
sedimentary
Fossiliferous Limestone
Calcite (CaCO3) Rich Bio-sedimentary Rock
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Tan, beige, or grey with visible fossil imprints; Luster: Dull or earthy; Crystal structure: Usually microcrystalline matrix with macrofossils; Cleavage: None (rhombohedral cleavage only in pure calcite crystals); Specific gravity: 2.3–2.7
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, or grey with visible fossil imprints
- Luster
- Dull or earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, or grey with visible fossil imprints; Luster: Dull or earthy; Crystal structure: Usually microcrystalline matrix with macrofossils; Cleavage: None (rhombohedral cleavage only in pure calcite crystals); Specific gravity: 2.3–2.7
Formation & geological history
Formed in warm, shallow marine environments through the accumulation of shell, coral, algal, and fecal debris over millions of years. This specimen likely dates from the Phanerozoic Eon, when marine life was abundant.
Uses & applications
Used primarily in the construction industry as building stone, road base, and in the production of cement. Small specimens are popular for educational purposes and novice fossil collecting.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. It often tells a story of ancient oceans that once covered landmasses that are now high above sea level.
Field identification & locations
Identify in the field by looking for visible shells or skeletal fragments; it will also vigorously effervesce (fizz) when a drop of weak hydrochloric acid or vinegar is applied. Commonly found in quarries, road cuts, and riverbeds.
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