
sedimentary
Limestone
Calcium carbonate (CaCO3) / Limestone
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Tan, beige, off-white to yellowish-brown; Luster: Dull to earthy; Texture: Fine-grained, porous, microcrystalline matrix; Specific Gravity: 2.5-2.7.
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, off-white to yellowish-brown
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, off-white to yellowish-brown; Luster: Dull to earthy; Texture: Fine-grained, porous, microcrystalline matrix; Specific Gravity: 2.5-2.7.
Formation & geological history
Formed primarily in shallow, warm marine environments by the accumulation and compaction of organic debris such as shell fragments, coral, and calcium carbonate precipitates over millions of years.
Uses & applications
Widely used in construction as building stone, crushed aggregate for concrete and roads, manufacture of cement, soil conditioner in agriculture, and neutralizer in chemical processes.
Geological facts
Limestone reacts strongly with dilute hydrochloric acid, producing carbon dioxide gas bubbles (effervescence), which is the primary field test used by geologists to identify it.
Field identification & locations
Can be identified in the field by its light tan/grey color, soft surface that can be scratched by steel, earthy texture, and effervescent reaction to acid. Commonly found in karst landscapes, quarries, and exposed sedimentary rock layers worldwide.
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