
sedimentary
Limestone
Calcium carbonate rock (CaCO3)
Hardness: 3 on Mohs scale; Color: typically light gray, tan, white, or yellowish; Luster: earthy to sub-vitreous; Crystal structure: microcrystalline or fine-grained; Cleavage: none distinct; Specific gravity: 2.7 - 2.9
- Hardness
- 3 on Mohs scale
- Color
- typically light gray, tan, white, or yellowish
- Luster
- earthy to sub-vitreous
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Physical properties
Hardness: 3 on Mohs scale; Color: typically light gray, tan, white, or yellowish; Luster: earthy to sub-vitreous; Crystal structure: microcrystalline or fine-grained; Cleavage: none distinct; Specific gravity: 2.7 - 2.9
Formation & geological history
Formed through the accumulation of skeletal fragments of marine organisms such as coral, algal, and foraminifera, or through the chemical precipitation of calcium carbonate from water. Deposited in shallow marine environments over millions of years.
Uses & applications
Widely used in construction as building stone, a primary component of Portland cement, crushed stone for road base, agricultural lime to neutralize soil acidity, and in the production of glass and steel.
Geological facts
Limestone is famous for forming spectacular karst landscapes, including underground caves, stalactites, and stalagmites. Many of the world's most famous monuments, including the Great Pyramid of Giza, are built from limestone.
Field identification & locations
Easily identified by its characteristic fizz when a weak acid like vinegar (acetic acid) is applied, due to the release of carbon dioxide gas. Found worldwide in sedimentary basins and ancient sea beds.
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