Rock Identifier
Pearl (Biogenic calcium carbonate; mainly aragonite (CaCO₃), sometimes calcite, in nacre) — gemstone
gemstone

Pearl

Biogenic calcium carbonate; mainly aragonite (CaCO₃), sometimes calcite, in nacre

AI-generated identification · may be incorrect

Small rounded cream-white bead with pearly luster, likely a cultured freshwater pearl. Mohs hardness about 2.5–4.5; nacreous layered structure, no cleavage, specific gravity about 2.60–2.85. The surface appears smooth and reflective, with a possible drill hole or dimple.

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Physical properties

Small rounded cream-white bead with pearly luster, likely a cultured freshwater pearl. Mohs hardness about 2.5–4.5; nacreous layered structure, no cleavage, specific gravity about 2.60–2.85. The surface appears smooth and reflective, with a possible drill hole or dimple.

Formation & geological history

Formed by a mollusk depositing concentric nacre layers around an irritant; most jewelry pearls are cultured. Freshwater pearls commonly form in mussels, while marine pearls form in oysters. The image alone cannot establish age or species.

Uses & applications

Used primarily in jewelry and ornamentation. Value depends on luster, nacre quality, shape, size, surface blemishes, color, and whether it is natural, cultured, or imitation.

Geological facts

Pearls are biogenic gemstones rather than rocks in the strict petrological sense, but they qualify here as geological specimens. They should not be exposed to acids, perfumes, heat, or prolonged dryness.

Field identification & locations

The warm cream color and rounded form are consistent with a cultured pearl, but a bead of glass, plastic, or shell-coated material is also possible. Check for a drill hole, nacre layering, tooth feel (slightly gritty, not glassy), and X-ray testing for confirmation. Sabah’s region supports pearl aquaculture, but origin cannot be determined visually.