
sedimentary
Limestone
Calcium carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: tan, cream, or light grey; Luster: dull to earthy; Texture: fine-grained to clastic; Cleavage: none; Specific Gravity: 2.5-2.7.
- Hardness
- 3 on Mohs scale
- Color
- tan, cream, or light grey
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: tan, cream, or light grey; Luster: dull to earthy; Texture: fine-grained to clastic; Cleavage: none; Specific Gravity: 2.5-2.7.
Formation & geological history
Primarily formed in marine environments through the accumulation of shell, coral, algal, and fecal debris. It can also be formed by the precipitation of calcium carbonate from lake or ocean water.
Uses & applications
Used extensively in construction (aggregate, cement), agriculture (lime to neutralize soil acidity), and as a filler in products like toothpaste, paper, and plastics.
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 easily dissolved by acidic groundwater.
Field identification & locations
Identify in the field by its softness (can be scratched by a copper coin) and its effervescence (bubbles) when a drop of weak acid is applied. Commonly found in areas that were once ancient sea beds.
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