
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on the Mohs scale; Color: White, gray, tan, yellow, or brown; Luster: Dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Perfect in three directions (for pure calcite); Specific gravity: 2.7 to 2.9
- Hardness
- 3 on the Mohs scale
- Color
- White, gray, tan, yellow, or brown
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on the Mohs scale; Color: White, gray, tan, yellow, or brown; Luster: Dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Perfect in three directions (for pure calcite); Specific gravity: 2.7 to 2.9
Formation & geological history
Formed through the accumulation of skeletal fragments from marine organisms such as coral, mollusks, 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 the construction industry for crushed stone in road base, production of Portland cement, as a building dimension stone, in agriculture to neutralize acidic soils, and as a chemical feedstock.
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 constructed largely from limestone blocks.
Field identification & locations
Can be easily identified in the field by its characteristic reaction to dilute hydrochloric acid, producing effervescence (fizzing) due to the release of carbon dioxide gas. Found worldwide in sedimentary basins and ancient sea beds.
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