
sedimentary
Limestone
Calcium Carbonate (CaCO3 - Calcite)
Hardness: 3 on Mohs scale; Color: Gray to dark gray; Luster: Dull to earthy; Texture: Fine-grained, microcrystalline to sub-crystalline; Cleavage: Perfect rhombohedral in calcite grains, but massive in rock form
- Hardness
- 3 on Mohs scale
- Color
- Gray to dark gray
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Gray to dark gray; Luster: Dull to earthy; Texture: Fine-grained, microcrystalline to sub-crystalline; Cleavage: Perfect rhombohedral in calcite grains, but massive in rock form
Formation & geological history
Formed primarily in shallow, warm marine environments from the accumulation and compaction of organic debris such as shell fragments, coral, and micro-algae, as well as chemical precipitation of calcium carbonate from seawater.
Uses & applications
Extensively used in construction as aggregate, in cement and lime manufacturing, soil conditioning in agriculture, industrial acid neutralization, and building stone.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth. It readily reacts with dilute hydrochloric acid, producing visible effervescence (fissing/bubbling), which is a key diagnostic field test.
Field identification & locations
Identify by its gray color, softness (can be scratched by a steel nail), dull luster, and positive acid test. Common worldwide in sedimentary basins, roadcuts, and limestone quarries.
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