Table of Contents
- What is a Petoskey Stone?
- Coral Terminology
- Devonian Period
- Devonian Mass Extinctions
- How Coral Turns into Limestone
- Michigan on the Move
- Quaternary Ice Coverage
- Scientific Classification
- Michigan Hexagonaria Species
- Stratigraphy
- Hexagonaria alpenensis
- Hexagonaria anna
- Hexagonaria attenuata
- Hexagonaria cristata
- Hexagonaria fusiformis
- Hexagonaria potterensis
- Hexagonaria profunda
- Hexagonaria subcarinata
- Hexagonaria percarinata
- Gravel Point Formation
- Worldwide Hexagonaria
On February 28, 2022, I presented a pared-down version of this research on the Petoskey Stone, Michigan’s state stone, to the Ozark Mountain Gem & Mineral Society. During my research, I discovered that much of the information available—whether online, in books, or even in magazines—was inaccurate or inconsistent. Determined to separate fact from fiction, I spent four months analyzing sources, cross-referencing data, and compiling the most reliable information into one comprehensive resource.
What is a Petoskey Stone?
Fossilized Colonial Rugose Coral
A Petoskey Stone is a fossilized colony of rugose coral, an extinct group of corals that thrived during the Devonian Period. These corals, which once lived in Michigan’s ancient tropical seas, are now preserved in limestone deposits, their hexagonal patterns making them instantly recognizable.
Understanding Corals and Rugose Corals
Corals are marine invertebrates that have existed from the Ordovician Period (about 485 million years ago) to today, with a 14-million-year gap during the Triassic. They are simple organisms consisting of a polyp, a hollow, cylindrical sac anchored to the seafloor, with a mouth surrounded by tentacles. Unlike more complex animals, coral lack a central nervous system and internal organs. Instead, they extract calcium carbonate (CaCO₃) from seawater to build external skeletons for protection.
Rugose (“Wrinkled”) Corals
- Existed from the Ordovician to the Permian.
- Lived as solitary individuals or in colonial formations.
- Individual corallites (skeleton cups housing polyps) remained small, but entire colonies could grow several feet across.
- Likely had stinging tentacles used to capture prey, similar to modern reef-building corals.
Did Rugose Corals Have Symbiotic Algae?
Scientists debate whether rugose corals had a symbiotic relationship with algae. Unlike tabulate corals, which were primary reef-builders, rugose corals played a more minor role in reef formation. In modern corals, this relationship works as follows:
- The coral provides a home for algae.
- The algae perform photosynthesis using the coral’s waste products.
- This process produces oxygen and carbohydrates, benefiting the coral.
Corals are susceptible to temperature—not because they can’t survive in cold water, but because the algae can’t. Most reef-forming corals require temperatures between 73°–84°F (23°–29°C) and clear water for sunlight penetration. Some corals, like those in deeper, colder waters, have adapted to life without algae, but this is a slow evolutionary process.
Coral Terminology
Understanding the structure of rugose corals, including the Petoskey Stone, requires familiarity with key anatomical terms. Below is a breakdown of essential coral features:
- Polyp: The living coral animal, consisting of a soft body, mouth, tentacles, and gullet. Since polyps are made of soft tissue, they do not fossilize.
- Corallite: The skeletal cup secreted by the polyp, where it lived and could retract for protection.
- Calyx, calice (pl. calyxes, calices): The central part of the corallite where the polyp resided.
- Columella: The center of the calyx, where the septa intertwine or form a dome-like or pillar-like structure.
- Septum (pl. septa): Radiating support plates within the calyx that provide structural integrity.
- Tabula (pl. tabulae): As the polyp aged, it continuously deposited calcium carbonate, raising the walls. When buried under sediment, it built floor-like layers beneath itself to keep growing.
- Dissepiment: Curved support plates that connect the septa and tabulae, enhancing vertical stability.
- Carina (pl. carinae): A vertical bar found on the septa.
Devonian Period
Laurussia: The Devonian Supercontinent
During the Devonian Period (419–359 million years ago), North America, Greenland, and Europe were part of a massive supercontinent called Laurussia, located along the equator and surrounded by warm, shallow seas. The area that is now Michigan’s Lower Peninsula was completely submerged under these tropical waters.
Evolution of Terrestrial Life
The Devonian was a time of dramatic biological advancements, marking the transition of life from water to land:
- The first trees emerged, growing up to 10 meters (33 feet) tall.
- Early tetrapods (four-legged vertebrates) began to venture onto land.
- The first terrestrial arthropods, such as ancient insects and millipedes, made their appearance.
Marine Life & Reef Formation
Devonian oceans were teeming with diverse marine life, including:
- A rapid expansion of fish, ranging from jawless armored species to the first lobe-finned fish, the ancestors of modern amphibians.
- Corals and sponges formed the first extensive reef systems, which played a crucial role in:
- Protecting coastlines from 97% of wave action, reducing erosion.
- Providing habitats and shelter for a variety of marine species.
Devonian Mass Extinctions
Mass extinctions have shaped life on Earth, with five significant events being the most catastrophic. These occurred at the end of the Ordovician, Devonian, Permian, Triassic, and Cretaceous periods. Each was triggered by dramatic atmospheric chemistry and climate shifts, wiping out vast numbers of species.
The Devonian Extinctions: A Slow Crisis
Unlike some mass extinctions that happened abruptly, the Devonian Period (419–359 million years ago) experienced a series of extinctions over millions of years. These events eliminated 70-80% of all animal species, making it the smallest of the “Big Five” but still devastating—particularly for marine life. One of these extinctions nearly wiped out all coral species between the Middle and Upper Devonian.
What Caused the Devonian Extinctions?
Geologists have identified a layer of black shale in Devonian rock formations, indicating that low-oxygen environments played a key role in these extinctions. The most widely accepted theory links these events to the evolution of deep-rooted land plants, drastically altering Earth’s climate and ecosystems.
Step-by-Step Process of Environmental Collapse
Expansion of Deep-Rooted Plants
- The rise of large, vascular plants accelerated silicate weathering and soil formation.
Runoff and Carbon Sequestration
- As nutrients and carbonates washed from the land into rivers and seas, carbon was trapped in sediments instead of being recycled into the atmosphere.
- This led to a drop in atmospheric CO₂, cooling global temperatures.
Algal Blooms & Oxygen Depletion
- Excess nutrients fueled massive algal blooms.
- These algae blocked sunlight in deeper waters and, upon decaying, consumed oxygen, creating dead zones.
Coral Bleaching & Ecosystem Collapse
- Cooler temperatures and reduced sunlight disrupted coral-algae symbiosis.
- Corals expelled their symbiotic algae (zooxanthellae), a process known as bleaching.
- While some corals can adapt to cooler conditions, oxygen depletion was too rapid for survival.
How Coral Turns into Limestone
When a coral colony dies, it becomes buried beneath layers of sediment on the seafloor. The calyx (skeletal cup) fills with sediment as the soft polyp tissue decays. Over time, additional layers of sediment, marine debris, and calcium carbonate accumulate, compacting under pressure.
This process, known as lithification, gradually cements the coral skeletons and other marine remains, transforming them into limestone. This is how Petoskey Stones—fossilized rugose corals—formed over millions of years in what is now Michigan.
Michigan on the Move
Tectonic Plate Movement
Earth’s outer layer, the crust, is divided into 15 to 20 tectonic plates, which rest atop the partially molten mantle. These plates are constantly in motion, shifting between 2 to 15 centimeters per year due to radioactive processes within Earth’s interior. Their movement drives earthquakes, volcanic activity, and mountain formation:
- When plates slide past each other, they generate earthquakes.
- When plates collide, one plate may subduct beneath the other, forming mountain ranges.
Tracking Michigan’s Ancient Location
Geologists reconstruct the movement of tectonic plates using paleomagnetic data, which records the ancient positions of rocks. Scientists can determine when these landmasses were once connected by comparing matching rock formations on separate continents. Additionally, the continental shapes fit together like puzzle pieces, further supporting plate movement over time.
Michigan’s Journey Through Time
- Middle Devonian (~385 million years ago) – Michigan was located south of the equator, submerged beneath a warm, tropical sea.
- Late Carboniferous (~300 million years ago) – The seas retreated, exposing Michigan as a swampy, semi-tropical jungle. Trees in these ancient wetlands were buried over time, forming coal deposits.
- Permian (~280 million years ago) – All landmasses merged into the supercontinent Pangea. Michigan was far inland, preventing further marine fossilization.
- Permian to Quaternary (~280 to 2.6 million years ago) – Michigan remained above sea level, limiting fossil preservation due to erosion. This is why few fossils exist from this period, apart from some spore fossils.
Quaternary Ice Coverage
During the Quaternary Period (2.6 million years ago), Michigan was entirely covered by ice during all four major North American glaciations. These glaciers dramatically reshaped the landscape, leaving behind today’s geologic features.
How Glaciers Shaped Michigan
Ice Advance and Erosion
- As glaciers advanced, they picked up debris and acted like giant sandpaper sheets, scouring the land.
- This process eroded bedrock, smoothed landscapes, and carved out deep basins.
Ice Retreat and Deposition
- When the ice retreated, it left a glacial till, a mix of sand, gravel, clay, and boulders.
- This debris filled some areas, creating rolling hills and plains while leaving other regions with exposed bedrock.
Formation of Lakes and Landforms
- The glaciers excavated depressions, which later were filled with water and became the Great Lakes and other smaller lakes.
- The thickness of glacial till varies across Michigan:
- Thinner along coastlines, where bedrock is closer to the surface.
- Thicker in the interior, forming moraines and drumlins.
Scientific Classification
Like many fossils, the Petoskey Stone has undergone multiple taxonomic reclassifications as scientists have improved their understanding of its structure. Over time, researchers have refined its classification based on diagnostic features observed in Michigan specimens.
Historical Taxonomic Changes
1866 – Newton Horace Winchell
- Acervularia davidsoni (based on the 1855 work of Henri Milne-Edwards and Jules Haime).
1876 – Carl Ludwig Rominger
- Reclassified as Cyathophyllum davidsoni after determining that Acervularia required a central portion of polyp cells surrounded by an internal wall, which Michigan specimens lacked.
1935 – William Dickson Lang & Stanley Smith
- Reassigned from Cyathophyllum davidsoni to Prismatophyllum davidsoni, introducing new diagnostic criteria to differentiate Michigan specimens.
1939 – Laurence L. Sloss
- Renamed Prismatophyllum percarinatum, distinguishing it from P. davidsoni (France), which lacked carinae (ridge structures).
1970 – Erwin C. Stumm
- Hexagonaria percarinata – The most widely accepted modern classification.
Michigan Hexagonaria Species
Erwin C. Stumm’s Contributions
Dr. Erwin C. Stumm was a Professor of Geology and Curator of Paleozoic Invertebrates at the University of Michigan, widely regarded as a leading expert on Devonian invertebrate fossils. His research was prolific, with 56 published papers and his name cited in over 5,947 scholarly references.
One of his most significant works, Corals of the Traverse Group of Michigan, was a 13-part series (1949–1969) documenting the Devonian coral fauna of northern Michigan. Unfortunately, Stumm passed away before completing the entire series—his final contribution, Part 13: Hexagonaria, was published just 15 days before his death.
Hexagonaria Species in Michigan
In his research, Stumm identified nine distinct species of Hexagonaria from fossil specimens previously collected by Laurence L. Sloss and G.M. Ehlers. Each species is associated with specific Devonian rock formations in Michigan:
- Hexagonaria alpenensis: Alpena Limestone
- Hexagonaria anna: Bell Shale, upper Ferron Point Formation
- Hexagonaria attenuata: Alpena Limestone, Four Mile Dam Formation, Charlevoix Limestone
- Hexagonaria cristata: Gravel Point Formation
- Hexagonaria fusiformis: Genshaw Formation
- Hexagonaria percarinata: Gravel Point Formation
- Hexagonaria potterensis: Potter Farm Formation, Thunder Bay Limestone
- Hexagonaria profunda: one specimen from Petoskey Limestone
- Hexagonaria subcarinata: Alpena Limestone
Additionally, Stumm provided a chart of eight diagnostic characteristics used to differentiate these species.
Stratigraphy
What is Stratigraphy?
Stratigraphy is the branch of geology that studies rock layers’ order, relative position, and age (strata). Geologists can classify mappable rock units by examining rock sequences and determining their geologic timeframes.
The Michigan Basin
Michigan’s Lower Peninsula is centered on a large geologic basin known as the Michigan Basin. This bowl-shaped depression is deepest in the center and rises toward the coasts, explaining why older rock layers are more exposed along Michigan’s shorelines than in its interior.
Hexagonaria & Devonian Strata
Fossilized Hexagonaria corals (including the Petoskey Stone) are only found in situ (in their original rock layers) within the Traverse Group and Bell Shale formations in northern Michigan.
While other Middle Devonian rock layers exist throughout the state, including around Detroit, Hexagonaria fossils are only present in formations north of central Michigan.
Traverse Group Formations
The Traverse Group, which contains many of Michigan’s Devonian coral fossils, consists of over 20 formations and is divided into three geographic regions:
- Northwestern Region – Emmet & Charlevoix Counties
- North Central Region – Afton to Onaway
- Northeastern Region – Presque Isle & Alpena Counties
Hexagonaria alpenensis
Formation & Location
- Formation: Alpena Limestone
- Region: Northeast Lower Peninsula, Michigan
Description
- Found in Alpena Limestone, which consists of white, light gray, or light brown rock with many bioherms (reef-like structures).
- Displays extreme compositional variability compared to other Hexagonaria species.
- The smallest species of Hexagonaria identified in Michigan.
Hexagonaria anna
Formation & Location
- Formations:
- Bell Shale
- Rockport Quarry Limestone
- Ferron Point Formation
- Region: Northeast Lower Peninsula, Michigan
- Additional Occurrences: Found near Antwerp, Ohio
Formation Descriptions
- Bell Shale (BS) – Gray-blue, fossiliferous clay shale, soft and readily disintegrating.
- Rockport Quarry Limestone (RQL) – Gray to brown limestone, sublithographic, with yellow calcite specks.
- Ferron Point Formation (FPF) – Greenish-gray clay, forming a densely packed surface.
Hexagonaria attenuata
Formation & Location
- Formations & Regions:
- Alpena Limestone – Northeast Lower Peninsula, Michigan
- Four Mile Dam Formation – Northeast Lower Peninsula, Michigan
- Charlevoix Limestone – Northwest Lower Peninsula, Michigan
- Key Exposure Sites:
- Kegomic Quarry Syncline – Located at the eastern limit of Emmet County in the Bear Creek Valley, where the Petoskey Formation is exposed above the Charlevoix Limestone at Bay View.
- Only Hexagonaria species found on both coasts of Michigan’s Lower Peninsula.
Formation Descriptions
- Alpena Limestone (AL) – White, light gray, or light brown, highly variable composition with numerous bioherms (reef-like structures).
- Four Mile Dam Formation (FMD) – Brownish-gray limestone, interbedded with sandy shale partings.
- Charlevoix Limestone (CL) – Found in northwestern Michigan, prominently exposed in the Kegomic Quarry Syncline.
Distinctive Features
Similar to Hexagonaria subcarinata, but with:
- Longer major septa
- Smaller corallites
- Lack of a distinct boundary between the dissepimentarium and tabularium in transverse section
Hexagonaria cristata
Formation & Location
- Formation: Gravel Point Formation
- Region: Northwest Lower Peninsula, Michigan
- Primary Exposure Site: Little Traverse Bay
Formation Characteristics
- Found within a 10–15 ft limestone interval between the lower and upper blue shales.
- Associated with the Gravel Point Formation, which is known for well-preserved Devonian marine fossils.
Distinctive Features
Largest species of Hexagonaria identified in Michigan.
Hexagonaria fusiformis
Formation & Location
Formations & Region:
- Genshaw Formation – Northeast Lower Peninsula, Michigan
- Ferron Point Formation – Northeast Lower Peninsula, Michigan
- Newton Creek Limestone – Northeast Lower Peninsula, Michigan
Formation Descriptions
- Genshaw Formation (GF) – Gray to light brown limestone, occasionally containing small bioherms (reef-like structures).
- Ferron Point Formation (FPF) – Greenish-gray clay, forming a densely packed surface.
- Newton Creek Limestone (NCL) – Dark brown crystalline limestone.
Distinctive Features
Similar to Hexagonaria anna, but differs by:
- Longer rhopaloid major septa
- More distinctly zigzag corallite walls
Hexagonaria potterensis
Formation & Location
- Formations & Region:
- Potter Farm Formation – Northeast Lower Peninsula, Michigan
- Thunder Bay Limestone – Northeast Lower Peninsula, Michigan
- Key Exposure Site:
- Thunder Bay Limestone is exposed at or just below water level at Partridge Point.
Formation Descriptions
- Potter Farm Formation (PFF) – Brownish-gray limestone with sandy shale partings.
- Thunder Bay Limestone (TBL) – Bluish, argillaceous limestone that weathers to rusty brown.
Distinctive Features
Calyx walls are intermediate between Hexagonaria percarinata and Hexagonaria profunda.
Hexagonaria profunda
Formation & Location
- Formation: Petoskey Limestone
- Region: Northwest Lower Peninsula, Michigan
- Key Exposure Site: Kegomic Quarry
Formation Description
- Petoskey Limestone (PL) – Gray, shalelike limestone.
- Only one specimen of H. profunda has been found in Michigan.
- Identical to specimens from the Cedar Valley Limestone in Iowa.
Distinctive Features
Extremely rare in Michigan, making it unlikely to be encountered in the state.
Hexagonaria subcarinata
Formation & Location
- Formation: Alpena Limestone
- Region: Northeast Lower Peninsula, Michigan
Formation Description
- Alpena Limestone consists of white, light gray, or light brown rock, often containing numerous bioherms (reef-like structures).
- Highly variable composition compared to other Devonian formations.
Distinctive Features
Very similar to Hexagonaria percarinata, but:
- Lacks abundant carinae (ridge-like structures).
- Less likely to be found embedded in shale.
Hexagonaria percarinata
Formation & Location
- Formation: Gravel Point Formation
- Region: Northwest Lower Peninsula, Michigan
- Key Exposure Site: Little Traverse Bay
Formation Description
Found in Gravel Point Formation, composed of brownish-gray limestone with sandy shale interbeds.
Distinctive Features
Most common species of Hexagonaria in Michigan.
Can be distinguished from other species by:
- A false inner wall created by the crowding of dissepiments and carinae at the axial ends of the minor septa.
- Being much more heavily carinate compared to other Hexagonaria species.
Gravel Point Formation
Location & Exposure
- Region: Northwest Lower Peninsula, Michigan
- Key Exposure Site: Bay Harbor, Petoskey, Michigan
Formation Description
- Gravel Point Formation is a Devonian limestone formation known for its fossil-rich deposits, particularly Hexagonaria percarinata.
- The formation is prominently exposed behind Bay Harbor in Petoskey, Michigan, where rock strata can be observed.
Worldwide Hexagonaria
Global Distribution
- Over 70 species of Hexagonaria have been identified in 31 locations worldwide.
- Some species may have undergone reclassification due to advances in taxonomy.
Known Hexagonaria Species
(Note: This list may include synonyms or reclassified taxa)
adarensis
allani
amanshauseri
anna
approximans
arctica
basaltiformis
bassleri
bella
bompasi
bongbutensis
bouchardi
capitolium
caurus
cincta
curta
davidsoni
densa
firthi
fisherae
flexum
gamboni
hexagona
hypocrateriforme
inequalis
isylica
jurkowicensis
kirki
kuznetskiensis
lavali
laxa
longiseptata
mae
magna
marmini
meeki
meoualis
minuta
mirabilis
mireillae
occidens
orientalis
ovoidea
oweni
pachytheca
palmera
parallaxa
partita
parvula
pentagona
percarinata
philomena
playfordi
ponderosa
prisma
quadrigemina
reedi
rohrensis
sanctacrucensis
schucherti
septaforminalis
soraufi
stenotabulata
stewartae
subcarinata
tabulata
taurensis
truncata
tungkanlingensis
tuqiaoziensis
whitfieldi
yakovlevi
- North America:
- Alaska, Alberta, Arizona, Indiana, Iowa, Kentucky, Manitoba, Michigan, New Mexico, New York, Northwest Territories, Nunavut, Ohio, Ontario, Yukon
- Europe:
- Belgium, France, Germany, Poland, Spain, United Kingdom
- Asia & Middle East:
- Afghanistan, China, Iran, Kazakhstan, Tajikistan, Vietnam
- Oceania:
- Australia, New Zealand
- Africa:
- Morocco
- Russia & Former Soviet Regions:
- Russian Federation
Where to Look in Michigan
All of the previous information about where to find Hexagonaria in situ is correct, but people rarely take the time to dig them out of the ground. It’s much easier to go to a lower peninsula rocky beach, find them scattered in gravel throughout the state, or look through glacial moraines.
People have found Petoskey Stones at pretty much every lower peninsula rocky beach in the state. The best places to look are around Little Traverse Bay, but Grand Traverse Bay, Leelanau Peninsula, and Roger’s City to Alpena are also great locations. The reason for this is the Great Lakes didn’t exist when the coral formed. The formations that contain these fossils continue out into the lakes, primarily in the shallower bays. Waves bring the rocks into shore all the time, though the best time to look is in the spring after breakup or after a storm.
NOTE: There is a 25-lb weight limit per year on taking rocks from any State land in Michigan, including State parks and Lakes. The National Parks (Sleeping Bear Dunes, Pictured Rocks, and Isle Royale) are off-limits to rock collecting.
Northern Michigan was the one of the largest producers of limestone in the world and still has the single largest limestone quarry in the world (Calcite in Roger’s City). In 1978, Michigan had 31 limestone quarries in northern Michigan and the eastern half of the U.P. Limestone has a variety of uses including road and building constructions and for making cement. Northern Michigan has a lot of gravel roads, which were primarily supplied with local stone.
When the glaciers receded, Devonian fossils ended up all over the state in glacial till.
Origins of the Name
Legend says the Petoskey Stone was named after a great Ottawa chief, Pet-O-Sega, whose name meant “Rising Sun,” “Rays of Dawn,” or “Sunbeams of Promise.”
It more likely came about because it’s found in the Petoskey area and people were selling them as souvenirs, though it’s possible someone was savvy enough in marketing to associate the name with the stone. I find it unlikely that whomever first named it did so completely independent of any knowledge of how the city was named.
Petoskey was named after Biidassige (Light that is Coming), an Odawa fur trader and businessman born in 1787. His anglicized name was Ignatius Petoskey (also Neyas Petosega).
Bear River/Creek (Mukwa Ziibing) was a small Odawa fishing village for centuries. In 1836, Petoskey and his sons purchased 440-acres of land where the Bear River meets Lake Michigan. At the time, Michigan Native Americans were purchasing back land they had just sold to the Federal Government in the Treaty of Washington (1836). The Treaty ensured they would have permanent hunting and fishing rights, education, money, and services, but Congress altered the terms of the treaty to only five years. The Native Americans thought that by purchasing back the land, they would have the same rights as whites and could not be forcibly removed to west of the Mississippi River.
In 1852, a Presbyterian Mission was established in Bear River when a minister arrived with a deed to 80 acres of the 440. Warren Petoskey, the great-great-grandson of Ignatius Petoskey, wrote in his book, Dancing the Dream, that when Michigan became a State, Petoskey did not know he was required to pay taxes on the land. The State sold the land to the Presbyterian Church for back taxes. Petoskey did not contest the loss because he was afraid to draw the attention of the government and potentially have the Native Americans forcibly removed to Kansas.
In 1855, the Odawa entered into another treaty with the U.S. Government, The Treaty of Detroit (1855). This time, the Native Americans would be given 40-80-acre plots of land within specific townships. These areas were reserved for the Natives for 10-years and they could not sell or transfer the allotment. Exemptions were made for missions, churches, schools, and settlers already living in the areas. After the 10-years were up, Michigan could begin selling the leftover land and the titles were issued to the Native landowners.
According to Harriet Kilborn in an essay she wrote on The History of Petoskey Area, Petoskey and his sons added to the 360-acres they still had with allotted plots from the Treaty of 1855 and by the time the land was open for purchase, they owned most of downtown Bear River.
In 1873, the Grand Rapids and Indiana Railroad added a stop in Bear River. This brought an influx of people to the area. Dr. William Little applied for a post office and the job of postmaster, and asked for the town to be renamed Petoskey in Ignatius Petoskey’s honor.
Petoskey and his sons lost most of the lands. He died in 1885 and still has descendants living in the area today. His granddaughter, Ella Jane Petoskey, was a signatory to Act 89 of 1965 naming the Petoskey Stone the state stone of Michigan.
So, What is a Petoskey Stone?
Petoskey Stone is a colloquial, nickname, or marketing name for Hexagonaria found in Michigan.
Some people insist it must be found in northern Michigan, but glaciers dragged them all over the state (and Midwest) and the plethora of limestone quarries provided ample gravel to fill all of the gravel roads in the state.
Others insist only H. percarinata is a true Petoskey Stone. As far as I can tell, Laurence Sloss first identified which species of Hexagonaria is known as the Petoskey Stone in his doctoral dissertation to the University of Chicago in 1937 when he wrote “Prismatophyllum percarinatum is the coral of the familiar ‘Petoskey stone’ of northern Michigan.” It’s obvious from what he wrote that Petoskey Stones were already a well-known souvenir at least through the Great Lakes region since Sloss was from California and attending school in Illinois.
I don’t know whether or not Petoskey Stones were being collected and sold outside of Petoskey in 1937 or whether or not all of the Hexagonaria species were being sold as Petoskey Stones at the time. But, they are now. Souvenir shops throughout the state sell Petoskey Stones. People collect them from both Lake Michigan and Lake Huron (or wherever they happen to find them in the state) and sell them online as Petoskey Stones. Most people don’t know there are multiple species. If they do, they probably don’t know how to tell the difference between them or they don’t have the scientific equipment necessary to prepare and examine them.
Plus, most of the ones you find on the Lakes are coming from bedrock under the water, not the formations listed above. As far as I can tell, there has not been a geological undertaking to determine which species of Hexagonaria are in the Lake bedrock. Nor has there been a thorough examination of rocks found on different beaches to determine their species.
I’ve seen people argue online about whether a rock is a “true” Petoskey Stone. They state you can only find it in the Gravel Point Formation and then mention their “true” one was found on a beach around Leelanau. The Gravel Point Formation is not exposed in Leelanau and Erwin Stumm was very specific in his Corals of the Traverse Group of Michigan, Part 13 that you can only find H. percarinata in the Gravel Point Formation along Little Traverse Bay (emphasis is mine).
I’ve had someone tell me you can’t even find Petoskey Stones in Petoskey, they are just called that because the “Rising Sun” meaning behind the name works so well for the coral. They were irrationally dedicated to their belief that only “true” Petoskey Stones are ones found in their area.
I’ve heard others proclaim that they have an H. percarinata and it’s the “true” Petoskey Stone. When I asked them how they know it’s an H. percarinata and not an H. subcarinata, they had no idea how to tell me the difference.
I think any Hexagonaria found in the Great Lakes region could be called a Petoskey Stone. Let’s stop fighting among ourselves over what is a “true” Petoskey Stone. Leave the species designations to the paleontologists. Only call it an H. percarinata if you have examined a slice of it with a microscope, or pulled it straight out of exposed Gravel Point Formation along Little Traverse Bay, and can honestly tell what species of coral it is. Otherwise, it’s a Petoskey Stone.
Visual Identification
Limestone is normally white, but Petoskey Stones took on gray and brown tones from crude oil in their environment. The “eyes” filled with mud and silt, making them darker than the corallite skeletons.
Ones found along the coasts are usually smooth and contoured like a bar of soap. Most Petoskey Stones are pebble to fist-sized, with egg-sized being average. When dry, it looks like regular limestone, but when wet, the hexagon pattern starts to stand out.
Petoskey Stones found in the interior tend not to be as worn down. You can see the coral structure much better. Sometimes you will even find ones with the stem still attached, called a mushroom cap.
Occasionally you will find the tabula structure on the “top” of the stone as if the coral grew sideways or it will be mixed with other fossils.
Color Variations
Petoskey Stones can also be a variety of colors depending on what was present when it formed. The only way to know for sure is to use x-ray fluorescence, but the leading theory is that iron causes most of it.
- Ferric oxide (Fe2O3) = red, orange, or yellow (hematite, limonite)
- Ferrosoferric (Fe3O4) oxide = blue (magnetite)
- Mixture of ferrosoferric oxide with large amount of ferric oxide = purple
- Mixture of ferrosoferric oxide with small amount of ferric oxide = green
- Ferrous oxide (FeO) = colorless, will dilute color when mixed with other types (wüstite)
Other potential causes could be copper (blue-green), nickel (blue), low-oxygen sediments (blue-gray), or manganese (purple).
You will often see coral in other locations that was fossilized through silicification. This is where silica minerals replace the calcium carbonate in the skeleton. Silica better preserves the coral structure and allows for easy extraction of the fossil from other materials because silica is much harder than calcium carbonate and doesn’t dissolve in acids.
Petoskey Stones are rarely silicified. When they are, it happens after the original fossilization and the silica obscures rather than enhances the coral structure.
How to Spot a Fake
Petoskey Stone is a well-known marketing name for fossilized coral. You will find that people often sell their coral fossil as Petoskey Stone when it is not Hexagonaria from northern Michigan. While dishonest (or uninformed), that doesn’t mean the coral fossil is not a real fossil or that it isn’t as pretty, or good, or interesting as a Petoskey Stone. It just means it’s not Hexagonaria from northern Michigan.
Please see this guide on how to tell the difference between Petoskey Stones and other types of Devonian coral found in Michigan and other types of Rugose corals.
Coral fossils from Morocco are frequently misidentified as Petoskey Stones. While there has been a recorded find of Hexagonaria in Aferdoiu el Mrakib, Morocco, I have not been able to find an image of one.
One of the most frequent Moroccan coral fossils sold is Lonsdaleia. The way you can tell the difference between Lonsdaleia and Hexagonaria is the septa on Lonsdaleia do not go all the way to the corallite walls. Instead they stop at the edge of the calyx and there is a large zone of bubbly dissepiments between the calyx and corallite walls.
Acrocyathus is very similar to Lonsdaleia, except it has the lens-like columella. Acrocyathus can be found in the Mississippian Bayport Limestone in Michigan.
Indonesian agatized coral is a type of silicified Scleractinia. It is normally pink or yellow and is sometimes heated to produce more vivid colors. It’s also known as Chrysanthemum Coral. Of the two I have here, neither were marketed as a Petoskey Stone.
These last items are not stone at all. These are “Petoskey Stones” made out of polymer clay and are marketed that way. I just thought they were truly amazing and wanted to show them off to others.
How to Clean and Polish
You can clean Petoskey Stones with a soft-bristled toothbrush and vinegar. Be careful! Too much time in vinegar can destroy the fossil. Be sure to wash all of the vinegar off or use baking soda to neutralize it.
Petoskey Stones sand very easily, but they are very porous and often have spots that are difficult to polish. Sometimes you can work past it, sometimes, it’s just best to live with the defect.
I use a grinder to smooth out cracks and divots, then hand sand with 60-10,000 grit sandpaper. Spend a lot of time on the coarser grits and you will start seeing a shine by 3,000 grit at the latest. If not, go back down a few steps and start over. Doing this will not require soaking them or baking them in mineral oil.
You can tumble Petoskey Stones, but I have not gotten good results with it. I like to tumble them for a stage or two and then switch to hand sanding. This saves me the hard work of the coarser grits.
Here are some suggestions on how to tumble Petoskey Stones with notes from me:
- Start with 320 or 500 silicon carbide & a thickening agent to make a slurry (syrup, sugar, or molasses) – I use guar gum because I don’t want to deal with the sticky mess
- Use 600 or 800 silicon carbide with a ratio of 1 / 1 or 2 / 1 media (walnut shells or corn cob) to Petoskey Stones – I use cut up neoprene foam
- If you used 600 silicon carbide, follow with 600 aluminum oxide and media; otherwise jump to polishing stage
- Use cerium oxide or 0.5-0.8 micron aluminum oxide mixed with media and thickener
Please don’t coat them with epoxy, spray them with polyurethane or paint them with nail polish (unless it’s part of an art project). With a little time and attention, they can look so much better.
Conclusion
If you have any questions or comments, post them below or send me a message through the contact form.
Acknowledgments
I would like to thank the following for their assistance, either in providing knowledge, or selling me books/rocks for this presentation.
- 2020mountionc-27
- Ancient Michigan
- Anybook Ltd
- Asa Asa, Missouri Fossil Hunters
- BackToOurRootsCo
- beesal
- Better World Books
- bookintime
- brandoshilt
- broken_and_branded
- callistodesigns
- Camp Retriever
- Crystalman’s
- dinomite-rocks
- Down2Earth66
- Fossil Age Minerals
- Fossil Era
- FossilsByJosef
- gjo.uk.rhsoha
- GrandDadRocks
- GrauppsCabochons
- JonesMineralCabinet
- KraftByKara
- LakeshoreStonesLLC
- LittleLinkShop
- Little Traverse Bay Bands of Odawa Indians
- Mark Hettich
- MichiganGem
- michigan-rocks
- midwestshoresco
- MorianMiner
- Ozark Mountain Gem & Mineral Society
- The Fossil Forum
- PlanetGems
- The Polkadots
- Prettyfossilsnthings
- pr0teusunbound
- QuartzQueenTreasures
- RockCityByWill
- RocksforSocks
- Rocky Mountain Textbooks
- SaltyPetuniaVoyages
- SegerRockShop
- selltotheworld
- shh!actnatural
- Silver Trees Books
- spencer58
- SpottedWoodchuck
- SteveCabbingDesigns
- ukge-silvergeo
- VintagePennyLane
- Whitehorsewoodworks
References
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Last Updated on 17 January 2025 by Angel Doran