Crinoidal limestone is a sedimentary rock composed primarily of fossilized stem segments and plates from crinoids, ancient echinoderms known as sea lilies. Look for characteristic circular or star-shaped fossil fragments embedded within a calcium carbonate matrix, which are often visible on weathered surfaces or polished slabs. This rock formed in shallow marine environments and is commonly found in geologic strata from the Paleozoic era.
Is this crinoidal limestone?
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 crinoidal limestone with a known reference. Crinoidal Limestone sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Crinoidal Limestone leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Crinoidal Limestone typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, tan, white, brown.
- 5Look at form & habitTypical habit: massive.
Often confused with
Crinoidal Limestone vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside crinoidal limestone
Minerals reported to co-occur with crinoidal limestone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3
- Density
- 2.5-2.7 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Fluorescence
- Often Fluorescent Yellow or White
- Rarity
- Common
- Uses
- Decorative, Construction, Collector
- Host rock
- Marine Sedimentary Deposits
- Typical price
- $5-50 per specimen
Where rockhounds find crinoidal limestone
Classic worldwide localities
- USA
- United Kingdom
- Germany
- Belgium
- France
Field-hunting tip
Look in marine sedimentary deposits country — that is the host setting where crinoidal limestone typically forms. If you start seeing calcite, dolomite, quartz in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.






