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Petoskey Stone

Fossilized Coral (Sedimentary Rock)

Fossilized Hexagonaria percarinata coral (calcite)

Also known as: Michigan's State Stone

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Description

The Petoskey Stone is a fossilized colonial coral characterized by its distinctive hexagonal patterns, which are the cross-sections of the individual coral polyps (corallites). Each hexagon typically has a dark central 'eye' (the former mouth of the polyp) and radiating septa (skeletal partitions) that extend to the hexagonal wall. The color ranges from light gray to dark brown, often with contrasting patterns when wet or polished. It is composed primarily of calcite, making it relatively soft and easily polished.

How to Identify

Color
Typically gray to tan, sometimes brownish, with darker hexagonal patterns. The contrast becomes more pronounced when wet or polished.
Luster
Dull to earthy in its natural, unpolished state; vitreous (glassy) when polished.
Texture
Rough and porous when unpolished; smooth and cool to the touch when polished.
Crystal Form
Not a true crystal in the mineralogical sense, but rather a fossilized biological structure. The hexagonal patterns are the key identifying feature.
Cleavage
As a fossilized coral composed of calcite, it exhibits the characteristic rhombohedral cleavage of calcite, though this is rarely observed in the macroscopic fossil structure.
Geological Environment
Found in glacial till, gravel pits, and along the shores of lakes (especially Lake Michigan and Lake Huron) in Michigan, derived from Devonian-age limestones.

Key Facts

  • Hardness: 3 on the Mohs scale (due to calcite composition).
  • Specific Gravity: 2.71 (typical for calcite).
  • Crystal System: Trigonal (for the constituent calcite mineral). The fossil itself is amorphous in terms of crystal system.
  • Color: Gray, tan, brown, often with contrasting hexagonal patterns.
  • Luster: Dull to earthy (unpolished), Vitreous (polished).
  • Transparency: Opaque.
  • Fracture: Conchoidal to uneven (typical for calcite).
  • Cleavage: Perfect rhombohedral (for the constituent calcite mineral).
  • Composition: Calcium carbonate (CaCO3), primarily calcite.

Quick Check

  • Color: Gray to tan with darker hexagonal patterns.
  • Luster: Dull (unpolished), Vitreous (polished).
  • Streak: White (due to calcite composition).

Physical Characteristics

  • Crystal Habit: Not applicable for the fossil itself; the constituent calcite forms rhombohedral crystals, but these are microscopic within the fossil.
  • Cleavage Type: Perfect rhombohedral (for calcite).
  • Fracture Type: Conchoidal to uneven.
  • Tenacity: Brittle.
  • Luster Type: Dull to earthy (unpolished), Vitreous (polished).

Formation

The Petoskey Stone is a fossilized rugose coral, specifically Hexagonaria percarinata. These corals lived in warm, shallow, marine environments during the Devonian Period. When the corals died, their calcium carbonate skeletons were buried by sediments. Over millions of years, these sediments lithified into limestone, and the coral skeletons were preserved through a process of permineralization and replacement, primarily by calcite. Glacial activity during the Pleistocene Epoch subsequently eroded and transported these fossil-bearing limestones, depositing them in the northern Lower Peninsula of Michigan and surrounding areas.

Usage

Primarily used as a lapidary material for cabochons, spheres, carvings, and polished decorative items. It is also collected as a geological specimen and is a popular souvenir in Michigan.

Age Distribution

Devonian Period (approximately 350-400 million years old)

Where to Find

Lake Michigan Shorelines

Especially prevalent along the beaches of Lake Michigan in the northern Lower Peninsula of Michigan, particularly near Petoskey, Charlevoix, and Traverse City.

Lake Huron Shorelines

Can also be found along the shores of Lake Huron, though generally less common than on Lake Michigan.

Gravel Pits and Road Cuts

Occurs in glacial outwash and till deposits throughout the northern Lower Peninsula of Michigan.

Finding Tips

Search after storms

Storms and strong wave action can churn up the lake bottom and expose new stones on the beaches.

Look in shallow water

The patterns are often more visible when the stone is wet, making shallow water an ideal place to spot them.

Visit public beaches

Many public beaches in northern Michigan are excellent places to search, but be aware of local regulations regarding collection limits.

Bring a spray bottle

If searching on dry land, a spray bottle of water can help reveal the characteristic patterns.

Similar Rocks

Charlevoix Stone

Favosites spp.

Also known as: Favosites coral

Honeycomb Coral

Favosites spp.

Also known as: Favosites spp.

Chain Coral

Halysites spp.

Also known as: Halysites coral

Scientific Classification

Mineral Class
Carbonates (for calcite)
Group
Fossilized Rugose Coral
Crystal System
Trigonal (for calcite)
Chemical Formula
CaCO3 (for calcite)
Composition
Calcium carbonate

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