
sedimentary
Fossiliferous Limestone
Biogenic Limestone (Calcium Carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Tan, beige, grey, or yellow-brown; Luster: Dull/Earthy; Structure: Clastic or crystalline matrix with visible fossil inclusions; Reaction: Effervesces strongly with dilute hydrochloric acid.
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, grey, or yellow-brown
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, grey, or yellow-brown; Luster: Dull/Earthy; Structure: Clastic or crystalline matrix with visible fossil inclusions; Reaction: Effervesces strongly with dilute hydrochloric acid.
Formation & geological history
Formed in shallow, calm, warm marine waters from the accumulation of shell, coral, algal, and fecal debris. These sediments are lithified over millions of years through compaction and cementation.
Uses & applications
Used primarily in the construction industry as building stone, agricultural lime, and a component of cement. High-quality slabs are used for architectural cladding and floor tiles.
Geological facts
This rock acts as a biological record of ancient marine life. Many of the visible fragments are likely from brachiopods, crinoids, or gastropods. Limestone accounts for about 10% of the total volume of all sedimentary rocks.
Field identification & locations
Identify in the field by looking for visible fossil fragments and testing with acid (it will fizz). Commonly found in areas that were once ancient sea beds, such as the midwestern United States and southern England.
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