
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: typically grey, tan, or white; Luster: dull to earthy; Crystal Structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral (when crystalline); Specific Gravity: 2.3 to 2.7.
- Hardness
- 3 on Mohs scale
- Color
- typically grey, tan, or white
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically grey, tan, or white; Luster: dull to earthy; Crystal Structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral (when crystalline); Specific Gravity: 2.3 to 2.7.
Formation & geological history
Formed primarily from the accumulation of shell, coral, algal, and fecal debris in marine environments. It can also form through chemical precipitation from ocean water or cave environments (speleothems). Found in geological ages ranging from Precambrian to Holocene.
Uses & applications
Extensively used in construction as aggregate, road base, and a component of cement. Used in agriculture to neutralize soil acidity, in the chemical industry for steel manufacturing, and occasionally as dimension stone for architecture.
Geological facts
Limestone covers about 10% of the Earth's land surface. Most of the world's most famous caves, such as Mammoth Cave in Kentucky, are carved out of limestone by acidic groundwater. It often contains abundant fossils of ancient marine life.
Field identification & locations
Identify in the field using a 'fizz test'—it reacts vigorously with dilute hydrochloric acid. It often has a gritty texture and may contain visible fossils. Common in areas with ancient sea beds like the Midwestern US, UK, and the Alps.
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