
mineral
Calcite Rhomb
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Creamy white to pale yellow; Luster: Vitreous to pearly; Crystal Structure: Trigonal/Rhombohedral; Cleavage: Perfect rhombohedral in three directions; Specific Gravity: 2.71
- Hardness
- 3 on Mohs scale
- Color
- Creamy white to pale yellow
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 3 on Mohs scale; Color: Creamy white to pale yellow; Luster: Vitreous to pearly; Crystal Structure: Trigonal/Rhombohedral; Cleavage: Perfect rhombohedral in three directions; Specific Gravity: 2.71
Formation & geological history
Formed through sedimentary precipitation in marine environments or hydrothermal veins. This specimen likely originated from a larger crystalline mass that was cleaved into a rhombohedral shape.
Uses & applications
Used as a major component of cement and mortar in construction, as a soil conditioner in agriculture, and as a decorative mineral specimen for collectors. Transparent varieties are used in optical instruments.
Geological facts
Calcite is famous for its double refraction (birefringence); if you place a clear piece over text, it will appear as two images. It is the primary mineral found in limestone and marble.
Field identification & locations
Identifiable by its 75-degree rhombohedral cleavage and its strong effervescent reaction to dilute hydrochloric acid. Commonly found in limestone quarries and cave systems globally.
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