
sedimentary
Limestone
Calcium carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: tan, buff, light brown; Luster: dull, earthy; Texture: fine-grained, microcrystalline to clastic; Cleavage: none (conchoidal to uneven fracture).
- Hardness
- 3 on Mohs scale
- Color
- tan, buff, light brown
- Luster
- dull, earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: tan, buff, light brown; Luster: dull, earthy; Texture: fine-grained, microcrystalline to clastic; Cleavage: none (conchoidal to uneven fracture).
Formation & geological history
Formed primarily in shallow, warm marine environments through the accumulation and compaction of organic debris such as shell fragments, coral, and algal remains, or via chemical precipitation of calcium carbonate.
Uses & applications
Widely used as a construction material, in crushed stone for road bases, as a key component in cement production, and for soil acidity neutralisation in agriculture.
Geological facts
Limestone is highly susceptible to weathering by acidic rainwater, which dissolves the rock over time to create dramatic karst landscapes, including sinkholes, caves, and underground rivers.
Field identification & locations
Identifiable in the field by its soft nature (can be scratched by a steel nail), dull earthy appearance, and a vigorous effervescent reaction when exposed to dilute hydrochloric acid. Commonly found worldwide in ancient sea beds and sedimentary basins.
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