
sedimentary
Fossiliferous Limestone
Calcium Carbonate (CaCO3) with Bioclasts
AI-generated identification · may be incorrectHardness: 3 (Mohs scale); Color: Light gray to blue-gray; Luster: Dull to earthy; Structure: Granular with visible fossil imprints; Cleavage: None (conchoidal to irregular fracture); Specific Gravity: 2.5-2.7
- Hardness
- 3 (Mohs scale)
- Color
- Light gray to blue-gray
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 (Mohs scale); Color: Light gray to blue-gray; Luster: Dull to earthy; Structure: Granular with visible fossil imprints; Cleavage: None (conchoidal to irregular fracture); Specific Gravity: 2.5-2.7
Formation & geological history
Formed in warm, shallow marine environments from the accumulation of shell, coral, algal, and fecal debris. These sediments are lithified over millions of years through compaction and cementation. Often dates from the Paleozoic or Mesozoic eras.
Uses & applications
Used primarily in the construction industry as crushed stone for road base, concrete aggregate, and the production of cement and lime. It is also used as an agricultural soil conditioner.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. When it contains high concentrations of recognizable fossils, it provides a crucial record of ancient marine life and past climate conditions.
Field identification & locations
Identify in the field by its characteristic gray color and the presence of small shell or organic remains. A definitive test is the 'acid test': it will effervesce (fizz) vigorously when a drop of dilute hydrochloric acid or vinegar is applied. Found worldwide in regions once covered by inland seas.
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