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Crinoid Fossil in Limestone
Crinoidea (class) in Fossiliferous Limestone
Hardness: 3-4 (matrix), color: tan, grey, and reddish-brown, luster: dull/earthy, structure: circular/columnar segments (ossicles), cleavage: rhombohedral in calcite crystals.
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Physical properties
Hardness: 3-4 (matrix), color: tan, grey, and reddish-brown, luster: dull/earthy, structure: circular/columnar segments (ossicles), cleavage: rhombohedral in calcite crystals.
Formation & geological history
Formed in shallow marine environments where crinoids (sea lilies) lived on the ocean floor. The segmented stems disintegrated and were buried in calcium carbonate mud, typically during the Paleozoic era (approx. 250-500 million years ago).
Uses & applications
Educational specimens, fossil collecting, decorative stones, and scientific research into paleo-environments.
Geological facts
Crinoids are nicknamed 'sea lilies' because of their plant-like appearance, but they are actually echinoderms, related to starfish and sea urchins. In some cultures, the disc-shaped stem segments are known as 'fairy stones' or 'St. Cuthbert\'s beads'.
Field identification & locations
Look for small, stacked circular or star-shaped discs embedded in a sedimentary matrix. Commonly found in areas with exposed Paleozoic limestone, such as the Midwestern United States, parts of Europe, and North Africa.
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