
sedimentary
Fossiliferous Limestone
Autochthonous Biogenic Sedimentary Rock (CaCO3)
AI-generated identification · may be incorrectHardness: 3 (Mohs scale); Color: Cream, tan, or grey; Luster: Dull/Earthy; Structure: Clastic or crystalline matrix containing visible brachiopod or bivalve imprints; Cleavage: None (conchoidal to uneven fracture).
- Hardness
- 3 (Mohs scale)
- Color
- Cream, tan, or grey
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3 (Mohs scale); Color: Cream, tan, or grey; Luster: Dull/Earthy; Structure: Clastic or crystalline matrix containing visible brachiopod or bivalve imprints; Cleavage: None (conchoidal to uneven fracture).
Formation & geological history
Formed in shallow marine environments from the accumulation of calcium carbonate shells and skeletal fragments. Most specimens date from the Paleozoic or Mesozoic eras.
Uses & applications
Used in the production of cement, as a building stone (dimension stone), in agriculture to neutralize soil acidity, and as common collector specimens for amateur paleontologists.
Geological facts
This specimen contains clear impressions of prehistoric marine life, likely brachiopods. Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth.
Field identification & locations
Identify in the field by searching for visible shell fragments or imprints; it will effervesce (fizz) strongly when exposed to dilute hydrochloric acid or vinegar. Common in regions with ancient seabed outcrops.
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