
sedimentary
Limestone
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Tan, beige, or gray; Luster: Dull/Earthy; Crystal Structure: Trigonal (microcrystalline); Cleavage: Perfect rhombohedral in calcite crystals, though often inconspicuous in rock form.
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, or gray
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, or gray; Luster: Dull/Earthy; Crystal Structure: Trigonal (microcrystalline); Cleavage: Perfect rhombohedral in calcite crystals, though often inconspicuous in rock form.
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 calcium-rich waters.
Uses & applications
Used extensively in construction as road base, concrete aggregate, and building stone. Also used in the production of lime, cement, and as a soil conditioner in agriculture.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. Most of the world's caves are formed in limestone because it is easily dissolved by slightly acidic groundwater.
Field identification & locations
Identify in the field by its softness (can be scratched by a copper coin) and its effervescence (bubbling) when in contact with dilute hydrochloric acid or strong vinegar. Common in karst landscapes and coastal cliffs.
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