
sedimentary
Limestone (Fossiliferous)
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Gray to tan; Luster: Dull/Earthy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None/Conchoidal; Specific Gravity: 2.3–2.7
- Hardness
- 3 on Mohs scale
- Color
- Gray to tan
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Gray to tan; Luster: Dull/Earthy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None/Conchoidal; Specific Gravity: 2.3–2.7
Formation & geological history
Formed in marine environments from the accumulation of shell, coral, algal, and fecal debris. It can be millions of years old, often dating from the Paleozoic or Mesozoic eras.
Uses & applications
Used primarily in construction (crushed stone), cement manufacturing, soil conditioning in agriculture, and as a source of lime.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. When it contains visible fossils, as seen in the texture here, it is referred to as fossiliferous limestone.
Field identification & locations
Identify in the field by its reaction (fizzing) to a drop of dilute hydrochloric acid. Commonly found in quarries and surface outcrops in areas once covered by ancient seas.
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