
sedimentary
Fossiliferous Limestone
Biogenic Limestone (Calcium Carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3 (Mohs scale); Color: Dark grey to charcoal with white/tan biological inclusions; Luster: Dull/Earthy; Structure: Massive with micro-fossil fragments; Cleavage: None (conchoidal to irregular fracture); Specific Gravity: 2.5-2.7
- Hardness
- 3 (Mohs scale)
- Color
- Dark grey to charcoal with white/tan biological inclusions
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3 (Mohs scale); Color: Dark grey to charcoal with white/tan biological inclusions; Luster: Dull/Earthy; Structure: Massive with micro-fossil fragments; Cleavage: None (conchoidal to irregular fracture); Specific Gravity: 2.5-2.7
Formation & geological history
Formed in warm, shallow marine environments through the accumulation of organic debris, such as shell fragments and corals, which are later lithified. Most often dates from the Paleozoic or Mesozoic eras.
Uses & applications
Primary source of lime for cement, used in construction (crushed stone), soil conditioner in agriculture, and as a decorative building stone.
Geological facts
This specific piece appears to contain 'hash' or fragments of ancient marine life, possibly crinoid stems or small bivalve fragments. Limestone preserves the history of Earth's ancient oceans and represents one of the largest carbon sinks on the planet.
Field identification & locations
Identify in the field by its reaction (fizzing) when exposed to a drop of dilute hydrochloric acid (vinegar may work weakly). Look for visible shell fragments or small tubular shapes on weathered surfaces. Commonly found in former seabed regions.
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