
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Gray, tan, or white; Luster: Dull to earthy; Crystal structure: Trigonal (microcrystalline); Cleavage: None visible in hand samples; Specific gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- Gray, tan, or white
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Gray, tan, or white; Luster: Dull to earthy; Crystal structure: Trigonal (microcrystalline); Cleavage: None visible in hand samples; Specific gravity: 2.5-2.7
Formation & geological history
Formed primarily by the accumulation of shell, coral, algal, and fecal debris in marine environments. It can also form through chemical precipitation from lake or ocean water.
Uses & applications
Used extensively in construction (aggregate, cement), architecture, agriculture (soil treatment), and industrial manufacturing of glass and steel.
Geological facts
Limestone is the primary source of lime and makes up about 10% of the total volume of all sedimentary rocks on Earth. It is famous for containing diverse fossils.
Field identification & locations
Identify in the field by its susceptibility to react (fizz) with dilute hydrochloric acid. It is commonly found in large beds or layers in areas that were once prehistoric sea floors.
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