
sedimentary
Limestone
Limestone (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Grey, tan, off-white; Luster: Dull to earthy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None in massive form; Specific Gravity: 2.3-2.7
- Hardness
- 3 on Mohs scale
- Color
- Grey, tan, off-white
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Grey, tan, off-white; Luster: Dull to earthy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None in massive form; Specific Gravity: 2.3-2.7
Formation & geological history
Formed primarily from the accumulation of shell, coral, algal, and fecal debris in marine environments. Most widespread specimens date from the Paleozoic and Mesozoic eras.
Uses & applications
Extensively used in construction as building stone, road base, and a primary ingredient in Portland cement. Also used as a soil conditioner and in glass making.
Geological facts
Limestone is the primary source of the world's caves through the process of chemical weathering by slightly acidic rainwater. It often contains well-preserved fossils of ancient sea life.
Field identification & locations
Can be identified in the field by its effervescence (fizzing) when exposed to a drop of dilute hydrochloric acid. Common in areas that were once prehistoric seafloors. Look for visible shell fragments or fossils.
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