
sedimentary
Limestone
Calcium carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 (Mohs scale); Color: White, gray, or tan; Luster: Dull to earthy; Crystal structure: Trigonal (rhombohedral); Cleavage: Perfect rhombohedral (in calcite crystals); Specific gravity: 2.7
- Hardness
- 3 (Mohs scale)
- Color
- White, gray, or tan
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 (Mohs scale); Color: White, gray, or tan; Luster: Dull to earthy; Crystal structure: Trigonal (rhombohedral); Cleavage: Perfect rhombohedral (in calcite crystals); Specific gravity: 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 lake or ocean water.
Uses & applications
Used widely in construction (aggregate, cement making), as a soil conditioner in agriculture, and as a decorative stone in architecture and landscaping.
Geological facts
Limestone or chalk comprises about 10% of the total volume of all sedimentary rocks. It is the source of material for many of the world's most famous caves and karst landscapes.
Field identification & locations
Identify in the field by its softness (scratched by a copper penny) and its effervescence (fizzing) when in contact with dilute hydrochloric acid or strong vinegar. Commonly found in coastal areas and riverbeds.
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