
sedimentary
Fossiliferous limestone
Calcitic limestone, predominantly CaCO₃ (often containing fossilized coral or shell fragments)
AI-generated identification · may be incorrectUsually gray to buff, dull to weakly crystalline, with visible porous fossil textures; Mohs hardness 3, non-cleaved, specific gravity about 2.3–2.7. Calcite-rich surfaces fizz vigorously with dilute hydrochloric acid.
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Physical properties
Usually gray to buff, dull to weakly crystalline, with visible porous fossil textures; Mohs hardness 3, non-cleaved, specific gravity about 2.3–2.7. Calcite-rich surfaces fizz vigorously with dilute hydrochloric acid.
Formation & geological history
Forms in shallow marine environments from accumulated carbonate mud, shells, and reef organisms, commonly during Paleozoic–Cenozoic time. The prominent structure appears consistent with a fossil fragment, possibly coral, embedded in the limestone.
Uses & applications
Used for cement, aggregate, lime, building stone, and architectural slabs; attractive fossil-bearing pieces are collected or used decoratively. Generally low commercial value unless fossils are exceptionally preserved or legally collectible.
Geological facts
Limestone fossils may preserve coral colonies, brachiopods, crinoids, or mollusks; recrystallization can obscure original detail. The specimen appears naturally weathered rather than polished or manufactured.
Field identification & locations
Identify by gray carbonate matrix, fossil outlines, and acid effervescence; common in ancient marine sedimentary basins worldwide, including Europe, North America, and the Middle East. Avoid acid testing on valuable specimens and check collecting restrictions.
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