Rock Identifier
Crinoid Stem Fossil (Crinoid ossicle / stalk segment (Phylum Echinodermata)) — fossil
fossil

Crinoid Stem Fossil

Crinoid ossicle / stalk segment (Phylum Echinodermata)

Hardness: 3 (calcite); Color: Varies from tan, grey, brown to white; Luster: Vitreous to dull; Crystal structure: Trigonal (calcite composition); Cleavage: Perfect rhombohedral; Specific gravity: 2.71

Hardness
3 (calcite)
Color
Varies from tan, grey, brown to white
Luster
Vitreous to dull
Identified More fossil
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Physical properties

Hardness: 3 (calcite); Color: Varies from tan, grey, brown to white; Luster: Vitreous to dull; Crystal structure: Trigonal (calcite composition); Cleavage: Perfect rhombohedral; Specific gravity: 2.71

Formation & geological history

Formed from marine organisms known as crinoids (sea lilies) that lived in shallow oceans, primarily during the Paleozoic era (especially Mississippian and Pennsylvanian periods, roughly 350-300 million years ago), where their skeletal segments accumulated in limestone-forming deposits.

Uses & applications

Collected by fossil enthusiasts, used in educational displays, and sometimes cut into lapidary jewelry or ornamental items.

Geological facts

Crinoids are animals, not plants, despite their common name 'sea lilies'. Their segmented stems often break apart after death, leaving behind disc-like fossil fragments commonly referred to by collectors as 'Indian beads' or 'screw stones'.

Field identification & locations

Easily identified by their characteristic round, oval, or star-shaped segments with a central hole or canal. Frequently found weathered out of limestone or shale riverbeds and road cuts worldwide.