while synthetic opal is widely produced commercially.

Field identification & locations

Check for a drilled bead opening, perfectly regular color pattern, and a plastic-like feel; magnification may reveal a honeycomb or columnar pattern typical of synthetic opal. Avoid prolonged heat, chemicals, and ultrasonic cleaning.