
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: light gray to tan; Luster: dull to earthy; Crystal structure: Trigonal (microcrystalline); Cleavage: Rhombohedral (rarely visible in fine-grained specimens); Specific Gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- light gray to tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: light gray to tan; Luster: dull to earthy; Crystal structure: Trigonal (microcrystalline); Cleavage: Rhombohedral (rarely visible in fine-grained specimens); Specific Gravity: 2.5-2.7
Formation & geological history
Formed primarily in shallow marine environments from the accumulation of coral, shell, and algal debris over millions of years (primarily Paleozoic and Mesozoic eras). Lithification occurs through compaction and cementation of calcium carbonate.
Uses & applications
Widely used in construction (aggregate, cement production, building stone), agriculture (soil conditioner), and as a chemical feedstock for industrial lime production.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. It is the primary parent rock for Karst landscapes, where water creates caves, sinkholes, and underground rivers.
Field identification & locations
Identify in the field using the 'acid test'—it will effervesce (fizz) when a drop of dilute hydrochloric acid is applied. Look for fine grains, earthy texture, and occasional fossil inclusions. Extremely common globally.
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