
mineral
Optical Calcite
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Colorless to white; Luster: Vitreous to pearly; Crystal Structure: Trigonal (rhombohedral cleavage); Cleavage: Perfect rhombohedral in three directions; Specific Gravity: 2.71
- Hardness
- 3 on Mohs scale
- Color
- Colorless to white
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 3 on Mohs scale; Color: Colorless to white; Luster: Vitreous to pearly; Crystal Structure: Trigonal (rhombohedral cleavage); Cleavage: Perfect rhombohedral in three directions; Specific Gravity: 2.71
Formation & geological history
Formed in sedimentary environments as a chemical precipitate from evaporating seawater or in hydrothermal veins and hot springs. It can also form through biological processes in marine organisms.
Uses & applications
Used in the manufacture of high-grade optical instruments (polarizing prisms) due to its double refraction properties. Also used in construction (as limestone/marble), fertilizer, and as a popular collector's specimen.
Geological facts
Also known as Iceland Spar, this mineral exhibits double refraction, where light rays entering the crystal are split into two, making any text viewed through it appear doubled. Vikings may have used it for navigation on cloudy days.
Field identification & locations
Identified in the field by its rhombohedral shape, softness (can be scratched by a copper penny), and its strong reaction (fizzing) to cold dilute hydrochloric acid. Commonly found in Mexico, Iceland, and the United States.
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