A crinoid stem is a fossilized segment of a marine echinoderm, usually found as a stackable, wheel-like disc in limestone. It is identified by its central pentagonal or circular hole and is a staple find for amateur paleontologists in Paleozoic marine strata.
Is this crinoid stem?
5-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 crinoid stem with a known reference. Crinoid Stem sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Crinoid Stem leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Crinoid Stem typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, white, tan, brown.
- 5Look at form & habitTypical habit: cylindrical segments.
Often found alongside crinoid stem
Minerals reported to co-occur with crinoid stem. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCO₃
- Mohs hardness
- 3-4
- Density
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Cylindrical Segments
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Decorative, Educational
- Host rock
- Limestone
Where rockhounds find crinoid stem
3 mapped spotsClassic worldwide localities
- Indiana, USA
- Ohio, USA
- United Kingdom
- Germany
- Missouri, USA
Field-hunting tip
Look in limestone country, the host setting where crinoid stem typically forms. If you start seeing calcite, brachiopods, bryozoans in float, you are in the right ground. Field specimens usually show a cylindrical segments habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Texas, Michigan. Start trip planning there.

