
sedimentary
Fossiliferous Limestone (Crinoidal)
Bioclastic Limestone (predominantly CaCO3)
AI-generated identification · may be incorrectHardness: 3-4 (Mohs scale), Color: Dirty white to dark gray with brown weathering, Luster: Dull/Earthy, Crystal Structure: Microcrystalline matrix with visible calcite fossil inclusions, Cleavage: None (conchoidal to irregular fracture)
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Physical properties
Hardness: 3-4 (Mohs scale), Color: Dirty white to dark gray with brown weathering, Luster: Dull/Earthy, Crystal Structure: Microcrystalline matrix with visible calcite fossil inclusions, Cleavage: None (conchoidal to irregular fracture)
Formation & geological history
Formed in shallow, high-energy marine environments where skeletal debris (likely crinoid stems or shell fragments) accumulated on the sea floor and were lithified over millions of years, commonly from the Paleozoic era.
Uses & applications
Used primarily in the aggregate industry for road base, cement production, or as decorative garden stones. Larger, polished slabs are used for architectural cladding.
Geological facts
This specimen contains 'hash' fossils, which are fragmented remains of ancient marine organisms. These rocks often serve as a biological 'time capsule' for ancient reef systems that existed hundreds of millions of years ago.
Field identification & locations
Identify in the field by checking for the presence of visible shell or stem fragments and performing an acid test (it will fizz when in contact with diluted HCl or vinegar). Found globally in areas with exposed sedimentary bedrock.
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