
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on the Mohs scale; Color: typically white, gray, or tan; Luster: dull to earthy; Structure: non-crystalline or clastic (contains fossil fragments); Specific gravity: 2.3 to 2.7.
- Hardness
- 3 on the Mohs scale
- Color
- typically white, gray, or tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on the Mohs scale; Color: typically white, gray, or tan; Luster: dull to earthy; Structure: non-crystalline or clastic (contains fossil fragments); Specific gravity: 2.3 to 2.7.
Formation & geological history
Formed in marine environments from 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
Primary source of lime for cement; used in road construction, building materials, and as an agricultural soil conditioner.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. Many famous structures, including the Great Pyramids of Giza, were built using limestone.
Field identification & locations
Identifiable in the field by its tendency to fizz (effervesce) when a drop of diluted hydrochloric acid is applied. It is commonly found in areas that were once prehistoric seafloors.
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