Rock Identifier
Orthoceras Fossil Limestone (Orthoceras (extinct genus of cephalopod); Limestone matrix (CaCO3)) — sedimentary
sedimentary

Orthoceras Fossil Limestone

Orthoceras (extinct genus of cephalopod); Limestone matrix (CaCO3)

Hardness: 3-4 (Mohs); Color: Black or dark grey matrix with white to light-grey fossils; Luster: Polished/Vitreous; Structure: Massive limestone containing fossilized internal molds; Specific Gravity: Approx 2.7

Hardness
3-4 (Mohs)
Color
Black or dark grey matrix with white to light-grey fossils
Luster
Polished/Vitreous
Identified More sedimentary

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Physical properties

Hardness: 3-4 (Mohs); Color: Black or dark grey matrix with white to light-grey fossils; Luster: Polished/Vitreous; Structure: Massive limestone containing fossilized internal molds; Specific Gravity: Approx 2.7

Formation & geological history

Formed in marine environments during the Ordovician period (approx. 400-500 million years ago). The soft-bodied cephalopods died and their shells were buried in seafloor sediment, eventually mineralizing into calcite or aragonite within limestone.

Uses & applications

Primarily used for decorative items, jewelry (cabochons), paperweights, and educational fossil specimens. In some regions, large slabs are used for architectural tiling.

Geological facts

Orthoceras means 'straight horn,' referring to the characteristic long, conical shell. They are ancestors of the modern squid and lived in the seas long before the first dinosaurs appeared.

Field identification & locations

Identified by the distinct white, cone-shaped or bullet-shaped inclusions against a dark background, often showing internal chambers (septa). Most commercial specimens originate from the Atlas Mountains in Morocco.