
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3-4 on Mohs scale; Color: typically gray, tan, or white; Luster: dull to earthy; Structure: fine-grained to clastic; Cleavage: none (fractures); Specific Gravity: 2.5-2.7
- Hardness
- 3-4 on Mohs scale
- Color
- typically gray, tan, or white
- Luster
- dull to earthy
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Physical properties
Hardness: 3-4 on Mohs scale; Color: typically gray, tan, or white; Luster: dull to earthy; Structure: fine-grained to clastic; Cleavage: none (fractures); Specific Gravity: 2.5-2.7
Formation & geological history
Formed in marine environments from the accumulation of shell, coral, algal, and fecal debris. It can also form via chemical precipitation from ocean water or groundwater. Most deposits range from the Paleozoic to Cenozoic eras.
Uses & applications
Extensively used as a building material, in the manufacture of cement, as an aggregate for road bases, in agricultural lime to neutralize soil acidity, and as a flux in steel making.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. It is the primary reservoir for most of the world\'s karst topography including vast cave systems.
Field identification & locations
Identify in the field by its reaction (fizzing) with cold dilute hydrochloric acid. Commonly found in areas that were once prehistoric seabeds. Collectors look for fossiliferous limestone containing shells or crinoids.
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