
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Tan, beige, or light gray; Luster: Dull to earthy; Crystal Structure: Trigonal (often microcrystalline); Cleavage: Perfect rhombohedral (but rarely seen in bulk rock); Specific Gravity: 2.5 - 2.7
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, or light gray
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, or light gray; Luster: Dull to earthy; Crystal Structure: Trigonal (often microcrystalline); Cleavage: Perfect rhombohedral (but rarely seen in bulk rock); Specific Gravity: 2.5 - 2.7
Formation & geological history
Formed primarily from the accumulation of shell, coral, algal, and fecal debris in warm, shallow marine waters. Can also form through chemical precipitation from calcium-rich water. Age varies from Precambrian to Holocene.
Uses & applications
Widely used in the construction industry as aggregate for road base and railroad ballast, in the production of cement and lime, as a soil conditioner in agriculture, and as a dimension stone for architecture.
Geological facts
Limestone covers about 10% of the total surface area of the Earth. It is the primary component of many famous landscapes, including the White Cliffs of Dover and the pyramids of Giza, which were encased in Tura limestone.
Field identification & locations
Identify in the field by the 'acid test'—it will vigorously effervesce (fizz) when a drop of dilute hydrochloric acid is applied. Commonly found in areas that were once prehistoric seafloors. Collectors look for fossil inclusions.
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