Rock Identifier
Fossil shell fragment (Likely a fossilized bivalve or brachiopod valve; exact identification requires the other valve, locality, and matrix) — fossil
fossil

Fossil shell fragment

Likely a fossilized bivalve or brachiopod valve; exact identification requires the other valve, locality, and matrix

AI-generated identification · may be incorrect

White to cream, ribbed shell form with preserved radial ornamentation; likely calcite (CaCO₃), Mohs hardness about 3, pearly to dull luster, and strong cleavage in calcite. The apparent dark background is likely a display surface rather than matrix.

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Physical properties

White to cream, ribbed shell form with preserved radial ornamentation; likely calcite (CaCO₃), Mohs hardness about 3, pearly to dull luster, and strong cleavage in calcite. The apparent dark background is likely a display surface rather than matrix.

Formation & geological history

A marine shell was buried and mineralized during diagenesis, potentially replacing or preserving the original calcium-carbonate shell. Geological age cannot be determined from the image alone; fossil shells range from Paleozoic to Recent.

Uses & applications

Primarily a collector or educational specimen; fossil shell material is not generally used for construction or jewelry unless polished or set decoratively.

Geological facts

The ribbed, asymmetric shape may indicate a brachiopod, while shell curvature and ornament could indicate a bivalve. White coloration commonly reflects recrystallized calcite or aragonite alteration.

Field identification & locations

Identify it by hinge structure, symmetry, growth lines, and whether ribs radiate from a beak or umbo; locality and associated rock are essential. Common fossil-shell sources include marine sedimentary rocks worldwide.