mineral
Optical Calcite (Iceland Spar)
Calcite (Calcium Carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous; Crystal System: Trigonal; Cleavage: Perfect rhombohedral in three directions; Features double refraction (birefringence).
- Hardness
- 3 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Vitreous
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Physical properties
Hardness: 3 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous; Crystal System: Trigonal; Cleavage: Perfect rhombohedral in three directions; Features double refraction (birefringence).
Formation & geological history
Formed through chemical precipitation from calcium-rich solutions in sedimentary environments, or within hydrothermal veins. It is a primary constituent of limestone and marble.
Uses & applications
Used for optical instruments (historically in gun sights and polarizing microscopes), in the manufacturing of cement, as a soil conditioner in agriculture, and as a popular teaching specimen for mineralogy.
Geological facts
Optical calcite is famous for its 'double refraction' property; when you place the crystal over text, the text appears doubled. Vikings may have used it as a 'sunstone' for navigation on cloudy days.
Field identification & locations
Identify in the field by its rhombohedral shape (like a slanted sub-rectangle) and its vigorous reaction (fizzing) when exposed to cold dilute hydrochloric acid. Commonly found in Chihuahua, Mexico and various limestone regions.
