
sedimentary
Fossiliferous Limestone
Calcium Carbonate (CaCO3) - Limestone
AI-generated identification · may be incorrectHardness: 3 on Mohs scale. Color: Light beige, tan, grey, or off-white. Luster: Dull, earthy, or crystalline. Texture: Fine-grained matrix containing fossil fragments or shell remnants. Reacts strongly with dilute hydrochloric acid.
- Hardness
- 3 on Mohs scale
- Color
- Light beige, tan, grey, or off-white
- Luster
- Dull, earthy, or crystalline
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Physical properties
Hardness: 3 on Mohs scale. Color: Light beige, tan, grey, or off-white. Luster: Dull, earthy, or crystalline. Texture: Fine-grained matrix containing fossil fragments or shell remnants. Reacts strongly with dilute hydrochloric acid.
Formation & geological history
Formed in shallow, warm marine or coastal environments through the accumulation and cementation of organic remains such as shells, coral fragments, and calcium carbonate precipitates. Often dates from Paleozoic to Cenozoic eras.
Uses & applications
Used in construction, aggregate for road building, production of cement and lime, soil conditioning in agriculture, and as decorative stone or landscaping material.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth. Fossiliferous varieties often contain ancient marine organisms like brachiopods, crinoids, bryozoans, or mollusks preserved in fine detail.
Field identification & locations
Identified by its tan/grey color, soft nature (easily scratched by a copper coin or steel blade), earthy texture, visible fossil/shell fragments, and effervescence with weak acids. Commonly found along coastal areas, ancient lakebeds, and karst landscapes.
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