Rock Identifier
Fossil brachiopod or bivalve shell (Likely a ribbed brachiopod, possibly Spiriferida or Productida; exact identification requires locality and shell details) — fossil
fossil

Fossil brachiopod or bivalve shell

Likely a ribbed brachiopod, possibly Spiriferida or Productida; exact identification requires locality and shell details

AI-generated identification · may be incorrect

Fossilized calcitic shell with strong radial ribs, yellow-brown weathering, and dull to waxy luster; calcite hardness about 3, commonly showing cleavage and relatively high density (SG ~2.7).

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Physical properties

Fossilized calcitic shell with strong radial ribs, yellow-brown weathering, and dull to waxy luster; calcite hardness about 3, commonly showing cleavage and relatively high density (SG ~2.7).

Formation & geological history

A marine shell buried in carbonate sediment and mineralized during diagenesis, likely Paleozoic in age (about 541–252 million years ago). The bilateral ribbing and thick, curved form are consistent with a brachiopod, though a bivalve is possible.

Uses & applications

Primarily a teaching, display, and collecting specimen; fossil shells can also be used in educational geology and paleontology exhibits.

Geological facts

Brachiopods resemble clams but have symmetry through each valve rather than between the two valves. Radial ribs strengthened the shell and may have helped stabilize it on the seafloor.

Field identification & locations

Look for repeated ribs, a distinct hinge or beak, shell symmetry, and mineral-filled internal surfaces; acid testing is not recommended unless damage is acceptable. Common in Paleozoic limestone deposits worldwide, especially North America and Europe.