How to identify Pearl
Biogenic (calcium carbonate)
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Open the appTo correctly identify Pearl (Biogenic (calcium carbonate)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Typically white, cream, pink, silver, gold, green, blue, or black. The color is influenced by the type of mollusk and its environment.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Pearly (nacreous), often with an iridescent sheen known as 'orient'.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth, often slightly gritty when rubbed against the teeth (a traditional, though not recommended, test for authenticity).
- 4
Crystal Form
Shape of visible crystals or crystal faces
Concentric layers of microscopic aragonite (or calcite) crystals, typically hexagonal platelets, cemented by an organic matrix (conchiolin). Not a true crystal form in the mineralogical sense.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, as it is an aggregate of microscopic crystals.
- 6
Geological Environment
The rock formation and setting where it occurs
Formed within the mantle tissue of marine or freshwater mollusks (bivalves and gastropods). Natural pearls are found in wild mollusks, while cultured pearls are farmed in mollusk aquaculture operations.
Key Facts
- Hardness
- 2.5-4.5 on the Mohs scale (due to aragonite/calcite and organic matrix)
- Specific Gravity
- 2.60-2.85 (varies with composition and origin)
- Crystal System
- Orthorhombic (aragonite) or Trigonal (calcite) - refers to the constituent mineral phases, not the pearl as a whole.
- Color
- White, cream, pink, silver, gold, green, blue, black, and various overtones.
- Luster
- Pearly (nacreous)
- Transparency
- Opaque to translucent
- Fracture
- Conchoidal to uneven (due to layered structure)
- Cleavage
- None (as an aggregate)
- Composition
- Calcium carbonate (CaCO3) in the form of aragonite and/or calcite, with an organic binder (conchiolin) and water.
Physical characteristics
- Crystal Habit: Concentric layers of microscopic aragonite (or calcite) platelets, typically hexagonal, embedded in an organic matrix. Forms spherical, oval, button, drop, baroque, or ring shapes.
- Cleavage Type: None
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Pearly (nacreous)
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