
mineral
Black Tourmaline
Schorl (NaFe3Al6(BO3)3Si6O18(OH)4)
Hardness: 7-7.5 (Mohs scale), Color: Inky black, Luster: Vitreous to sub-metallic, Crystal Structure: Trigonal (often prismatic with vertical striations), Cleavage: Indistinct/Indiscernible, Specific Gravity: 3.0-3.2
- Hardness
- 7-7
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Physical properties
Hardness: 7-7.5 (Mohs scale), Color: Inky black, Luster: Vitreous to sub-metallic, Crystal Structure: Trigonal (often prismatic with vertical striations), Cleavage: Indistinct/Indiscernible, Specific Gravity: 3.0-3.2
Formation & geological history
Commonly forms in granitic pegmatites, hydrothermal veins, and metamorphic rocks such as mica schists via boron-rich fluids during the late stages of magmatic crystallization.
Uses & applications
Widely used in jewelry when faceted, as a collector specimen, and in industry for its pyroelectric and piezoelectric properties (gauges for measuring pressure transients).
Geological facts
Black tourmaline is the most common variety of tourmaline, making up 95% of all tourmaline in nature. It is strongly pleochroic and can become electrically charged when heated or squeezed.
Field identification & locations
Identify in the field by its characteristic jet-black color, triangular or hexagonal cross-section, and prominent vertical grooves (striations) running down the long axis of the crystals. Found globally in Brazil, Namibia, and the USA (California and Maine).
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Mineral/Rock
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