
sedimentary
Petoskey Stone
Hexagonaria percarinata (Fossilized Rugose Coral)
Hardness: 3.0-3.5 (Mohs scale); Color: Gray to tan when dry, distinct hexagonal patterns visible when wet; Luster: Dull to earthy (natural), vitreous (polished); Structure: Colonial coral hexagonal cells; Composition: Calcite (CaCO3).
- Hardness
- 3
- Luster
- Dull to earthy (natural), vitreous (polished)
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Physical properties
Hardness: 3.0-3.5 (Mohs scale); Color: Gray to tan when dry, distinct hexagonal patterns visible when wet; Luster: Dull to earthy (natural), vitreous (polished); Structure: Colonial coral hexagonal cells; Composition: Calcite (CaCO3).
Formation & geological history
Formed during the Devonian Period (approximately 350 million years ago) in warm, shallow saltwater seas. Over millions of years, the coral colonies were buried and fossilized through the replacement of organic matter with calcite, then later moved by glacial action.
Uses & applications
Predominantly used for jewelry making (pendants, beads), lapidary art, home decor, and as a popular souvenir or collector's item in the Great Lakes region.
Geological facts
It is the official state stone of Michigan. The name 'Petoskey' comes from the Ottawa Chief Pet-O-Sega, meaning 'rising sun' or 'rays of hope.' The hexagonal patterns are the former skeletons of individual coral polyps.
Field identification & locations
Identify in the field by looking for 'stones with eyes' along shorelines. They are easiest to spot when wet, as the hexagonal pattern disappears when the stone is dry. Found predominantly on the beaches of Lake Michigan and Lake Huron.
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