
sedimentary
Honeycomb Coral Fossil
Favosites (extinct genus of tabulate coral)
Hardness: 3-4 (calcite) to 7 (if silicified); Color: Tan, gray, or brown; Luster: Dull to waxy; Structure: Polygonal or hexagonal 'cells' (corallites) resembling a honeycomb; Composition: Calcium carbonate or Silica replacement.
- Hardness
- 3-4 (calcite) to 7 (if silicified)
- Color
- Tan, gray, or brown
- Luster
- Dull to waxy
Identified More sedimentary →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 3-4 (calcite) to 7 (if silicified); Color: Tan, gray, or brown; Luster: Dull to waxy; Structure: Polygonal or hexagonal 'cells' (corallites) resembling a honeycomb; Composition: Calcium carbonate or Silica replacement.
Formation & geological history
Formed in warm, shallow marine environments during the Ordivician to Devonian periods (approx. 488 to 359 million years ago). These corals grew in massive colonies on ancient reefs.
Uses & applications
Decorative display pieces, educational geological specimens, jewelry (when silicified/petrified), and used as biological indicators to date surrounding rock strata.
Geological facts
Favosites are known as 'tabulate' corals because their tubes are divided by horizontal plates called tabulae. They were major reef builders before the Permian mass extinction wiped them out.
Field identification & locations
Look for the distinct 'honeycomb' pattern of small holes or tubes. Found globally in areas with ancient seabed exposure, such as the Great Lakes region (USA) and diverse limestone outcrops. Collectors should look for specimens with well-defined hexagonal walls.
More like this
Other sedimentary specimens
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Sandstone
Arenite (primarily SiO2)
sedimentary
Shale or Slaty Mudstone
Argillaceous sedimentary rock
sedimentary
Chert Breccia
Brecciated Chert (Microcrystalline Silica)
sedimentary
Sandstone (Quartz-rich)
Arenite (SiO2)
sedimentary
Sandstone (with man-made markings)
Arenite (composed primarily of Quartz, SiO2)
sedimentary