
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: typically grey, white, or tan; Luster: dull to earthy; Crystal Structure: trigonal (when calcite is visible); Cleavage: perfect rhombohedral in calcite crystals; Specific Gravity: 2.5-2.7
- Hardness
- 3 on Mohs scale
- Color
- typically grey, white, or tan
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: typically grey, white, or tan; Luster: dull to earthy; Crystal Structure: trigonal (when calcite is visible); Cleavage: perfect rhombohedral in calcite crystals; Specific Gravity: 2.5-2.7
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 lake or ocean water. Geological age can range from Precambrian to Recent.
Uses & applications
Extensively used as a building material, in the manufacture of cement/lime, as an aggregate for the base of roads, as a white pigment or filler in products such as toothpaste or paints, and as a soil conditioner in agriculture.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. It is the primary material found in famous karst landscapes and cave systems like Mammoth Cave in the USA. Most fossils are found within limestone layers.
Field identification & locations
Identify in the field by its tendency to fizz (effervesce) when a drop of dilute hydrochloric acid is applied. It often contains visible fossils and occurs in massive beds. Common worldwide, especially in areas that were once prehistoric shallow seas.
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