Rock Identifier
Fossiliferous Limestone (Autochthonous Biogenic Sedimentary Rock (CaCO3)) — sedimentary
sedimentary

Fossiliferous Limestone

Autochthonous Biogenic Sedimentary Rock (CaCO3)

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).

Hardness
3 (Mohs scale)
Color
Cream, tan, or grey
Luster
Dull/Earthy
Identified More sedimentary
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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.