sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: typically white, gray, or tan; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral in calcite crystals, but usually massive; Specific Gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- typically white, gray, or tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically white, gray, or tan; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral in calcite crystals, but usually massive; Specific Gravity: 2.5-2.7
Formation & geological history
Formed primarily in marine environments from the accumulation of shell, coral, algal, and fecal debris. It can also form through chemical precipitation from calcium-rich water in caves or springs.
Uses & applications
Extensively used as a building material, in the manufacturing of cement/concrete, as a soil conditioner in agriculture, and as a flux in steel production.
Geological facts
Limestone provides the base for many of the world's most famous landmarks, including the Great Pyramids of Giza and the Parthenon. It is the primary rock type in karst landscapes, leading to the formation of extensive cave systems.
Field identification & locations
Identify in the field by its effervescence (bubbling) when in contact with dilute hydrochloric acid. It is commonly found in ancient seabed regions and mountain ranges with sedimentary origins.
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