sedimentary

Crinoid Stem Fragment

Crinoid (Phylum Echinodermata, Class Crinoidea)

AI-generated identification · may be incorrect

Hardness: 3 (Calcite-based); Color: Gray, tan, or white; Luster: Dull to earthy; Crystal structure: Trigonal/Hexagonal (internal crystalline calcite); Cleavage: Perfect rhombohedral in individual ossicles; Specific gravity: Approx 2.7.

Hardness: 3 (Calcite-based)
Color: Gray, tan, or white
Luster: Dull to earthy

Identified March 14, 2026More sedimentary →

Explore Crinoid Stem Fragment in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Formed through the organic accumulation and fossilization of marine arthropod stems. These specimens lived in shallow seas during the Paleozoic era (approx. 250-500 million years ago) and were buried in marine sediments.

Uses & applications

Used primarily in education, fossil collecting, and occasionally as decorative beads in jewelry known as 'St. Cuthbert's beads'. Can also be a component of 'encrinal limestone' used in construction.

Geological facts

Crinoids are known as 'sea lilies' because of their plant-like appearance, but they were actually animals. They are still alive today in deep ocean environments, though they were much more abundant in the prehistoric past.

Field identification & locations

Identify in the field by their cylindrical shape and clear central hole (lumen) or star/circle patterns on the ends. They are commonly found in limestone outcrops, riverbeds, and gravel pits across North America and Europe.