Rock Identifier
Crinoidal Limestone (Fossiliferous Limestone containing Crinoid stem fragments (Echinodermata)) — fossil
fossil

Crinoidal Limestone

Fossiliferous Limestone containing Crinoid stem fragments (Echinodermata)

Hardness 3-4 (Mohs), Light gray to buff matrix, Dull luster, Effervesces with dilute hydrochloric acid, Contains circular and rod-like fossil inclusions.

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Physical properties

Hardness 3-4 (Mohs), Light gray to buff matrix, Dull luster, Effervesces with dilute hydrochloric acid, Contains circular and rod-like fossil inclusions.

Formation & geological history

Formed in warm, shallow marine environments through the accumulation of calcium carbonate and biological remains during the Paleozoic era (approx. 250-500 million years ago).

Uses & applications

Crushed for aggregate in construction, used in lime production, and highly valued as educational and decorative fossil specimens.

Geological facts

Crinoids are also known as 'sea lilies,' though they are animals related to starfish rather than plants. The disc-shaped sections of their stems are often called 'Indian beads.'

Field identification & locations

Commonly found in riverbeds and limestone outcrops in the Midwest USA (e.g., Ohio, Indiana, Kentucky). Identified by the presence of small, donut-shaped or rectangular fossil segments embedded in the rock.