
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Gray, tan, or beige; Luster: Dull to earthy; Structure: Often contains visible fossil fragments or tiny shells; Cleavage: None; Specific Gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- Gray, tan, or beige
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Gray, tan, or beige; Luster: Dull to earthy; Structure: Often contains visible fossil fragments or tiny shells; Cleavage: None; Specific Gravity: 2.5-2.7
Formation & geological history
Formed in marine environments through the accumulation of shell, coral, algal, and fecal debris. It can also form via precipitation from calcium-rich water in caves or springs.
Uses & applications
Extensively used in construction as an aggregate, in the manufacture of cement, and as a soil conditioner in agriculture. Pure forms are used in the chemical and glass industries.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth. It is the primary material found in many famous caves and karst landscapes.
Field identification & locations
Identify in the field by its light color and the 'fizz' test: it will bubble when a drop of diluted hydrochloric acid or white vinegar is applied. Commonly found in areas that were once prehistoric seafloors.
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