
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Tan, beige, or grey; Luster: Dull to earthy; Crystal structure: Trigonal (microcrystalline); Cleavage: None in rock form; Specific Gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, or grey
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, or grey; Luster: Dull to earthy; Crystal structure: Trigonal (microcrystalline); Cleavage: None in rock form; Specific Gravity: 2.5-2.7
Formation & geological history
Formed in clear, warm, shallow marine waters from the accumulation of shell, coral, algal, and fecal debris. It can also form chemically through the precipitation of calcium carbonate from lake or ocean water.
Uses & applications
Used primarily in construction (crushed stone, cement), as an architectural material, in glass making, and for soil treatment in agriculture.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth. It is the primary stone used in the construction of the Great Pyramids of Giza.
Field identification & locations
Identify in the field by applying a drop of dilute hydrochloric acid; it will effervesce (fizz) vigorously. It is commonly found in regions that were once ancient sea beds, such as the Midwestern United States and Central Europe.
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