
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: typically grey, white, or tan; Luster: dull to earthy; Crystal Structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral; Specific Gravity: 2.5–2.7
- Hardness
- 3 on Mohs scale
- Color
- typically grey, white, or tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically grey, white, or tan; Luster: dull to earthy; Crystal Structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral; Specific Gravity: 2.5–2.7
Formation & geological history
Formed in marine environments through the accumulation of shell, coral, algal, and fecal debris. It can also be formed by the chemical precipitation of calcium carbonate from lake or ocean water.
Uses & applications
Used extensively in construction (as building blocks and aggregate), in the manufacturing of cement, as a soil conditioner in agriculture, and in the production of lime.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. Most caves are formed in limestone when acidic water dissolves the rock over millions of years.
Field identification & locations
Identification includes a fizz test (reaction to dilute hydrochloric acid). Look for fossil remains or a fine-grained, earthy texture. Common in areas with ancient seabeds.
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