
sedimentary
Limestone with Calcite Veins
Calcium Carbonate (CaCO3)
Hardness: 3 (Mohs scale); Color: Dark grey to bluish-black matrix with white veins; Luster: Dull to earthy (matrix), vitreous (veins); Cleavage: Perfect rhombohedral in calcite portions; Specific Gravity: 2.71.
- Hardness
- 3 (Mohs scale)
- Color
- Dark grey to bluish-black matrix with white veins
- Luster
- Dull to earthy (matrix), vitreous (veins)
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Physical properties
Hardness: 3 (Mohs scale); Color: Dark grey to bluish-black matrix with white veins; Luster: Dull to earthy (matrix), vitreous (veins); Cleavage: Perfect rhombohedral in calcite portions; Specific Gravity: 2.71.
Formation & geological history
Formed in marine environments from the accumulation of shell, coral, and algal debris. The white veins are secondary calcite deposits that filled fractures within the stone via hydrothermal fluids or groundwater over millions of years.
Uses & applications
Used primarily in construction for building stone, aggregate for concrete, and the production of cement. Distinctive veined specimens are sometimes used for decorative landscaping or small carvings.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. The presence of white veins often indicates tectonic activity that cracked the original rock, allowing mineral-rich water to seep in and crystallize.
Field identification & locations
Identified in the field by its reaction (fizzing) to dilute hydrochloric acid. It is commonly found in mountain ranges that were once ancient sea beds, such as the Alps or the Appalachians. To collect, look for eroded pebbles in riverbeds or near limestone cliffs.
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