
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3-4 (Mohs scale); Color: White, gray, tan; Luster: Dull to earthy; Crystal structure: Trigonal (microscopic); Cleavage: Perfect rhombohedral in calcite; Specific gravity: 2.5-2.7
- Hardness
- 3-4 (Mohs scale)
- Color
- White, gray, tan
- Luster
- Dull to earthy
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Physical properties
Hardness: 3-4 (Mohs scale); Color: White, gray, tan; Luster: Dull to earthy; Crystal structure: Trigonal (microscopic); Cleavage: Perfect rhombohedral in calcite; Specific gravity: 2.5-2.7
Formation & geological history
Formed through the accumulation of shell, coral, algal, and fecal debris in clear, warm, shallow marine waters. Can also form organically through the precipitation of calcium carbonate from lake or ocean water.
Uses & applications
Used primarily in construction for building stone, aggregate for roads, and as a raw material for cement/lime. Also used in agriculture to neutralize soil acidity.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. Most of the world's caves are formed in limestone because it is soluble in weak acidic solutions like rainwater.
Field identification & locations
Can be identified by a 'fizz test' (effervescence) when a small amount of dilute hydrochloric acid or strong vinegar is applied. Commonly found in areas that were once prehistoric seafloors.
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