
sedimentary
Petoskey Stone
Hexagonaria percarinata
AI-generated identification · may be incorrectHardness: 3-3.5 on Mohs scale; Color: Gray and beige with distinctive hexagonal patterns; Luster: Matte to waxy (pearly when wet or polished); Crystal Structure: Orthorhombic (fossilized calcite); Cleavage: Perfect rhombohedral; Specific Gravity: 2.7
- Hardness
- 3-3
- Color
- Gray and beige with distinctive hexagonal patterns
- Luster
- Matte to waxy (pearly when wet or polished)
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Physical properties
Hardness: 3-3.5 on Mohs scale; Color: Gray and beige with distinctive hexagonal patterns; Luster: Matte to waxy (pearly when wet or polished); Crystal Structure: Orthorhombic (fossilized calcite); Cleavage: Perfect rhombohedral; Specific Gravity: 2.7
Formation & geological history
Formed by fossilization of ancient colonial rugose coral (Hexagonaria) during the Devonian period, roughly 350 million years ago, in shallow warm seas that once covered Michigan. Glaciation later spread these stones across the region.
Uses & applications
Used primarily in jewelry making (pendants, rings), decorative lapidary arts, and highly sought after by rocky hobbyists and fossil collectors.
Geological facts
It is the state stone of Michigan. The unique 'eye' pattern only appears clearly when the stone is wet or polished because the dry fossilized coral cells are often indistinguishable from the matrix.
Field identification & locations
Identify in the field by looking for the honeycomb or hexagonal pattern on rocks near shorelines, especially after rain or when wet. Most commonly found on the beaches of Lake Michigan and Lake Huron.
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