
sedimentary
Limestone
Limestone (Calcium Carbonate, CaCO3)
Hardness: 3 on the Mohs scale. Color: Varies widely, commonly white, gray, tan, or yellowish. Luster: Earthy to dull. Crystal structure: Microcrystalline or granular calcite. Cleavage: Good rhombohedral cleavage in pure crystals. Specific gravity: 2.7 to 2.9.
- Hardness
- 3 on the Mohs scale
- Color
- Varies widely, commonly white, gray, tan, or yellowish
- Luster
- Earthy to dull
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Physical properties
Hardness: 3 on the Mohs scale. Color: Varies widely, commonly white, gray, tan, or yellowish. Luster: Earthy to dull. Crystal structure: Microcrystalline or granular calcite. Cleavage: Good rhombohedral cleavage in pure crystals. Specific gravity: 2.7 to 2.9.
Formation & geological history
Forms mainly in clear, warm, shallow marine waters through the accumulation of shell, coral, algal, and fecal debris, or through the chemical precipitation of calcium carbonate from water.
Uses & applications
Widely used in the construction industry as crushed stone for road base, aggregate in concrete, and as a primary raw material for manufacturing Portland cement and lime.
Geological facts
Limestone often contains fossils of ancient marine organisms since it forms in water bodies. Famous structures like the Great Pyramid of Giza were built largely using limestone blocks.
Field identification & locations
Can be easily identified in the field by applying a drop of dilute hydrochloric acid, which will cause it to fizz vigorously due to the release of carbon dioxide gas. Found globally in sedimentary basins.
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