Favosites is a genus of extinct tabulate coral characterized by tightly packed polygonal corallites that resemble a honeycomb structure. Collectors typically find these fossils in Paleozoic limestone deposits, often silicified, making them excellent candidates for lapidary work and polishing.
Is this favosites?
4-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch favosites with a known reference. Favosites sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Name the organismDecide what left the fossil before worrying about the rock. Organism: Tabulate coral (genus Favosites). Age: Late Ordovician to Late Permian.
- 3Read the lusterHold the specimen under a strong light. Luster: dull.
- 4Match the color rangeCompare against the expected color range: gray, tan, brown, white, black.
Often confused with
Favosites vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside favosites
Minerals reported to co-occur with favosites. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-4
- Density
- 2.6-2.7 g/cm³
- Luster
- Dull
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Collector, Lapidary, Decorative
- Host rock
- sedimentary limestone
- Organism
- Tabulate coral (genus Favosites)
- Age
- Late Ordovician to Late Permian
Where rockhounds find favosites
3 mapped spotsClassic worldwide localities
- Michigan, USA
- Ontario, Canada
- Gotland, Sweden
- Eifel, Germany
Field-hunting tip
Where it forms: sedimentary limestone. If you start seeing calcite, dolomite, quartz in float, you are in the right ground. In the U.S., the densest reported localities are in Michigan, New York, Wisconsin. Start trip planning there.



