
sedimentary
Fossiliferous Limestone
Biogenic Limestone (Calcium Carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Tan, beige, grey, and cream; Luster: Dull to earthy; Crystal structure: Hexagonal/Trigonal (calcite); Cleavage: Perfect rhombohedral in calcite matrix; Specific gravity: 2.71
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, grey, and cream
- Luster
- Dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, grey, and cream; Luster: Dull to earthy; Crystal structure: Hexagonal/Trigonal (calcite); Cleavage: Perfect rhombohedral in calcite matrix; Specific gravity: 2.71
Formation & geological history
Formed in shallow marine environments where organic debris like shells, corals, and algal remains accumulate and are compressed over millions of years. This specimen appears to contain brachiopod or bivalve imprints common from the Paleozoic to Mesozoic eras.
Uses & applications
Used primarily in construction (crushed stone, cement manufacturing), as a building material, in agriculture for soil conditioning, and as educational or decorative specimens for collectors.
Geological facts
Limestone contains roughly 10% of the total volume of all sedimentary rocks. The presence of shells in this rock indicates it was once part of an ancient seafloor.
Field identification & locations
Identify in the field by the visible presence of fossilized shells or casts and by testing with diluted hydrochloric acid; limestone will effervesce (fizz). Commonly found in areas with past marine history like the Midwest United States or the UK.
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