
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: typically white, gray, or tan; Luster: dull to earthy; Texture: fine to coarse grained; Cleavage: none (fractures); Specific Gravity: 2.7
- Hardness
- 3 on Mohs scale
- Color
- typically white, gray, or tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically white, gray, or tan; Luster: dull to earthy; Texture: fine to coarse grained; Cleavage: none (fractures); Specific Gravity: 2.7
Formation & geological history
Primarily formed in marine environments from the accumulation of shell, coral, algal, and fecal debris. It can also form through chemical precipitation from ocean water or cave environments.
Uses & applications
Used extensively in construction as building stone and aggregate, in the production of cement, for soil neutralization in agriculture, and as a filler in paper, plastics, and paint.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. It is the primary rock type found in karst landscapes, which are famous for spectacular caves and sinkholes.
Field identification & locations
Identify in the field by its reaction to cold dilute hydrochloric acid (it fizzes). Often contains visible marine fossils. Commonly found in areas that were once prehistoric shallow seabeds.
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