
sedimentary
Limestone
Sedimentary Rock (Primarily CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Grey, white, or tan; Luster: Earthy to dull; Crystal Structure: Microcrystalline; Cleavage: None distinct (conchoidal fracture); Specific Gravity: 2.7
- Hardness
- 3 on Mohs scale
- Color
- Grey, white, or tan
- Luster
- Earthy to dull
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Physical properties
Hardness: 3 on Mohs scale; Color: Grey, white, or tan; Luster: Earthy to dull; Crystal Structure: Microcrystalline; Cleavage: None distinct (conchoidal fracture); Specific Gravity: 2.7
Formation & geological history
Formed through the accumulation and compaction of organic remains such as shells, coral, and algal debris, or through the chemical precipitation of calcium carbonate in marine environments over millions of years.
Uses & applications
Used heavily in construction (as aggregate for concrete and road base), production of lime and cement, and in agriculture to neutralize acidic soils.
Geological facts
Limestone often contains well-preserved fossils of ancient marine organisms and makes up about 10% of the total volume of all sedimentary rocks on Earth.
Field identification & locations
Can be easily identified in the field by its characteristic effervescence (fizzing) when a drop of weak acid, such as vinegar, is applied to its surface due to the release of carbon dioxide.
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