
sedimentary
Limestone
Calcium Carbonate (CaCO3) / Limestone
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Gray, light brown, tan, off-white; Luster: Dull to earthy; Crystal Structure: Trigonal (calcite matrix); Cleavage: Perfect rhombohedral in calcite grains; Specific Gravity: ~2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- Gray, light brown, tan, off-white
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Gray, light brown, tan, off-white; Luster: Dull to earthy; Crystal Structure: Trigonal (calcite matrix); Cleavage: Perfect rhombohedral in calcite grains; Specific Gravity: ~2.5-2.7
Formation & geological history
Formed predominantly in clear, warm, shallow marine waters through the accumulation and compaction of organic debris such as shell fragments, coral reef material, and chemical precipitation of calcium carbonate over millions of years.
Uses & applications
Extensively used in construction, road base, crushed stone for aggregate, cement and lime production, soil acidity regulation in agriculture, and as a dimension stone in architecture.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks worldwide. Large karst landscapes, complete with caves and sinkholes, are formed by the dissolution of limestone by acidic rainwater.
Field identification & locations
Identified easily in the field by its effervescent reaction (fizzing) when exposed to cold dilute hydrochloric acid or strong household vinegar. Found abundantly in ancient sea beds and sedimentary rock formations worldwide.
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