
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: typically white, gray, or tan; Luster: earthy to dull; Crystal structure: Orthorhombic or Trigonal (as calcite/aragonite); Cleavage: perfect rhombohedral in crystal form; Specific Gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- typically white, gray, or tan
- Luster
- earthy to dull
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Physical properties
Hardness: 3 on Mohs scale; Color: typically white, gray, or tan; Luster: earthy to dull; Crystal structure: Orthorhombic or Trigonal (as calcite/aragonite); Cleavage: perfect rhombohedral in crystal form; Specific Gravity: 2.5-2.7
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 water in caves or mineral springs.
Uses & applications
Extensively used in construction as aggregate, road base, and as a key ingredient in cement (Portland cement). It is also used in agriculture for soil neutralization and in the steel manufacturing process.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth. Most of the world's great cave systems, such as Mammoth Cave, are carved out of limestone by acidic groundwater.
Field identification & locations
Identify in the field by its softness (can be scratched by a copper coin or steel knife) and its strong effervescent reaction ('fizzing') when a drop of diluted hydrochloric acid or vinegar is applied. Often contains visible fossils.
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