
sedimentary
Limestone
Calcareous sedimentary rock (primarily CaCO3)
Hardness: 3 on Mohs scale; Color: typically off-white, buff, or gray; Luster: dull to earthy; Crystal structure: microcrystalline or massive calcite; Cleavage: rhombohedral in calcite crystals but often invisible in bulk rock; Specific gravity: approx 2.5-2.7.
- Hardness
- 3 on Mohs scale
- Color
- typically off-white, buff, or gray
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically off-white, buff, or gray; Luster: dull to earthy; Crystal structure: microcrystalline or massive calcite; Cleavage: rhombohedral in calcite crystals but often invisible in bulk rock; Specific gravity: approx 2.5-2.7.
Formation & geological history
Formed in marine environments from the accumulation of shell, coral, algal, and fecal debris. It can also form through chemical precipitation from calcium-rich water. Most surface limestone is Paleozoic or Mesozoic in age.
Uses & applications
Major ingredient in cement/concrete, used as building stone, road base, and in agricultural lime for pH balancing. High-purity limestone is used in glass making and chemical processes.
Geological facts
Limestone contains roughly 10% of the total volume of all sedimentary rocks. It often contains fossils of marine organisms because it forms in shallow sea beds.
Field identification & locations
Identify in the field by testing with cold dilute hydrochloric acid; it will effervesce (fizz) vigorously. It is commonly found in areas with karst topography, caves, and cliffs. Look for light-colored, relatively soft rock that reacts to acid.
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