
sedimentary
Limestone
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 (Mohs scale); Color: cream, tan, or yellowish-brown; Luster: dull to earthy; Texture: clastic or non-clastic grain structure; Cleavage: none in rock form, rhombohedral in calcite crystals; Specific Gravity: 2.3-2.7
- Hardness
- 3 (Mohs scale)
- Color
- cream, tan, or yellowish-brown
- Luster
- dull to earthy
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Physical properties
Hardness: 3 (Mohs scale); Color: cream, tan, or yellowish-brown; Luster: dull to earthy; Texture: clastic or non-clastic grain structure; Cleavage: none in rock form, rhombohedral in calcite crystals; Specific Gravity: 2.3-2.7
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 waters in caves or springs.
Uses & applications
Extensively used in construction as building stone, road base, and a key ingredient in cement/concrete. Also used as a soil conditioner and in the production of lime.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks on Earth. Most cave systems in the world are formed in limestone because it is easily dissolved by acidic groundwater.
Field identification & locations
Identify in the field by testing with a drop of cold dilute hydrochloric acid; it will effervesce (fizz) vigorously. It is commonly found in ancient seabed deposits and mountainous regions.
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