
sedimentary
Limestone
Limestone (Calcium Carbonate: CaCO3)
Hardness: 3 on Mohs scale; Color: typically gray, tan, or white; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Rhombohedral (microscopic)
- Hardness
- 3 on Mohs scale
- Color
- typically gray, tan, or white
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically gray, tan, or white; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Rhombohedral (microscopic)
Formation & geological history
Formed in marine environments through the accumulation of shell, coral, algal, and fecal debris. It can also be formed by the chemical precipitation of calcium carbonate from lake or ocean water.
Uses & applications
Used extensively in construction as road base, aggregate, and a key ingredient in cement/concrete. Also used as a soil conditioner and in glass making.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. It is the primary rock found in cavern systems and often contains visible fossils.
Field identification & locations
Can be identified in the field by its softness (easily scratched by a steel nail) and its rapid effervescence (bubbling) when exposed to a drop of dilute hydrochloric acid.
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