
mineral
Black Tourmaline (Schorl)
Schorl (NaFe2+3Al6(BO3)3Si6O18(OH)4)
Hardness: 7-7.5 on Mohs scale. Color: Jet black to brownish-black. Luster: Vitreous to sub-metallic. Crystal system: Trigonal. Cleavage: Indistinct. Specific gravity: 3.0-3.2. These specimens are tumbled and polished.
- Hardness
- 7-7
- Color
- Jet black to brownish-black
- Luster
- Vitreous to sub-metallic
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Physical properties
Hardness: 7-7.5 on Mohs scale. Color: Jet black to brownish-black. Luster: Vitreous to sub-metallic. Crystal system: Trigonal. Cleavage: Indistinct. Specific gravity: 3.0-3.2. These specimens are tumbled and polished.
Formation & geological history
Forms primarily in granitic pegmatites, hydrothermal veins, and metamorphic rocks like schist and gneiss. It is a boron-rich silicate mineral commonly associated with quartz and feldspar.
Uses & applications
Used extensively in jewelry, as protective talismans in metaphysical circles, and historically in scientific instruments due to its piezoelectric and pyroelectric properties.
Geological facts
Black tourmaline is the most common member of the tourmaline group, making up about 95% of all tourmaline found in nature. It was known as 'Schorl' as early as the 14th century, named after a village in Saxony, Germany.
Field identification & locations
Identified by its deep black color, vertical striations (if untumbled), and strong hardness. It is common in pegmatites globally, with notable deposits in Brazil, Namibia, and China. Collectors look for high-gloss polish and minimal inclusions.
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