Rock Identifier
Crinoid Stem Fossil (Crinoid ossicle (phylum Echinodermata)) — fossil
fossil

Crinoid Stem Fossil

Crinoid ossicle (phylum Echinodermata)

Hardness: 3 on Mohs scale (calcite). Color: Varies from white, grey, to tan or brownish. Luster: Vitreous to dull. Crystal structure: Trigonal (composed of single calcite crystals). Cleavage: Perfect rhombohedral cleavage.

Hardness
3 on Mohs scale (calcite)
Color
Varies from white, grey, to tan or brownish
Luster
Vitreous to dull
Identified More fossil
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Physical properties

Hardness: 3 on Mohs scale (calcite). Color: Varies from white, grey, to tan or brownish. Luster: Vitreous to dull. Crystal structure: Trigonal (composed of single calcite crystals). Cleavage: Perfect rhombohedral cleavage.

Formation & geological history

Formed during the Paleozoic era (particularly Mississippian and Pennsylvanian periods) when crinoids, marine animals related to starfish and sea urchins, lived in ancient shallow seas. After death, their segmented stems broke apart and were preserved in sedimentary limestone deposits.

Uses & applications

Used in fossil collecting, educational displays, and occasionally lapidary work or jewelry making when polished.

Geological facts

Crinoids are commonly known as 'sea lilies' because of their flower-like appearance. In some cultures, fossilized crinoid stems were known as 'St. Cuthbert's beads' or fairy money.

Field identification & locations

Easily identified by their circular or pentagonal shape with a central hole or star pattern. Found globally in limestone and shale formations rich in marine fossils.