Rock Identifier
Polished fossil shell fragment (likely ammonite or bivalve) (Fossilized mollusk shell; likely aragonite/calcite replaced by silica or iron-rich minerals) — fossil
fossil

Polished fossil shell fragment (likely ammonite or bivalve)

Fossilized mollusk shell; likely aragonite/calcite replaced by silica or iron-rich minerals

AI-generated identification · may be incorrect

Dark brown-black, glossy, smoothly polished, with curved shell-like banding and possible rib or growth structures. Original shell mineral was commonly aragonite or calcite; hardness is approximately 3–7 depending on replacement, with no clearly visible crystal structure.

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Physical properties

Dark brown-black, glossy, smoothly polished, with curved shell-like banding and possible rib or growth structures. Original shell mineral was commonly aragonite or calcite; hardness is approximately 3–7 depending on replacement, with no clearly visible crystal structure.

Formation & geological history

Formed when a marine mollusk shell was buried in sediment and mineralized during diagenesis, typically over millions of years; exact age and identity cannot be confirmed from the image alone.

Uses & applications

Primarily a collectible, jewelry, or ornamental specimen; polished fossil fragments are sometimes mounted as pendants or used in cabochons.

Geological facts

The visible curved layering resembles fossil shell growth lines, though a polished dark agate or mineralized wood fragment is also possible.

Field identification & locations

Look for consistent biological symmetry, growth lines, ribs, chambers, or shell curvature; acid testing is risky and inconclusive on polished material. Comparable fossils occur in marine limestone and shale worldwide.