
sedimentary
Orthoceras Fossil Limestone
Orthoceras (extinct genus of cephalopod); Limestone matrix (CaCO3)
AI-generated identification · may be incorrectHardness: 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
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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.
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