
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: typically gray, white, or tan; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral; Specific gravity: 2.71.
- Hardness
- 3 on Mohs scale
- Color
- typically gray, white, or tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically gray, white, or tan; Luster: dull to earthy; Crystal structure: Trigonal (as calcite); Cleavage: Perfect rhombohedral; Specific gravity: 2.71.
Formation & geological history
Formed primarily from the accumulation of shell, coral, algal, and fecal debris in marine environments. It can also form through chemical precipitation from ocean or lake water. Most deposits range from the Paleozoic to Mesozoic eras.
Uses & applications
Used extensively in construction as road base, railroad ballast, and an ingredient in cement. In industry, it is used for steel manufacturing, glass making, and as a soil conditioner in agriculture.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. Famous structures like the Great Pyramid of Giza and the Parthenon were constructed using various forms of limestone.
Field identification & locations
Identify in the field by its reaction to dilute hydrochloric acid (it will fizz/effervesce). It often contains visible fossils. Commonly found in areas that were once covered by ancient seas, such as the Midwestern United States and Western Europe.
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Sandstone or Siltstone
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