
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on the Mohs scale; Color: typically grey, tan, or white; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: perfect rhombohedral; Specific gravity: 2.7.
- Hardness
- 3 on the Mohs scale
- Color
- typically grey, tan, or white
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on the Mohs scale; Color: typically grey, tan, or white; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: perfect rhombohedral; Specific gravity: 2.7.
Formation & geological history
Formed primarily in marine environments from the accumulation of shell, coral, algal, and fecal debris. It can also form through chemical precipitation from calcium-rich waters in caves or hot springs. Geological age varies from Precambrian to Holocene.
Uses & applications
Extensively used in construction as building stone, road base, and a primary ingredient in cement/concrete. Used in agriculture to neutralize soil acidity, and in the chemical industry for steel manufacturing and glass making.
Geological facts
Limestone is the source of approximately 10% of all sedimentary rocks. Many of the world's most famous landmarks, including the Great Pyramids of Giza and the Parthenon, are constructed primarily from limestone.
Field identification & locations
Can be identified in the field using the 'acid test'—it will effervesce (fizz) when a drop of diluted hydrochloric acid or strong vinegar is applied. Commonly found in areas that were once ancient sea beds. Check for fossil inclusions to confirm organic origin.
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